@inproceedings{TaklaRaabRaab, author = {Takla, Melanie and Raab, Thomas and Raab, Alexandra}, title = {Standort 4 - Eisenh{\"u}ttenwerk Peitz. Die fr{\"u}hindustrielle K{\"o}hlerei in der J{\"a}nschwalder Heide (Niederlausitz). Eine GIS-basierte Rekonstruktion des Wald- und Landschaftszustandes mithilfe historischer Karten ab dem 18. Jahrhundert}, series = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie- Jahrestagung 2013, 2.-4.5.2013, BTU Cottbus}, booktitle = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie- Jahrestagung 2013, 2.-4.5.2013, BTU Cottbus}, editor = {Raab, Thomas and Hirsch, Florian and Raab, Alexandra and Schopper, Franz and Freytag, Klaus}, publisher = {BTU Cottbus}, address = {Cottbus}, pages = {89 -- 97}, abstract = {Die hier vorgestellte Forschungsarbeit besch{\"a}ftigt sich mit der Rekonstruktion der Landschafts- und Umweltgeschichte mithilfe Geographischer Informationssysteme (GIS) und historischer Karten. In einem Modell sollen die r{\"a}umliche Dimension der K{\"o}hlerei, der damit verbundene Holzverbrauch, der Zustand der W{\"a}lder, die vorhandene Infrastruktur etc. errechnet und dargestellt werden. Zeitlicher Schwerpunkt ist die zweite H{\"a}lfte des 18. Jahrhunderts und die Mitte des 19. Jahrhunderts.}, language = {de} } @incollection{TaklaRaabRaab, author = {Takla, Melanie and Raab, Thomas and Raab, Alexandra}, title = {Mit dem GIS zur Landschaftsgeschichte. Datengrundlage und Forschungsansatz zum Modell der fr{\"u}hindustriellen Holzkohleproduktion in der J{\"a}nschwalder Heide}, series = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2009/2010}, booktitle = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2009/2010}, editor = {Schopper, Franz}, publisher = {Brandenburgisches Landesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Landesmuseum}, address = {W{\"u}nsdorf}, isbn = {978-3-910011-73-1}, pages = {267 -- 273}, language = {de} } @misc{NicolayRaabRaabetal., author = {Nicolay, Alexander and Raab, Alexandra and Raab, Thomas and R{\"o}sler, Horst and B{\"o}nisch, Eberhard and Murray, Andrew S.}, title = {Evidence of (pre-) historic to modern landscape and land use history near J{\"a}nschwalde (Brandenburg, Germany)}, series = {Zeitschrift f{\"u}r Geomorphologie, Suppl.}, volume = {58}, journal = {Zeitschrift f{\"u}r Geomorphologie, Suppl.}, number = {2}, issn = {1864-1687}, doi = {10.1127/0372-8854/2014/S-00162}, pages = {7 -- 31}, abstract = {In the apron of the active lignite opencast pit J{\"a}nschwalde (Brandenburg, Germany), three archaeological survey trenches were investigated in an area where aeolian sand deposits are widespread. The investigated sediment sequences contain evidence of aeolian morphodynamics, soil formation and agricultural land use. To study the age and the causes of sand drifting and surface stabilization, standard soil physical and chemical laboratory analyses as well as optically stimulated luminescence (OSL) and radiocarbon dating (14C) were carried out. Two main sedimentological units were identified: Unit 1 consists of glacio-fluvial and Late Glacial aeolian sands representing the parent material for the native Podsol- Braunerde, while Unit 2 represents the Late Holocene aeolian deposits. Four periods of Late Glacial and Holocene aeolian activity and three phases of geomorphological stability have been identified: (i) Aeolian sedimentation during the Late Glacial, (ii) Mesolithic reactivation of aeolian processes, (iii) soil formation until Late Roman Iron Age settlers intensified the agricultural land use, (iv) intensive drift sand formation during the High Middle Ages due to agricultural expansion, (v) stabilization of the drift sands and weak soil formation, (vi) reactivation of aeolian processes due to the increasing wood consumption and charcoal production from the early 17th until the mid-19th century, (vii) surface stabilization and formation of Regosols since the mid-19th century due to afforestation.}, language = {en} } @misc{SchneiderTaklaNicolayetal., author = {Schneider, Anna and Takla, Melanie and Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {A Template-matching Approach Combining Morphometric Variables for Automated Mapping of Charcoal Kiln Sites}, series = {Archaeological Prospection}, volume = {22}, journal = {Archaeological Prospection}, number = {1}, issn = {1099-0763}, doi = {10.1002/arp.1497}, pages = {45 -- 62}, abstract = {Analysing the spatial distribution of anthropogenic relief structures can contribute to the understanding of past landuse systems. With automated mapping routines, small relief forms can be detected efficiently from high-resolution digital terrain models (DTMs). In this study, we describe an approach for the automated mapping of charcoal kiln sites from an airborne laser-scanning DTM. The study site is located north of Cottbus, Germany, where an exceptionally large historic charcoal production field has been documented in previous archaeological surveys. The goal of this study was to implement, evaluate and improve an automated GIS-based routine for mapping these features based on the template-matching principle. In addition to the DTM, different morphometric variables were evaluated for their suitability to detect kiln sites. The mapping results were validated against a comprehensive database of kiln sites recorded from archaeological excavations and via manual digitization. The effects of irregular kiln-site geometry and DTM noise were evaluated using synthetic DTMs. The results of the synthetic DTM mapping show that the template-matching results differed depending on the morphometric variable used for the mapping process. In accordance with this observation, a validation of the mapping procedure for the field site suggests that feature mapping can be improved. In particular, the number of false detections can be reduced using a combination of morphometric variables. For the validation area, the kiln sites with diameters of at least 10m were mapped using the automated routine, with detection rates that were close to those of manual digitization. Therefore, the described method can considerably facilitate the mapping and distribution analysis of kiln sites or similar small relief forms that are prominent in a specific landscape.}, language = {en} } @inproceedings{HirschSchneiderRaabetal., author = {Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas and Buras, Allan and Maaten, Ernst van der and Takla, Melanie and R{\"a}biger, Christin and Cruz-Garc{\´i}a, Roberto and Wilmking, Martin}, title = {Effects of historic charcoal burning on soil properties}, series = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, booktitle = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{SchneiderTaklaRaabetal., author = {Schneider, Anna and Takla, Melanie and Raab, Alexandra and Raab, Thomas and Bonhage, Alexander and Hirsch, Florian and R{\"o}sler, Horst}, title = {Towards an inventory of historic charcoal production fields in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, booktitle = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{HirschSchneiderNicolayetal., author = {Hirsch, Florian and Schneider, Anna and Nicolay, Alexander and Błaszkiewicz, Mirosław and Kordowski, Jarosław and Noryskiewicz, Agnieszka M. and Tyszkowski, Sebastian and Raab, Alexandra and Raab, Thomas}, title = {Late Quaternary landscape development at the margin of the Pomeranian phase (MIS 2) near Lake Wygonin (Northern Poland)}, series = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, booktitle = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{NicolayRaabRaabetal., author = {Nicolay, Alexander and Raab, Alexandra and Raab, Thomas and R{\"o}sler, Horst and B{\"o}nisch, Eberhard}, title = {Holocene landscape reconstruction and land use changes in Lower Lusatia (Southern Brandenburg, East Germany) - pedological and geomorphological approaches}, series = {2010 GSA Annual Meeting in Denver Colorado, USA 2010, 31 October - 3 November}, booktitle = {2010 GSA Annual Meeting in Denver Colorado, USA 2010, 31 October - 3 November}, publisher = {Geological Society of America}, address = {Boulder, Colo.}, pages = {S. 419}, abstract = {Modern lignite mining in southern Brandenburg (East Germany) causes the destruction of entire landscapes. To date, research concentrated on the reclamation of areas affected by mining-related activities, but the significance of prehistoric and historic cultures on land use changes is disregarded. Recently, a joint research project was launched for interdisciplinary long-term palaeoenvironmental research and to study anthropogenic landscape change in southern Brandenburg. The project partners are geoscientists from the Brandenburg University of Technology (BTU) Cottbus and archaeologists from the Brandenburgisches Landesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Museum (BLDAM), within the scope of this project pedological and geomorphological investigations are carried out to reconstruct Holocene landscape and land use change in the apron of the opencast pit J{\"a}nschwalde (Lower Lusatia), c. 100 southeast of Berlin and c. 15 km northeast of Cottbus. By law large-scale surveys and excavations have to be carried out in the forefield to document all archaeological findings. In combination with the excellent outcrop situation the archaeological investigation offers ideal conditions to study the soil geomorphology on a landscape scale. Fieldwork includes topographical surveying by differential GPS. Soils and sediments are described along cross-sections (up to 140 m long, up to 2 m deep). Field-portable XRF analyzes (FPXRF) is used for a quick characterization of total element concentrations of the substrates. Standard analytical methods (e.g., soil texture, contents of pedogenic oxides) are carried out in the laboratory. To obtain chronological information, radiocarbon and OSL (optically stimulated luminescence) dating are applied on suitable material. Evidence of different land use and land use change in the study area is abundant. For example, at several cross-sections agricultural soil horizons are covered with up to 150 cm thick eolian sands, proving that deforestation and agricultural use induced eolian soil erosion. In addition, remnants of charcoal piles buried under up to 150 cm thick eolian sands indicate remobilization of Quaternary sands as a consequence of clearing for charcoal production. The ongoing investigations will concentrate on fieldwork. Preliminary results are presented.}, language = {en} } @inproceedings{BłaszkiewiczBrademannBraueretal., author = {Błaszkiewicz, Mirosław and Brademann, Brian and Brauer, Achim and Brykała, Dariusz and Deg{\´o}rski, Marek and Froehlich, Wojciech and Gierszewski, Piotr and Hirsch, Florian and Kaczmarek, Halina and Kordowski, Jarosław and Kramkowski, Mateusz and Krzymińska, Jarmila and Lamparski, Piotr and Lutyńska, Monika and Mirosław-Grabowska, Joanna and Nicolay, Alexander and Noryśkiewicz, Agnieszka M. and Noryśkiewicz, Bożena and Obremska, Milena and Ott, Florian and Raab, Alexandra and Raab, Thomas and Schneider, Anna and Schwab, Markus}, title = {Introduction to ICLEA fieldtrips - Stara Kiszewa 2013}, series = {2nd Annual ICLEA Workshop 2013, Dynamics of climate and landscape evolution of cultural landscapes in the Northern Central European Lowlands since the last ice age, Abstract volume \& Excursion guide}, booktitle = {2nd Annual ICLEA Workshop 2013, Dynamics of climate and landscape evolution of cultural landscapes in the Northern Central European Lowlands since the last ice age, Abstract volume \& Excursion guide}, publisher = {Deutsches GeoForschungsZentrum GFZ}, address = {Potsdam}, doi = {10.2312/GFZ.b103-13047}, pages = {53 -- 67}, language = {en} } @incollection{RaabRaab, author = {Raab, Thomas and Raab, Alexandra}, title = {Impacts of Early Land Use and Mining on River Landscapes}, series = {World Heritage and Cultural Diversity}, booktitle = {World Heritage and Cultural Diversity}, editor = {Offenh{\"a}ußer, Dieter and Zimmerli, Walther Ch. and Albert, Marie-Theres}, publisher = {German Commission for UNESCO}, address = {Bonn}, isbn = {978-3-940785-20-6}, pages = {252 -- 259}, language = {en} } @incollection{SchneiderRaabRoesleretal., author = {Schneider, Anna and Raab, Alexandra and R{\"o}sler, Horst and Takla, Melanie and Hirsch, Florian and Ritschl, Bosse and Raab, Thomas}, title = {Geophysikalische Prospektion und Mikrodrohnenbefliegungen zur Dokumentation von Meilerpl{\"a}tzen in der J{\"a}nschwalder Heide}, series = {Ausgrabungen im Niederlausitzer Braunkohlerevier 2013/2014}, booktitle = {Ausgrabungen im Niederlausitzer Braunkohlerevier 2013/2014}, editor = {Schopper, Franz and B{\"o}nisch, Eberhard}, publisher = {Brandenburgisches LAndesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Landesmuseum}, address = {Zossen OT W{\"u}nsdorf}, isbn = {978-3-910011-79-3}, pages = {145 -- 154}, language = {de} } @misc{SchneiderHirschWechleretal., author = {Schneider, Anna and Hirsch, Florian and Wechler, Klaus-Peter and Raab, Alexandra and Raab, Thomas}, title = {Reconstruction of a Paleosurface and Archaeological Site Location in an Anthropogenic Drift Sand Area}, series = {Archaeological Prospection}, volume = {24}, journal = {Archaeological Prospection}, number = {4}, issn = {1099-0763}, doi = {10.1002/arp.1571}, pages = {297 -- 310}, abstract = {Knowledge of the position of archaeological remains in the surface relief provides important basic information for archaeological survey design and interpretation. Geomorphological processes in (pre)history may have resulted in a modification of the local relief around archaeological sites, especially in areas that are prone to sediment erosion and relocation, such as sheet sand and dune landscapes. In this study, we reconstructed and analysed the palaeorelief of an archaeological excavation site in an inland dune area in southern Brandenburg, Germany. The remains of two Mesolithic sites were documented in the archaeological excavations and found to be associated with a buried soil horizon. To gather information on the relief of the buried soil surface, we used a combination of sedimentological and pedological profile descriptions along archaeological survey trenches and geophysical prospection with ground penetrating radar supplemented with microdrone photography and photogrammetry, global positioning system (GPS) surveys, and analysis of LiDAR-based elevation models. A digital elevation model of the buried surface was generated and analysed using a geographical information system (GIS). A comparison of the palaeosurface model with the recent surface elevation model shows that sand remobilization resulted in a considerable reshaping of the relief. Further, an analysis of the buried surface model shows that the relief position of the two archaeological sites in the study area was considerably more prominent in relation to the corresponding buried soil surface than in relation to the recent surface morphology. The results affirm the significance of Holocene sediment relocation for the local surface morphology and the importance of considering such relief modifications in archaeological surveys.}, language = {en} } @inproceedings{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Bonhage, Alexander and Raab, Thomas}, title = {Bodenver{\"a}nderungen durch die historische Holzkohleproduktion in Brandenburg}, series = {Abstracts der Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, G{\"o}ttingen, 2017}, booktitle = {Abstracts der Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, G{\"o}ttingen, 2017}, publisher = {DBG}, address = {G{\"o}ttingen}, pages = {1}, language = {de} } @inproceedings{RaabRaabTaklaetal., author = {Raab, Thomas and Raab, Alexandra and Takla, Melanie and Nicolay, Alexander and Hirsch, Florian and Schneider, Anna and R{\"o}sler, Horst}, title = {Integrative Application of Traditional and Cutting-Edge Techniques to Reconstruct Holocene Earth Surface Processes and Landscape Dynamics - A Case Study from the Northern German Lowland}, series = {AGU Joint Assembly, Montreal, 2015, abstracts listing}, booktitle = {AGU Joint Assembly, Montreal, 2015, abstracts listing}, pages = {135 -- 136}, abstract = {This study outlines the opportunities to reconstruct Holocene landscape dynamics in active opencast lignite mines in southern Brandenburg (Germany). Studies on extensive outcrops that address geomorphology, pedology and archaeology provide unique insights into human-induced environmental changes. Our approach uses a variety of traditional and cutting-edge techniques to characterize small-scale landforms (high-resolution DEMs by micro-drone and LiDAR), to analyze soils and substrate properties in the field (GPR, ERT, geomagnetics, Field Portable XRF and XRD) and to provide chronological information (OSL, 14C, tree-ring dating). This approach is combined with a GIS for data integration. We present the most recent results and review important findings from the last several years. Studies conducted in the opencast mines focus on soil development and Late Quaternary geomorphodynamics and as well as past land use and the legacy of agriculture and woodland use. Our results regarding the human-induced geomorphodynamics are similar to those in other regions in Central Europe, but we also observe regional differences caused by the local setting, e.g., intensification of soil erosion coinciding with the expansion of farming of cultivated lands in the Slavic Middle Ages. By analyzing LiDAR data the largest area of historical charcoal production in the Northern European Lowland (NEL) has been revealed. We are clearly only beginning to understand the massive dimensions of charcoal production in the region and the impact on late Holocene geomorphodynamics. The usage of new high-resolution imagery is essential to identify small-scale anthropogenic landforms hidden in the landscape. Future work will consist of developing and improving our integrative approach. However, comprehensive ground truth data provided by the archaeological prospections in the open-cast mines are an excellent basis for GIS-based analyses of high-resolution ALS data and geomorphological research.}, language = {en} } @inproceedings{SchneiderTaklaRaabetal., author = {Schneider, Anna and Takla, Melanie and Raab, Alexandra and Raab, Thomas and Hirsch, Florian and R{\"o}sler, Horst}, title = {Mapping historic charcoal production fields from excavation to landscape scale}, series = {AGU Joint Assembly, Montreal, 2015, abstracts listing}, booktitle = {AGU Joint Assembly, Montreal, 2015, abstracts listing}, pages = {168}, abstract = {In the forefield of the open-cast mine J{\"a}nschwalde (north of Cottbus, Germany), archaeological excavations have revealed one of the largest charcoal production fields described so far. As remains of the historic charcoal kilns, small mounds of sediment rich in charcoal fragments and ash cover the soil surface. We applied a combination of methods for mapping such kiln relicts across a range of scales, in order to analyze the spatial distribution of kiln sites and to improve the understanding of historic forest use systems. In archaeological excavations in the mine forefield, the geometry of kiln relicts could be studied in high detail. We used a microdrone to record high-resolution photographs of excavation sites for the documentation of kiln site ground plans and other traces of historic land use. Based on airborne laser scanning elevation models, kiln site mapping was extended to areas beyond the mine forefield. Manual digitization from shaded relief maps was used for mapping kiln sites in further woodland areas surrounding an historic ironwork north of Cottbus. An automated mapping approach based on template matching was developed to detect charcoal production fields on a larger scale, and was applied for an area of about 1000 km2up to now. In archaeological excavations, about 900 kiln sites have been documented on an approximately 17 km2 large area. Excavation documentations and aerial photographs show variations in the kiln site ground plans. By manual digitization from Shaded Relief Maps, more than 5000 kiln sites with diameters up to 29 m were detected in the 32 km2 area of the royal forest J{\"a}nschwalder Heide north of Cottbus. First results of mapping for larger areas indicate similar densities, but smaller diameters of kiln sites in other charcoal production fields; and show that charcoal production is a so far underestimated component of the land use history in many areas in the Northern European Lowlands.}, language = {en} } @inproceedings{RaabRaabSchneideretal., author = {Raab, Thomas and Raab, Alexandra and Schneider, Anna and Takla, Melanie and Nicolay, Alexander and R{\"o}sler, Horst}, title = {Mapping the legacies of historic charcoal production}, series = {American Geophysical Union, Fall Meeting San Franisco, USA, 2014}, booktitle = {American Geophysical Union, Fall Meeting San Franisco, USA, 2014}, abstract = {The historic production of charcoal is an important component of the late Holocene fire history for many landscapes. Charcoal production can have numerous effects on ecosystems, e.g., through changes in forest area and structure, or through the effects of pyrolysis, charcoal and ash addition to soils. To assess such effects, it is necessary to understand the spatial extent and patterns of historic charcoal production, which has so far hardly been approached for the Northern European Lowlands. In the forefield of the open-cast mine J{\"a}nschwalde (north of Cottbus, Germany), archaeological excavations have revealed one of the largest charcoal production fields described so far. For this area, we applied and evaluated different methods for mapping the spatial distribution of charcoal kiln remains. We present methods and results of our work in this exceptionally well-described charcoal production field and of additional studies on kiln site distribution in regions of the Northern European Lowlands. The large-scale excavations in the mine forefield provide exact information on kiln site geometry. Using airborne laser scanning elevation models, the mapping of kiln sites could be extended to areas beyond the mine forefield. To detect kiln sites for larger areas, an automated GIS based mapping routine, based on a combination of morphometric parameters, was developed and evaluated. By manual digitization from Shaded Relief Maps, more than 5000 kiln sites in an area of 32 km2 were detected in the J{\"a}nschwalde mine forefield, with 1355 kiln sites that are wider than 12 m. These relatively large kiln sites could be mapped with detection rates that are close to those of manual digitization using the automated routine. First results for different study areas indicate that charcoal production is a so far underestimated component of the land use history in many parts of the Northern European Lowlands.}, language = {en} } @misc{RaabHirschOuimetetal., author = {Raab, Thomas and Hirsch, Florian and Ouimet, William and Johnson, Katharine M. and Dethier, David and Raab, Alexandra}, title = {Architecture of relict charcoal hearths in northwestern Connecticut, USA}, series = {Geoarchaeology}, volume = {32}, journal = {Geoarchaeology}, number = {4}, issn = {1520-6548}, doi = {10.1002/gea.21614}, pages = {502 -- 510}, abstract = {Relict charcoal hearths are round or elliptical earthen platforms up to 11 m in diameter and a widespread feature of historical industry that supplied charcoal used in the production of iron in furnaces or smelters. The iron industry dominated Litchfield County, Connecticut, and surrounding areas in the northeastUnited States throughout the 19th century, peaking in ∼1850. The large number of charcoal hearths in this region is a relic of >150 years of widespread iron production. In this study, we describe the architecture and soil stratigraphy of 26 charcoal hearths in Litchfield County. This contribution aims to (1) compare soils that comprise the charcoal hearths with "natural" adjacent soils, (2) measure the thickness of topsoil developed upon the hearths, and (3) characterize the stratigraphy associated with these features. Results indicate that the black topsoils overlying the charcoal hearths contain residual charcoal and are on average 2.6 times thicker than adjacentCambisols. Charcoal hearths display two ormore black, charcoal-rich strata separated by layers of reddish-brown soil low in charcoal content indicating multiple episodes of use.We also find that many charcoal hearths have been stabilized with boulders on the downslope side during construction and repeated use.Overall, the results presented here provide significant information regarding the construction, use, and associated impacts of earthen platforms for charcoal production in the northeastUnited States, with further relevance to other areas where historical charcoal production occurred.}, language = {en} } @inproceedings{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Bonhage, Alexander and Raab, Thomas}, title = {Assessing the legacy effects of historic charcoal production in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {Charcoal produced in kilns or hearths was an important source of energy in many regions of Europe and Northern America until the 19th century, and charcoal production in hearths is still common in many other regions of the world. The remains of charcoal hearths are therefore a widespread legacy of historic land use in forest areas. Soils on charcoal hearth sites are characterized by a technogenic layer rich in charcoal and ash on top of the soil profile, and by a pyrogenic modification of substrates below the former hearth. The aims of our study are to examine how these alterations to the natural soil profiles affect the soil water regime and other soil physical properties, and to assess the relevance of these effects on the landscape scale. We present first results of a mapping of hearth site occurrence in forest areas in the state of Brandenburg, Germany, and of a characterization of the infiltration behaviour on hearth sites as compared with undisturbed forest soils. Results of mapping small-scale relief features from LIDAR-based digital elevation models show that charcoal hearths occur in a high density in many large forest areas throughout Brandenburg. In the areas studied so far, up to almost 3\% of the soil surface were found to be affected by the remains of historic hearths. First analyses of soil physical properties indicate differences in the infiltration characteristics of hearth site soils and undisturbed forest soils: Hood infiltrometer measurements show a very high spatial variability of hydraulic conductivity for hearth site soils, and water-drop-penetration-time tests reflect extremely high hydrophobicity of the technogenic layer on the sites. Results of dye tracer experiment show considerably strong preferential flow and therefore a higher spatial variability of soil wetness below the hearth remains. Overall, our first results therefore indicate that the legacy effects of historic charcoal production might significantly affect overall site conditions in forest areas with a high density of charcoal hearth remains.}, language = {en} } @inproceedings{HirschSchneiderRaabetal., author = {Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas and Ouimet, William and Dethier, David}, title = {Late Holocene biochar enrichment in soils - implications of an anthropogenic legacy for ecosystems}, series = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, booktitle = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, editor = {Schwab, Markus and Błaszkiewicz, Mirek and Raab, Thomas and Wilmking, Martin and Brauer, Achim}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-17037}, pages = {79 -- 81}, language = {en} } @inproceedings{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Dye tracer visualization of infiltration patterns in soils on historic charcoal hearth sites}, series = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, booktitle = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, editor = {Schwab, Markus and Błaszkiewicz, Mirek and Raab, Thomas and Wilmking, Martin and Brauer, Achim}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-17037}, pages = {150 -- 151}, language = {en} } @inproceedings{SchneiderHirschWechleretal., author = {Schneider, Anna and Hirsch, Florian and Wechler, Klaus-Peter and Raab, Alexandra and Raab, Thomas}, title = {Mapping a palaeosurface and archaeological site location in an anthropogenic drift sand area}, series = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, booktitle = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, editor = {Schwab, Markus and Błaszkiewicz, Mirek and Raab, Thomas and Wilmking, Martin and Brauer, Achim}, doi = {10.2312/GFZ.b103-17037}, pages = {152 -- 154}, language = {en} } @inproceedings{SchneiderRaabHirschetal., author = {Schneider, Anna and Raab, Alexandra and Hirsch, Florian and Bonhage, Alexander and Raab, Thomas}, title = {Assessing the legacies of historical charcoal production in Brandenburg}, series = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, booktitle = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, editor = {Schwab, Markus and Błaszkiewicz, Mirek and Raab, Thomas and Wilmking, Martin and Brauer, Achim}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-17037}, pages = {155 -- 156}, language = {en} } @inproceedings{HirschMaatenTheunissenMaatenetal., author = {Hirsch, Florian and Maaten-Theunissen, Marieke van der and Maaten, Ernst van der and Schneider, Marcus and Bauriegel, Albrecht and Raab, Alexandra and Raab, Thomas}, title = {Soil physics and chemistry at two medieval ridge and furrow sites in northeastern Germany}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Bodenkundlich-geomorphologische Untersuchung von Meilerpl{\"a}tzen um Weiherhammer}, series = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, volume = {12}, journal = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, issn = {1617-4461}, pages = {433 -- 448}, language = {de} } @misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Dye Tracer Visualization of Infiltration Patterns in Soils on Relict Charcoal Hearths}, series = {Frontiers in Environmental Sciences}, volume = {6}, journal = {Frontiers in Environmental Sciences}, doi = {doi.org/10.3389/fenvs.2018.00143}, pages = {1 -- 14}, language = {en} } @misc{HirschRaabOuimetetal., author = {Hirsch, Florian and Raab, Thomas and Ouimet, William and Dethier, David and Schneider, Anna and Raab, Alexandra}, title = {Soils on Historic Charcoal Hearths: Terminology and Chemical Properties}, series = {Soil Science Society of America, International Soils Meeting, Soils Across Latitudes, San Diego 2019}, journal = {Soil Science Society of America, International Soils Meeting, Soils Across Latitudes, San Diego 2019}, language = {en} } @misc{DonovanSchneiderHirschetal., author = {Donovan, Sally and Schneider, Anna and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Thermal conductivity of charcoal-richsoils-preliminary results from a study on relict charcoal hearth (RCH) sites from Germany and the USA}, series = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, journal = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, address = {Katlenburg-Lindau}, pages = {1}, language = {en} } @misc{BonhageMykhailovaHirschetal., author = {Bonhage, Alexander and Mykhailova, Larysa and Hirsch, Florian and Schneider, Anna and Raab, Thomas and Fischer, Thomas and Raab, Alexandra and Donovan, Sally and Ouimet, William}, title = {Effects of historical charcoal burning on soil landscapes in West Connecticut - Quantifying pyrogenic and organic soil carbon content of Technosols by FTIR analysis}, series = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, journal = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, address = {Katlenburg-Lindau}, language = {en} } @misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Thomas and Raab, Alexandra}, title = {The temperature regime of a charcoal-enriched land use legacy soil}, series = {Soil Science Society of America Journal}, volume = {83}, journal = {Soil Science Society of America Journal}, number = {3}, issn = {1435-0661}, doi = {10.2136/sssaj2018.12.0483}, pages = {565 -- 574}, language = {en} } @misc{SchneiderHirschBonhageetal., author = {Schneider, Anna and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Verbreitung und Eigenschaften von Meilerb{\"o}den in Brandenburg}, series = {Erfassung und Bewertung von vorindustriellen Meilerstandorten - Workshop 19. Februar 2019}, journal = {Erfassung und Bewertung von vorindustriellen Meilerstandorten - Workshop 19. Februar 2019}, editor = {Raab, Thomas and Raab, Alexandra and Schopper, Franz}, publisher = {Brandenburgische Technische Universit{\"a}t Cottbus - Senftenberg, Fachgebiet Geopedologie und Landschaftsentwicklung}, address = {Cottbus}, doi = {10.26127/BTUOpen-4817}, pages = {23 -- 42}, language = {de} } @misc{BonhageRaabRaabetal., author = {Bonhage, Alexander and Raab, Thomas and Raab, Alexandra and Schneider, Anna and Ramezany, Shaghayegh and Ouimet, William}, title = {Pyrogenic carbon in temperate forests - long-lasting impact of historical charcoal production on soils and ecosystems}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-8312}, abstract = {Pre- and early industrial charcoal production has left a striking legacy effect on today's soil landscapes in many forests of Central Europe and the North Eastern USA. Charcoaling in upright standing hearths (also called kilns) resulted in distinct circular micro relief structures, easily identifiable today in the field and on high resolution LiDAR-based digital elevation maps. Soils on these sites are characterized by one or multiple layers of decimetre thick charcoal rich substrate, which makes them Spolic Technosols according to the WRB soil classification. The focus of research on these sites increasingly deals with the difference of their soil physical and chemical properties in relation to unaffected forest soils and the potential implications for changes in vegetation and faunal growth. The controlling factor thereby is the soils large content of charcoal in various particle sizes, ranging from fine dust to large chunks. Studies have repeatedly shown the soils significant increase in total organic- and pyrogenic carbon content. The increase in total carbon stocks is thereby not only caused by pyrogenic carbon, but also by an apparently increased accumulation of non-pyrogenic organic matter. Here we present the latest findings regarding the carbon contents of centennially old charcoal rich technogenic substrates, sampled as part of multiple research projects in Brandenburg, Germany and the Litchfield hills in North-western Connecticut, USA. A focus will be the determination of highly aromatic carbon by the molecular marker Benzene-polycarboxylic acid (BPCA) and its prediction by FTIR-MIR chemometric methods. We discuss the results on forest soil carbon stocks on a site specific to a landscape and regional scale. Furthermore, the potential to use these sites to study the long term effects of charcoal admixture to soils by wildfires or biochar application will be discussed.}, language = {en} } @misc{MalikBohrWistubaetal., author = {Malik, Ireneusz and Bohr, Marcin and Wistuba, Małgorzata and Raab, Thomas and Bonhage, Alexander and Verschoof-van der Vaart, Wouter and Raab, Alexandra and Woskowicz-Ślęzak, Beata}, title = {Multi-Period Ore Exploitation in Upper Silesia, Central Europe}, series = {Journal of Field Archaeology}, volume = {48}, journal = {Journal of Field Archaeology}, number = {5}, issn = {0093-4690}, doi = {10.1080/00934690.2023.2200583}, pages = {366 -- 379}, language = {en} } @misc{HirschRaabOuimetetal., author = {Hirsch, Florian and Raab, Thomas and Ouimet, William and Dethier, David and Schneider, Anna and Raab, Alexandra}, title = {Soils on historic charcoal hearths - terminology and chemical properties}, series = {Soil Science Society of America Journal : SSSAJ}, volume = {81}, journal = {Soil Science Society of America Journal : SSSAJ}, number = {6}, issn = {1435-0661}, doi = {10.2136/sssaj2017.02.0067}, pages = {1427 -- 1435}, abstract = {Historic charcoal hearth remains provide a unique archive of the long term interaction between biochar, soil development and plant growth. Charcoal as raw material was crucial for production of iron in iron works and hence numerous charcoal hearths can be found in the forests near historic iron works in Europe as well as the Eastern United States. Charcoal hearths are round to elliptical forms often around 10 m in diameter, and consist of several decimeter thick layers that contain charcoal fragments, ash, and burnt soil. We studied the soil chemistry of 24 charcoal hearths and compared them to the surrounding 'natural' soils in the northern Appalachians of northwestern Connecticut. The thickness of the topsoils on the charcoal hearths and their carbon content are remarkably higher than in the surrounding topsoils. The presence of residual products from charcoal production classifies the soils as Anthropic Udorthents (US Soil Taxonomy) or Spolic Technosols (Humic) according to the World Reference Base for Soil Resources. The widespread occurrence of charcoal hearth remains and their high spatial density in different ecosystems underlines their importance for further pedological research.}, language = {en} } @misc{HirschSchneiderBauriegeletal., author = {Hirsch, Florian and Schneider, Anna and Bauriegel, Albrecht and Raab, Alexandra and Raab, Thomas}, title = {Formation, Classification, and Properties of Soils at Two Relict Charcoal Hearth Sites in Brandenburg, Germany}, series = {Frontiers in Environmental Science}, volume = {6}, journal = {Frontiers in Environmental Science}, issn = {2296-665X}, doi = {10.3389/fenvs.2018.00094}, pages = {1 -- 15}, abstract = {Historical charcoal production can have significant effects on soil properties. We studied soils at former charcoal production sites (relict charcoal hearths, RCHs) and compared these soils with undisturbed soil next to the charcoal hearths and four typical soils on similar parent material located at distances between 10 and 70 km from the RCHs. In a landscape typical of the northern German lowland, we found Podsolige Braunerde [WRB: Brunic Arenosols (Protospodic)] outside of the RCHs and soils with a clearly different stratigraphy within the RCHs. The main feature of the soils at both of the studied RCHs is a heterogeneous, charcoal-bearing deposit that is ~30 cm thick. No indications of translocation or mineral transformation processes, which form distinct soil horizons after the deposition of anthropogenic material on the RCHs, are present. Except for the differences in color and total carbon content, the soil chemistry of the RCHs hardly differs from that of the soil outside of the charcoal hearth sites. The soil colors and magnetic susceptibility values strongly suggest that the RCH substrates and the underlying topsoil were affected by thermally induced transformation of iron (hydr-)oxides. Although the charring procedure normally requires ~2 weeks, the heating effect only reaches to a maximum depth of 8 cm into the buried soil below the charcoal hearths. The presence of reddish soil and an abrupt increase in magnetic susceptibility in the upper 2 cm of the soil below the charcoal hearths indicate the heat-induced transformation of iron (hydr-)oxides into maghemite. Brighter soil color and an increase in soil organic matter (SOM) in the lower parts of the buried topsoil demonstrate the combustion of SOM up to 5 cm depth below the RCH. According to the German Guidelines for Soil Mapping, the soils in the RCHs are classified as Regosols above Braunerde [WRB: Spolic Technosols (Arenic)]. However, because the anthropogenic features of these soil sediments are disregarded in the German Guidelines for Soil Mapping, we suggest adapting the "M" horizon to permit a jM horizon. Thus, the soils in the RCHs could be classified as Kolluviale Braunerde.}, language = {en} } @misc{BonhageMykhailovaHirschetal., author = {Bonhage, Alexander and Mykhailova, Larysa and Hirsch, Florian and Schneider, Anna and Raab, Thomas and Raab, Alexandra and Ouimet, William}, title = {FTIR-based inquiry on carbon in forest soil substrate enriched by aged biochar, West Connecticut, USA}, series = {Jahrestagung der Bodenkundlichen Gesellschaft der Schweiz und der Deutschen Bodenkundlichen Gesellschaft, Abstract-Band 2019}, journal = {Jahrestagung der Bodenkundlichen Gesellschaft der Schweiz und der Deutschen Bodenkundlichen Gesellschaft, Abstract-Band 2019}, pages = {S. 198}, abstract = {Relict charcoal hearths (RCHs) are sites of former charcoal production that are an increasingly well documented anthropogenic feature in forests of the temperate climate zone. However, the type and extent of a possible legacy effect from RCHs on soil physical and chemical properties is still largely unknown. In the Litchfield Hills in west Connecticut, RCH sites are located mainly on slopes and therefore differ in their architecture from lowland sites found in Europe. One of the striking characteristics of a RCH site regardless of its architecture is the enrichment of the soil with charcoal in varying particle sizes. In this study, we use chemical digestion coupled with a PLSR-model to quantify organic carbon and pyrogenic carbon in RCH substrate by MIR-DRIFT measurements. Furthermore, we analyse the quality of carbon compounds by MIR-DRIFT measurements on multiple grain size fractions to assess the post-burn enrichment of soil organic matter. Preliminary results show a markedly increase in organic and pyrogenic carbon in RCH substrates in relation to the natural forest soil. Also, our first results suggest that the enrichment of organic carbon is favoured on RCHsites. However, the causality between the enrichment of soil organic matter and site features remains open. Experiments using chemical extraction techniques on our samples hint at an increase of labile organic compounds and/or microbial biomass. This legacy effect of RCHs is however evident and further studies need to focus on how to address them.}, language = {de} } @misc{SchneiderBonhageRaabetal., author = {Schneider, Anna and Bonhage, Alexander and Raab, Alexandra and Hirsch, Florian and Raab, Thomas}, title = {Large-scale mapping of anthropogenic relief features—legacies of past forest use in two historical charcoal production areas in Germany}, series = {Geoarchaeology}, volume = {35}, journal = {Geoarchaeology}, number = {4}, issn = {1520-6548}, doi = {10.1002/gea.21782}, pages = {545 -- 561}, language = {en} } @misc{BonhageHirschSchneideretal., author = {Bonhage, Alexander and Hirsch, Florian and Schneider, Anna and Raab, Thomas and Raab, Alexandra and Ouimet, William and Drohan, Patrick J.}, title = {Effects of Historical Charcoal Burning on Soil Landscapes in West Connecticut, USA}, series = {Soil Science Society of America, International Soils Meeting, Soils Across Latitudes, San Diego 2019}, journal = {Soil Science Society of America, International Soils Meeting, Soils Across Latitudes, San Diego 2019}, language = {en} } @misc{RaabRaabBonhageetal., author = {Raab, Thomas and Raab, Alexandra and Bonhage, Alexander and Schneider, Anna and Hirsch, Florian and Birkhofer, Klaus and Drohan, Patrick J. and Wilmking, Martin and Kreyling, J{\"u}rgen and Malik, Ireneusz and Wistuba, Małgorzata and Maaten, Ernst van der and Maaten-Theunissen, Marieke van der and Urich, Tim}, title = {Do small landforms have large effects? A review on the legacies of pre-industrial charcoal burning}, series = {Geomorphology}, volume = {413}, journal = {Geomorphology}, issn = {0169-555X}, doi = {10.1016/j.geomorph.2022.108332}, pages = {16}, abstract = {Relict charcoal hearths (RCHs) are small, anthropogenic landforms resulting from past charcoal burning and reaching significant land coverage in pre-industrial mining areas. We review three coupled legacies linked by RCH development: (i) a landscape-scale geomorphic effect, (ii) a unique soil fingerprint, and (iii) an evolving novel ecosystem. The history and technique of charcoal production are described to clarify legacy effects. Applying a recently presented morpho-genetic catalogue is useful for classified mapping of RCH findings. The RCH numbers and calculated RCH densities per study region vary greatly and impose uncertainties due to insufficient methods causing over- or underestimations. Areas with high RCH densities between 50 and 500 RCH/km2 seem reasonable. Machine learning-based remote sensing techniques are promising approaches with which to better assess the full scale of charcoal burning legacies. RCH soil properties feature dark charcoal-rich technogenic substrate layers classified as Auh horizons according to the World Reference Base with significantly increased C contents. These Auh horizons can also exhibit specific physical and chemical properties, such as relatively low bulk density, high porosity, high plant available water content, low thermal conductivity and differences in cation exchange capacity or nutrient status. However, relevant studies are rare, and thus, the effects may differ by study region. Regarding vegetation, there seem to be four main effects: changes in forest structure, species composition, recruitment pattern and productivity. The number of studies on this issue is, however, also very limited. Even fewer studies have examined the soil fauna in RCHs; thus, the reported effects cannot be used to draw general conclusions. Notably, RCH research has made considerable progress in the last five years, especially in the Light Detection and Ranging-based mapping of these small landforms and identification of RCH-specific soil properties, but ecological legacies are not well understood; thus, more interdisciplinary and integrative studies are needed.}, language = {en} } @inproceedings{RaabRaabSchneideretal., author = {Raab, Thomas and Raab, Alexandra and Schneider, Anna and Hirsch, Florian and Takla, Melanie and Nicolay, Alexander and Bonhage, Alexander and Bauriegel, Albrecht and R{\"o}sler, Horst}, title = {Landnutzungsgeschichte und historische Landschaftsentwicklung in der Niederlausitz - Neue Befunde und aktuelle Forschung}, series = {Jahrestagung Arbeitskreis Geoarch{\"a}ologie, T{\"u}bingen, 4. Mai bis 7. Mai 2016}, booktitle = {Jahrestagung Arbeitskreis Geoarch{\"a}ologie, T{\"u}bingen, 4. Mai bis 7. Mai 2016}, abstract = {Seit 2010 untersucht eine interdisziplin{\"a}re Forschergruppe der BTU, des BLDAM und des LBGR die Landnutzungsgeschichte sowie die nat{\"u}rliche und anthropogen induzierte Landschaftsentwicklung in der Niederlausitz, Brandenburg. Systematische arch{\"a}ologische Grabungen des BLDAM im Vorfeld der laufenden Tagebaue sind eine wichtige Grundlage f{\"u}r geopedologische Untersuchungen. Die Arbeiten hatten zun{\"a}chst ihren r{\"a}umlichen Schwerpunkt in den Braunkohletagebauen nord{\"o}stlich von Cottbus (Tgb. Cottbus Nord, Tgb. J{\"a}nschwalde) und wurden dann ausgedehnt auf weitere Forstfl{\"a}chen n{\"o}rdlich von Peitz. Wir geben einen {\"U}berblick {\"u}ber die wichtigsten Erkenntnisse der letzten Jahre, pr{\"a}sentieren aktuelle Ergebnisse und zeigen zuk{\"u}nftige Forschungsfelder auf. Im Tagebau J{\"a}nschwalde sind zwischenzeitlich mehr als 1000 Relikte von Holzkohlmeilern (HKM) als Zeugen einer intensiven historischen Holznutzung arch{\"a}ologisch dokumentiert. Mit Stand Januar 2016 liegen Dendroalter von 64 HKM vor. Die Alter schwanken zwischen dem ausgehenden 16. Jahrhundert und der Mitte des 19. Jahrhunderts, was in etwa dem Betriebszeitraum des H{\"u}ttenwerks in Peitz entspricht. Die Mehrzahl der Meiler datiert auf den Beginn des 18. Jahrhunderts. Weitere Hinterlassenschaften der historischen Landnutzung sind u.a. W{\"o}lb{\"a}cker und begrabene Ackerb{\"o}den. Fossile B{\"o}den und ehemalige Landoberfl{\"a}chen sind stellenweise mit {\"a}olischen Sedimenten {\"u}berdeckt. 14C- und OSL-Datierungen an diesen B{\"o}den und Sedimenten lassen auf eine Intensivierung der {\"a}olischen Aktivit{\"a}t zur slawischen Zeit und im Deutschen Mittelalter schließen. Einige Relikte von HKM sind mit Sand {\"u}berweht worden, und an einer Stelle konnte das Alter dieser {\"a}olischen Sedimentation mittels Dendrodatierung des begrabenen Meilers auf1850 oder j{\"u}nger bestimmt werden. Allerdings stellt dies die Ausnahme dar. Der weitaus gr{\"o}ßere Teil der HKM-Relikte liegt direkt an der Oberfl{\"a}che und ist nicht begraben, was auf eine sehr geringe Winderosion in der Neuzeit schließen l{\"a}sst. Seit 2015 konnte im Rahmen des DFG-Projekts „R{\"a}umliche und zeitliche Dimension der historischen K{\"o}hlerei im Tauerschen Forst (Niederlausitz, Brandenburg). Ein Beitrag zur Kulturlandschaftsentwicklung des Norddeutschen Tieflands" (Az RA 1129/3-1; RA 931/6-1) ein weiteres Gebiet mit hoher HKM-Dichte untersucht werden. Erste Auswertungen der LiDAR-Daten ergeben eine Anzahl von 4449 ehemaligen Meilerstandorten im Tauerschen Forst. 26 Meilerstellen sind beprobt, die Dendroalter hierzu sind in Bearbeitung. Ebenfalls in j{\"u}ngerer Zeit fanden Untersuchungen zur Verbreitung von HKM-Relikten f{\"u}r das gesamte Land Brandenburg statt. Mit Hilfe eines bin{\"a}ren Modells wurden Gebiete mit hoher Wahrscheinlichkeit von HKM-Standorten detektiert. Im Rahmen des im November 2016 beginnenden DFG-Projekts „Die historische K{\"o}hlerei in Brandenburg - Analyse der r{\"a}umlichen Dimension und der Effekte auf bodenhydraulische Eigenschaften" (SCHN 1349/1-1) sollen nun neben der Verbreitung der historischen K{\"o}hlerei auch bodenrelevante Auswirkungen beschrieben und bewertet werden.}, language = {de} } @inproceedings{RaabRaabSchneideretal., author = {Raab, Alexandra and Raab, Thomas and Schneider, Anna and Hirsch, Florian and Takla, Melanie and Nicolay, Alexander and Bonhage, Alexander and M{\"u}ller, Frank and Heußner, Karl-Uwe and R{\"o}sler, Horst}, title = {Reconstructing anthropogenic landscape transformation in the surroundings of the ironwork Peitz (SE Brandenburg, Germany) - 16th to mid-19th centuries}, series = {4th International Landscape Archaeology Conference, Uppsala, 22nd - 25th August 2016}, booktitle = {4th International Landscape Archaeology Conference, Uppsala, 22nd - 25th August 2016}, publisher = {Department of archaeology and ancient history, Uppsala university,}, address = {Uppsala}, pages = {S. 152}, abstract = {Various sources provide information about land use history and landscape transformation. For a variety of reasons, the quality of information differs and is often discontinuous or incomplete. In this interdisciplinary study we take advantage of comprehensive archaeological data gathered by large-scale excavations that were necessary because of opencast lignite mining in Lusatia, Brandenburg, Germany. By using a GIS we integrate these archaeological findings with results from archival and literature studies, from historical maps, from landforms and soils as well as from analyses of shaded-relief maps derived from up-to-date LiDAR data. The long-term aim is to develop a palaeoenvironmental model and thus to reconstruct landscape changes caused by human activities. The focus of the study is the Peitz ironwork in SE Brandenburg, which was a large consumer of commodities for about 300 years. During the time it operated, extensive transformations are supposed to have affected the landscape in the vicinity because of wood consumption and especially charcoal production. Digital datasets about forested areas for different timespans reconstructed from historical maps were made available. In combination with dendrochronological dating of charred trees, the spatiotemporal dimension of charcoal kilns was determined. Also, sites of former bog iron ore mining could be identified. Moreover, the different sources contain further information about other forms of land uses such as agriculture, pastoralism and even viticulture. In conclusion we can highlight that the mosaic of past land use systems is different from the modern structure but that major changes in the forests have been retained.}, language = {en} } @misc{RaabBonhageVerschoofvanderVaartetal., author = {Raab, Thomas and Bonhage, Alexander and Verschoof-van der Vaart, Wouter and Malik, Ireneusz and Raab, Alexandra and Schneider, Anna and Chauhan, Jai Singh and Thekkethala, Jeenus Joby}, title = {Soils on mining relicts in Upper Silesia, Poland - first results from the Mala Panew River catchment and the UNESCO heritage site Tarnowskie G{\´o}ry}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-969}, abstract = {The mining region of Upper Silesia has a long tradition with international significance. In 2017, the historic silver mine in Tarnowsky Gory was recognized as a UNESCO World Heritage Site. With the mining of galena (PbS), the region developed into one of the most important industrial centers in Central Europe in the 16th century. In addition to the underground galleries, the historical mining has left thousands of mining shafts as small relief forms, which have not been systematically investigated so far. Partly the mining shafts are associated with Relict Charcoal Hearths (RCH), another small form which is a result of charcoal production. In the Mala Panew River valley, north of Tarnowsky Gory, several tens of thousands of these RCH are found, which could be mapped by LiDAR in recent years. More detailed pedological investigations, which would allow a systematic comparison with other known RCH sites, are missing so far. Within the framework of a Polish-German cooperation project, we started in 2021 to investigate the mining shafts and the RCH in Tarnowsky Gory and in the Mala Panew River valley from a pedological-sedimentological point of view. At the RCH sites on the Mala Panew River, we focused on the following questions: How was the soil stratigraphy changed by the RCH construction? What are main processes of soil development before and after RCH construction? What was the role of the pits surrounding the RCH? How do the sites differ from the RCHs at Tarnowsky Gory especially with respect to soil properties and soil genesis? In Tarnowsky Gory, where a RCH was excavated directly next to a mining shaft, the following questions were in focus: How did the mining activity change soil distribution and soil properties? What are main processes of soil development on the different parts? What is the origin of the pit infill? What is the origin of the shaft rim deposits? Our work program included the construction of excavator trenches across the mining remains, construction, description and sampling of soil profiles along the trenches, schematic drawing of the soil stratigraphy, and laboratory analyses for the determination of texture, Munsell color, pH (CaCl2, H20), CaCO3 content, Ctotal \& Ntotal and total elements by FPXRF. We present the first results of the ongoing investigations.}, language = {en} } @misc{BonhageHirschSchneideretal., author = {Bonhage, Alexander and Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas and Donovan, Sally}, title = {Long term anthropogenic enrichment of soil organic matter stocks in forest soils - detecting a legacy of historical charcoal production}, series = {Forest Ecology and Management}, volume = {459}, journal = {Forest Ecology and Management}, issn = {0378-1127}, doi = {10.1016/j.foreco.2019.117814}, pages = {11}, abstract = {Recent findings of several thousand relict charcoal hearths (RCHs) in the Tauer Forest (Brandenburg, Germany) raise questions about the legacy effects of historical charcoal production on soil properties. RCH sites are characterized by the admixture of charcoal fragments to the natural forest soil, constituting an anthropogenic addition of carbon. Dendrochronological dating of large charcoal pieces has identified RCH ages ranging from 1709 AD to 1823 AD for a subarea in the Tauer Forest, which allows for assessing century old effects of charcoal application on forest soils. We measured the geometry and soil organic matter (SOM) content of 20 RCH sites in a selected part of the forest. The results provide a basis for estimating RCH SOM stocks on a 40-ha forest plot with 120 RCH sites. We also assessed the accuracy of RCH mapping based on digital elevation models (DEMs) with results from a ground survey. Over 50 \% of sites were not detected by the DEM-based mapping. In the range of statistical uncertainties, RCHs add between 18 \% and 32 \% of SOM to the stock of the natural forest soil in the study area. This equals an additional 4.9 - 8.9 Mg of carbon per hectare of forest soil. These substantial amounts of SOM are so far not recognized by any survey or forest soil SOM inventories. Considering recent studies, which uncovered tens- and hundreds- of thousands of RCHs throughout Europe and the USA, we conclude that further knowledge of RCH SOM is important for quantifying anthropogenic SOM stocks on a global scale.}, language = {en} } @misc{HirschRaabRaabetal., author = {Hirsch, Florian and Raab, Thomas and Raab, Alexandra and Schneider, Anna and Bonhage, Alexander and Schneider, Marcus and Bauriegel, Albrecht}, title = {Quaternary and geoarcheology in Lower Lusatia}, series = {DEUQUA Special Publications}, volume = {4}, journal = {DEUQUA Special Publications}, issn = {2625-8137}, doi = {10.5194/deuquasp-4-59-2022}, pages = {59 -- 71}, abstract = {Open-cast lignite mines in Lower Lusatia provide unique insights into human-induced environmental changes in the Northern European Lowland and improve our understanding of Quaternary landscape dynamics. The excursion will focus on soils and sediments of Late Pleistocene and Holocene age that have been modified by land use since the Slavic Middle Ages. In the vicinity of the open-cast mine J{\"a}nschwalde and in the Tauer forest north of Cottbus characteristic remains of historical charcoal production, a ridge-and-furrow system and late Quaternary rubification in soils are presented.}, language = {en} } @misc{RaabBonhageSchneideretal., author = {Raab, Alexandra and Bonhage, Alexander and Schneider, Anna and Raab, Thomas and R{\"o}sler, Horst and Heußner, Karl-Uwe and Hirsch, Florian}, title = {Spatial distribution of relict charcoal hearths in the former royal forest district Tauer (SE Brandenburg, Germany)}, series = {Quaternary International}, volume = {Vol. 511}, journal = {Quaternary International}, issn = {1040-6182}, doi = {10.1016/j.quaint.2017.07.022}, pages = {153 -- 165}, abstract = {Historical charcoal production has long been an unconsidered type of forest utilization in lowland areas. The archaeological discovery of a large charcoal burning area in the forefield of the active opencast lignite mine J€anschwalde in SE Brandenburg (North German Lowlands) has highlighted the need for multidisciplinary research in the study of the dimensions of historical charcoal burning. The charcoal produced in our study area, the former royal forest district Tauer, provided energy for the nearby Peitz ironworks during its operation from the mid-16th to the mid-19th century. Here, we aimed to record the amount, size and distribution of relict charcoal hearths (RCHs) to examine their context with respect to the ironworks and to better understand the potential impacts on late Quaternary landscape change. The applied methods combined archaeological research with shaded-relief mapping of RCHs. To evaluate the detection success of RCHs in the shaded-relief maps (SRMs), we compared the results with the results from specific archaeological surveys and conventional forest site mapping. Furthermore, we analyzed our dataset with descriptive, comparable and spatial statistics. Additionally, dendrochronological dating of charcoal fragments from selected RCHs was used to investigate the temporal relationships among the RCHs. Approximately 6000 circular RCHs were manually digitally identified in the SRMs of the 109-km2 evaluable area. However, ground truthing showed that the shaded-relief maps could not completely capture all RCHs in our study area due to local conditions. At the regional scale, two focus areas with high RCH site densities were found. Statistical analysis revealed that the diameters of the RCHs range widely from 4 to 30.5 m. Spatial statistics were applied to the RCH diameters to aggregate areas with larger or smaller RCHs. At the small scale, no systematic arrangement of RCHs was obvious in the SRMs. Dendrochronological dating of selected RCHs lying close together could not detect significant spatiotemporal relationships or patterns. The dating results also showed that some areas have been preferentially used for charcoal production for over 300 years. Due to the homogeneity of the physiogeographical location factors, we assume that these factors are not superficially responsible for site selection. Instead, economic location factors and contemporary regulations are more likely responsible for the distribution of RCHs.}, language = {en} } @misc{BonhageHirschRaabetal., author = {Bonhage, Alexander and Hirsch, Florian and Raab, Thomas and Schneider, Anna and Raab, Alexandra and Ouimet, William}, title = {Characteristics of small anthropogenic landforms resulting from historical charcoal production in western Connecticut, USA}, series = {Catena}, volume = {195}, journal = {Catena}, issn = {0341-8162}, doi = {10.1016/j.catena.2020.104896}, pages = {14}, language = {en} } @misc{HirschSchneiderBonhageetal., author = {Hirsch, Florian and Schneider, Anna and Bonhage, Alexander and Raab, Alexandra and Drohan, Patrick J. and Raab, Thomas}, title = {An initiative for a morphologic-genetic catalog of relict charcoal hearths from Central Europe}, series = {Geoarchaeology}, volume = {35}, journal = {Geoarchaeology}, number = {6}, issn = {1520-6548}, doi = {10.1002/gea.21799}, pages = {974 -- 983}, language = {en} } @misc{SchneiderHirschBonhageetal., author = {Schneider, Anna and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {The soil moisture regime of charcoal-enriched land use legacy sites}, series = {Geoderma}, volume = {366}, journal = {Geoderma}, issn = {0016-7061}, doi = {10.1016/j.geoderma.2020.114241}, pages = {15}, language = {en} } @misc{SchneiderBonhageHirschetal., author = {Schneider, Anna and Bonhage, Alexander and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Hot spots and hot zones of soil organic matter in forests as a legacy of historical charcoal production}, series = {Forest Ecology and Management}, volume = {504}, journal = {Forest Ecology and Management}, issn = {1872-7042}, doi = {10.1016/j.foreco.2021.119846}, abstract = {Human land use often leads to distinct modifications of soils within small, clearly delimited areas. Legacy effects of past land use are also abundant in recent forest areas, but are hardly considered in ecosystem assessment and soil mapping. The soils on relict charcoal hearths (RCHs) are a widespread example for such land use legacy soils in forests. Soils on RCHs differ clearly from surrounding forest soils in their stratigraphy and properties, and are most prominently characterized by a technogenic substrate layer with high contents of charcoal and thus soil organic matter (SOM). Although RCH soils can clearly contribute to the SOM stocks of forest soils, their relevance on the landscape scale has hardly been quantified. In this paper we analyze and discuss the distribution and effects of RCH soils across scales for forests in the state of Brandenburg, Germany, with a focus on SOM stocks. Our analysis is based on a large-scale mapping of RCHs from digital elevation models (DEMs), combined with a linear regression model of SOM stocks in RCH soils. The spatial distribution of RCH soils in the study region has a scale dependent heterogeneity. The large-scale variation in site densities is related to the concentration of charcoal production to specific forest areas while the small-scale variation is related to the irregular distribution of single RCHs within the charcoal production fields. Up to 1.5 \% of the surface are covered by RCH soils in the forest areas within the study region. The results also show that RCHs can significantly contribute to the SOM stocks of forests, even where they cover only a small fraction of the soil surface, with up to 18 \% additional SOM for forest areas. Because of the heterogeneous distribution of RCHs, the SOM stock additions depend on the scale of observation. Our results suggest that RCH SOM additions can be overestimated when sites in small areas (< 1 km²) are analyzed; and that characteristic spatial concentration patterns of RCHs are even observable when values are aggregated to large areas (25 km² and more). Aggregating effects to irregularly-sized forest administrative units resulted in maps that well represent the spatial distribution of RCH soils and SOM. The study highlights that considering land use legacy effects can be relevant for the results of soil mapping and inventories; and that prospecting and mapping land use legacies from DEMs can contribute to improving such approaches.}, language = {en} } @misc{BonhageEltaherRaabetal., author = {Bonhage, Alexander and Eltaher, Mahmoud and Raab, Thomas and Breuß, Michael and Raab, Alexandra and Schneider, Anna}, title = {A modified Mask region-based convolutional neural network approach for the automated detection of archaeological sites on high-resolution light detection and ranging-derived digital elevation models in the North German Lowland}, series = {Archaeological Prospection}, volume = {28}, journal = {Archaeological Prospection}, number = {2}, issn = {1099-0763}, doi = {10.1002/arp.1806}, pages = {177 -- 186}, language = {en} } @misc{BonhageRaabSchneideretal., author = {Bonhage, Alexander and Raab, Thomas and Schneider, Anna and Fischer, Thomas and Ramezany, Shaghayegh and Ouimet, William and Raab, Alexandra and Hirsch, Florian}, title = {Vertical SOC distribution and aromatic carbon in centuries old charcoal-rich Technosols}, series = {European Journal of Soil Science}, volume = {73}, journal = {European Journal of Soil Science}, number = {4}, doi = {10.1111/ejss.13293}, pages = {1 -- 16}, abstract = {Charcoal-rich Technosols on century-old relict charcoal hearths (RCHs) are the subject of ongoing research regarding potential legacy effects that result from historic charcoal production and subsequent charcoal amendments on forest soil properties and forest ecosystems today. RCHs consist mostly of Auh horizons that are substantially enriched in soil organic carbon (SOC), of which the largest part seems to be of pyrogenic origin (PyC). However, the reported range of SOC and PyC contents in RCH soil also suggests that they are enriched in nonpyrogenic SOC. RCH soils are discussed as potential benchmarks for the long-term influence of biochar amendment and the post-wildfire influences on soil properties. In this study, we utilised a large soil sample dataset (n = 1245) from 52 RCH sites in north-western Connecticut, USA, to quantify SOC contents by total element analysis. The contents of condensed highly aromatic carbon as a proxy for black carbon (BC) were predicted by using a modified benzene polycarboxylated acid (BPCA) marker method in combination with diffuse reflectance infrared Fourier transform (DRIFT) spectroscopy-based partial least square regression (r2 = 0.89). A high vertical spatial sampling resolution allowed the identification of soil organic matter (SOM) enrichment and translocation processes. The results show an average 75\% and 1862\% increase in TOC and BPCA-derived carbon, respectively, for technogenic Auh horizons compared to reference soils. In addition to an increase in aromatic properties, increased carboxylic properties of the RCH SOC suggest self-humification effects of degrading charcoal and thereby the continuing formation of leachable aromatic carbon compounds, which could have effects on pedogenic processes in buried soils. Indeed, we show BPCA-derived carbon concentrations in intermediate technogenic Cu horizons and buried top/subsoils that suggest vertical translocation of highly aromatic carbon originating in RCH Auh horizons. Topmost Auh horizons showed a gradual decrease in total organic carbon (TOC) contents with increasing depth, suggesting accumulation of recent, non-pyrogenic SOM. Lower aliphatic absorptions in RCH soil spectra suggest different SOM turnover dynamics compared to reference soils. Furthermore, studied RCH soils featured additional TOC enrichment, which cannot be fully explained now.}, language = {en} } @inproceedings{SchneiderRaabBonhageetal., author = {Schneider, Anna and Raab, Alexandra and Bonhage, Alexander and Hirsch, Florian and Raab, Thomas}, title = {Legacies of historic charcoal production in Brandenburg, Germany}, series = {Conference booklet, 5th International Landscape Archaeology Conference, 17th-20th September 2018 Newcastle and Durham, UK}, booktitle = {Conference booklet, 5th International Landscape Archaeology Conference, 17th-20th September 2018 Newcastle and Durham, UK}, pages = {S. 214}, language = {en} } @misc{RaabRaabBonhageetal., author = {Raab, Alexandra and Raab, Thomas and Bonhage, Alexander and Schneider, Anna and Verschoof-van der Vaart, Wouter and Bauriegel, Albrecht}, title = {Geomorphology of the Schwarze Elster Valley (Southwest Brandenburg, Germany) at the Bronze Age barrow cemetery Schweinert - Findings from the 2023 research campaign}, series = {DGGM Meeting 2023 Conference proceedings 04.-06.10.2023, RWTH Aachen}, journal = {DGGM Meeting 2023 Conference proceedings 04.-06.10.2023, RWTH Aachen}, pages = {S. 60}, language = {de} } @misc{RaabRaabBonhageetal., author = {Raab, Thomas and Raab, Alexandra and Bonhage, Alexander and Schneider, Anna and Drohan, Patrick J. and Wistuba, Małgorzata and Malik, Ireneusz and Verschoof-van der Vaart, Wouter}, title = {Small anthropogenic landforms from past land use - what have we (already) learned and what do we (still) want to know}, series = {DGGM Meeting 2023 Conference proceedings 04.-06.10.2023, RWTH Aachen}, journal = {DGGM Meeting 2023 Conference proceedings 04.-06.10.2023, RWTH Aachen}, pages = {S. 61}, language = {de} } @misc{HirschSchneiderNicolayetal., author = {Hirsch, Florian and Schneider, Anna and Nicolay, Alexander and Blaszkiewicz, Miroslaw and Kordowski, Jarosław and Noryskiewicz, Agnieszka M. and Tyszkowski, Sebastian and Raab, Alexandra and Raab, Thomas}, title = {Late Quaternary landscape development at the margin of the Pomeranian phase (MIS 2) near Lake Wygonin (Northern Poland)}, series = {Catena}, volume = {124}, journal = {Catena}, issn = {0341-8162}, doi = {10.1016/j.catena.2014.08.018}, pages = {28 -- 44}, abstract = {In Central Europe, Late Quaternary landscapes experienced multiple phases of geomorphologic activity. In this study,we used a combined geomorphological, pedological, sedimentological and palynological approach to characterize landscape development after the Last Glacial Maximum (LGM) near Lake Wygonin in Northern Poland. The pedostratigraphical findings from soil pits and drillings were extrapolated using ground-penetrating radar (GPR) and electric resistivity tomography (ERT). During the Pomeranian phase, glacial and fluvioglacial processes dominated the landscape near Lake Wygonin. At the end of the glacial period, periglacial processes became relevant and caused the formation of ventifacts and coversands containing coated sand grains. At approximately 15,290-14,800 cal yr BP, a small pond formed in a kettle hole (profile BWI2). The lacustrine sediments lack eolian sand components and therefore indicate the decline of eolian processes during that time. The increase of Juniperus and rock-rose (Helianthemum) in the pollen diagram is a prominent marker of the Younger Dryas. At the end of the Younger Dryas, a partial reshaping of the landscape is indicated by abundant charcoal fragments in disturbed lake sediments. No geomorphologic activity since the beginning of the Holocene is documented in the terrestrial and wetland archives. The anthropogenic impact is reflected in the pollen diagram by the occurrence of rye pollen grains (Secale cereale) and translocated soil sediments dated to 1560-1410 cal yr BP, proving agricultural use of the immediate vicinity. With the onset of land use, gully incision and the accumulation of colluvial fans reshaped the landscape locally. Since 540-460 cal yr BP, further gully incision in the steep forest tracks has been associated with the intensification of forestry. Outside of the gully catchments, the weakly podzolized Rubic Brunic Arenosols show no features of Holocene soil erosion.}, language = {en} } @inproceedings{SchneiderRaabBonhageetal., author = {Schneider, Anna and Raab, Alexandra and Bonhage, Alexander and Hirsch, Florian and Raab, Thomas}, title = {Relikte der historischen K{\"o}hlerei in Brandenburg}, series = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, booktitle = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, editor = {Berg, Stefanie and Eckmeier, Eileen and Linzen, Sven and Werther, Lukas and Zielhofer, Christoph}, publisher = {Friedrich-Schiller-Universit{\"a}t Jena [u.a.]}, address = {Jena [u.a.]}, doi = {10.22032/dbt.34521}, pages = {S. 28}, language = {de} } @inproceedings{HirschMaatenTheunissenMaatenetal., author = {Hirsch, Florian and Maaten-Theunissen, Marieke van der and Maaten, Ernst van der and Schneider, Marcus and Schneider, Anna and Raab, Alexandra and Raab, Thomas}, title = {Pedology and effects on vegetation at two medieval ridge and furrow sites in northeastern Germany}, series = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, booktitle = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, editor = {Berg, Stefanie and Eckmeier, Eileen and Linzen, Sven and Werther, Lukas and Zielhofer, Christoph}, publisher = {Friedrich-Schiller-Universit{\"a}t Jena [u.a.]}, address = {Jena [u.a.]}, doi = {10.22032/dbt.34521}, pages = {S. 18}, language = {en} } @inproceedings{BonhageHirschSchneideretal., author = {Bonhage, Alexander and Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas}, title = {Multiproxy analysis of a relict charcoal hearth field in Brandenburg (Germany)}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{SchneiderRaabBonhageetal., author = {Schneider, Anna and Raab, Alexandra and Bonhage, Alexander and Hirsch, Florian and Raab, Thomas}, title = {Legacies of historic charcoal production in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{BonhageHirschSchneideretal., author = {Bonhage, Alexander and Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas}, title = {Multiproxy analysis of a relict charcoal hearth field in Brandenburg (Germany)}, series = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, booktitle = {Jahrestagung des Arbeitskreises Geoarch{\"a}ologie, M{\"u}nchen, 2018}, editor = {Berg, Stefanie and Eckmeier, Eileen and Linzen, Sven and Werther, Lukas and Zielhofer, Christoph}, publisher = {Friedrich-Schiller-Universit{\"a}t Jena [u.a.]}, address = {Jena [u.a.]}, doi = {10.22032/dbt.34521}, pages = {S. 27}, language = {en} } @inproceedings{SchneiderBonhageHirschetal., author = {Schneider, Anna and Bonhage, Alexander and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Spatial and temporal variability of soil physical properties on legacies of historic charcoal production}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {The spatial variability of soil physical properties on the landscape scale is often increased by anthropogenic land occupation, not only by current land use but also through the legacies of past land use systems. The remains of historic charcoal hearts are an example for such a disturbance of the soil landscape by former forestry. Such relict charcoal hearths (RCH) exhibit a clearly altered soil stratigraphy, most prominently characterized by a technogenic substrate layer on the soil surface, and their soil physical properties can considerably differ from those of surrounding forest soils. The aim of our study is to characterize the soil water and temperature regime on RHC in a pre-industrial charcoal production area in Brandenburg, Germany, as compared with the surrounding sandy forest soils. Soil properties were analyzed in profiles on and around hearth sites and are monitored in a sensor transect equipped with soil moisture sensors and pF-meters. Results of soil sample analyses show differences in density and porosity between the RCH soils and surrounding forest soils, not only in the technogenic layer but also in the buried soil layers on hearth sites. The soil water characteristic curves determined in the laboratory indicate a modified pore size distribution and lower plant available water contents in the RCH soils. Preliminary results of the ongoing soil water monitoring, however, show increased soil wetness in the RCH soils, along with lower soil moisture tensions. Furthermore, the measurements show higher variations of soil temperature in RCH soils. The results affirm that the legacies of historic charcoal production can increase the spatial variability of soil physical properties and therefore also of ecological site conditions in forest areas. The results of soil moisture monitoring suggest that a determination of soil physical parameters in the laboratory is not sufficient to characterize the spatio-temporal variations of the soil water regime.}, language = {en} } @inproceedings{HirschBonhageBauriegeletal., author = {Hirsch, Florian and Bonhage, Alexander and Bauriegel, Albrecht and Schneider, Anna and Raab, Alexandra and Raab, Thomas and Gypser, Stella}, title = {Occurrence, soil parameters and genesis of Rhodic Arenosols ('Fuchserden') in northeastern Germany}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{HirschSchneiderBauriegeletal., author = {Hirsch, Florian and Schneider, Anna and Bauriegel, Albrecht and Raab, Alexandra and Raab, Thomas}, title = {Formation, classification and properties of soils at two relict charcoal hearth sites in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{BonhageRaabOuimetetal., author = {Bonhage, Alexander and Raab, Thomas and Ouimet, William and Raab, Alexandra}, title = {Effects of historical charcoal burning on soil landscapes in West Connecticut, USA}, series = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2018, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @misc{RaabKimBonhageetal., author = {Raab, Alexandra and Kim, Minhye and Bonhage, Alexander and Schneider, Anna and Raab, Thomas and Bauriegel, Albrecht}, title = {Initial processes of soil formation on Relict Charcoal Hearths (RCHs) in the Tauer Forest (Brandenburg, Germany)}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-3563}, abstract = {In the Tauer Forest, a woodland area north of the city of Peitz (Brandenburg, Germany), extensive charcoal burning was carried out from the mid-16th century to the mid-19th century resulting in numerous Relict Charcoal Hearths (RCHs). The most prominent feature of the soils on RCHs is the anthropogenically modified 20-30 cm thick RCH substrate that buries the former forest soil. The RCH substrate is a quite heterogenous mixture of mineral and organic compounds which were modified through heat during charring. It is characterized by its black color resulting from charcoal fragments (from fine dust to decimetre size pieces), lower bulk density, and higher porosity. After their use, the charcoal production sites were abandoned and soon became overgrown. Soil formation could commence in this anthropogenically modified RCH substrate. During recently conducted field work on RCHs in the Tauer Forest we detected features of initial podzolisation (bleaching of quartz grains) within this RCH substrate. To further investigate initial processes of soil formation (acidification, podzolisation, accumulation of soil organic matter) on RCHs, two different RCH sites were selected in the Tauer Forest: one RCH site in the forest district Tannenwald and one RCH site in the forest district Kleinsee. The Tannenwald site (RCH no. 29958) is situated in the western part of the Tauer Forest. It is an inland dune area with a coniferous forest (Scots pine, Pinus sylvestris L.) plantation. The forest soils are Podzols and the soils on the RCHs are classified as Spolic Technosols. The dense undergrowth consists of mainly blueberry (Vaccinium L.). Dendrochronological ages (determination by K-U Heußner, DAI Berlin) of charcoal pieces proof, that the charcoal hearth was used after 1655. The Kleinsee site (RCH no. 29424) is situated in the eastern part of the Tauer Forest. The parent material is sand from glaciofluvial sediments of the Weichselian glaciation. The forest soils are Brunic Arenosols (Protospodic) and the soils on the RCHs are classified as Spolic Technosols (Arenic). The deciduous forest is dominated by sessile oak (Quercus petraea (Matt.) Liebl.). The undergrowth is only scarce with some ferns (sporadic), blueberry (Vaccinium L.), some shoots of rowan (Sorbus aucuparia L.) and some moss. There is no dendrochronological age available from the RCH, but RCHs nearby were dated from the 18th to the 19th centuries. At both sites, three soil monoliths were sampled on the RCH platform and three monoliths from the natural forest soil as reference soils. The soil monoliths were sampled continuously in 3 cm vertical spacings. Following lab analyses were carried out: pH (CaCl2), pH (H2O), total carbon (TC), total nitrogen (TN), CECeff and total concentrations of selected elements. Analyses of pedogenic Fe are in progress. First results of these study will be presented and discussed.}, language = {en} } @book{RaabRaabBonhageetal., author = {Raab, Alexandra and Raab, Thomas and Bonhage, Alexander and Schneider, Anna and Hirsch, Florian and Aghte, Markus and Pommerenke, Alf}, title = {Historische K{\"o}hlerei in S{\"u}dbrandenburg - Begleitband zum K{\"o}hlerpfad Waldschule Kleinsee}, editor = {Raab, Thomas}, publisher = {Brandenburgische Technische Universit{\"a}t Cottbus - Senftenberg, Fachgebiet Geopedologie und Landschaftsentwicklung}, address = {Cottbus}, issn = {2196-4122}, doi = {10.26127/BTUOpen-5488}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:co1-opus4-54883}, pages = {68}, language = {de} } @misc{UchinoRaabBonhageetal., author = {Uchino, Kazuki and Raab, Alexandra and Bonhage, Alexander and Schneider, Anna and Raab, Thomas and Wechler, Klaus-Peter and Bauriegel, Albrecht}, title = {Spatial heterogeneity of buried and recent soils in a drift sand area in North-Eastern Germany}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-2354}, abstract = {In the North European Lowland, on the sandy deposits of the Weichselian glaciation, soils developed during periods of landscape stability are often conserved under windblown sand. However, small-scale changes of sediments and other soil forming factors can result in high spatial variation of soil properties in these landscapes; and relocation of soil material by geomorphic processes further increases the spatial heterogeneity of the soil landscape. These spatial variations in soil properties and conservation need to be considered in order to correctly decipher and interpret the buried soils as records of past environmental conditions. In the forefield of the open-cast mine Cottbus-Nord, archaeological excavations in a dune and drift sand area revealed widespread buried soils of different characteristics. The densely spaced excavation trenches give exceptionally good insights into the pedosphere, allow for reconstructing the distribution of fossil and recent soils in a high spatial resolution, and offer good opportunities to improve the understanding of spatial and temporal patterns of soil formation. Remains of postpleistocene hunter-gatherer campsites were documented in archaeological excavations and found to be associated with a buried soil horizon. We recorded the stratigraphy of soil profiles along more than 15 trenches within an area of about 20 ha, and additionally described the position of buried soils from GPR surveys and microdrone photogrammetry. In a recently opened, 455 m long trench, all characteristic soils and sediments of the study region could be observed and stratigraphically connected. Within this trench, four profiles were identified for further research. Each profile was classified and described according to WRB and German Guidelines for Soil Mapping; and was sampled and investigated through laboratory analyses including determination of organic matter, total carbon and nitrogen contents, soil colour identification, texture analysis, magnetic susceptibility measurement, metal content analysis using X-ray fluorescence analyzer and pH measurement. The compaction and cementation of soil horizons was assessed in situ with a pocket penetrometer. Results show a small-scale mosaic of soils developed on fluvio-aeolian, limnic and aeolian sediments, high spatial variations in pedogenesis due to varying groundwater influence and intensity of horizontal and vertical leachate transport, and high variations in the erosion or conservation of fossil soils. The soil and sediment stratigraphy reflects several phases of landscape development: i) the formation of a Late Pleistocene soil on fluvio-aeolian deposits, ii) a fossilization by aeolian sands, iii) a stability phase with intensive podsolization and peat formation, and iv) a land use-induced aeolian remobilization of the sands.}, language = {en} } @misc{AlJobayerBlossPorschetal., author = {Al Jobayer, Md Adif and Bloß, Katharina and Porsch, Christopher and Maaten, Ernst van der and Maaten-Theunissen, Marieke van der and Bonhage, Alexander and Raab, Alexandra and Schneider, Anna and Raab, Thomas}, title = {Drought sensitivity of Pinus sylvestris L. on century old charcoal rich Technosols in the North-German Lowland}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-7978}, abstract = {Soils on relict charcoal hearths (RCHs), i.e. aged charcoal rich Technosols, feature documented legacy effects regarding their physical and chemical soil properties. These forest soils result from the pre-/early-industrial production of charcoal in upright standing hearths. Today, RCHs are found in forested areas as circular microrelief structures with average diameters of about 10 meters that contain technogenic soil horizons of about 20 cm thickness. RCH soils are most distinctly characterized by their large content of pyrogenic soil organic matter and consequently increased total carbon contents. The resulting changes in the soils' cation exchange capacity, soil acidity, total nitrogen contents and total element stocks are often significant. Furthermore, changes in soil physical properties like a lower bulk density and a higher porosity result in changed soil-water- and temperature regimes. Combined, these effects potentially result in unique soil microhabitats that are restricted to relatively small, clearly defined areas in many forest ecosystems. Recent studies on RCH soils increasingly focus on potential changes in microbiological and vegetational composition and abundances and report diverse effects. Here, we study the effects of century old charcoal rich Technosols on the drought sensitivity of Scots pine (Pinus sylvestris L.) on three RCH sites located in Lower Lusatia, Saxony (Germany). Through dendrochronologial analysis of increment cores and historical climate data, we study climate-growth relationships for trees on RCH soils and reference forest soils for two periods (AD 1963-1992 \& AD 1990-2019). Furthermore, we determine pointer years and components of resilience to quantify the trees' reaction to extreme weather conditions. This analysis was accompanied by soil sampling and analysis on the RCH sites and adjacent reference forest soils. Here, we present preliminary results and discuss them in the context of findings from other studies on RCH soils.}, language = {en} } @misc{RaabHirschRaabetal., author = {Raab, Thomas and Hirsch, Florian and Raab, Alexandra and Schneider, Anna and Bonhage, Alexander and B{\"o}nisch, Eberhard}, title = {B{\"o}den historischer Landnutzung in der Niederlausitz - W{\"o}lb{\"a}cker und Kohlemeiler}, series = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, volume = {26}, journal = {Brandenburgische Geowissenschaftliche Beitr{\"a}ge}, number = {1/2}, issn = {0947-1995}, pages = {5 -- 14}, abstract = {In der Niederlausitz finden sich - meist unter Kiefern- und Eichenforsten versteckt - zahlreiche Relikte der historischen Landnutzung, die bisher kaum bekannt sind. Zu den auff{\"a}lligsten Formen z{\"a}hlen W{\"o}lb{\"a}cker und Pl{\"a}tze ehemaliger Kohlemeiler. In einigen Regionen der Niederlausitz ist die Verbreitung der Landnutzungsrelikte so groß bzw. ihre Dichte so hoch, dass sie pr{\"a}gend f{\"u}r die Bodenlandschaft werden. Dieser Beitrag zeigt an repr{\"a}sentativen Beispielen die charakteristischen Merkmale und Eigenschaften der B{\"o}den auf W{\"o}lb{\"a}ckern und Relikten von Holzkohlenmeilern (HKM).}, language = {de} } @inproceedings{RaabSchneiderRaabetal., author = {Raab, Thomas and Schneider, Anna and Raab, Alexandra and Hirsch, Florian and Bonhage, Alexander}, title = {The geomorphic legacy of historic charcoal production in Brandenburg, Germany}, series = {4th Central European Geomorphology Conference, Bayreuth, October 9th-13th 2017}, booktitle = {4th Central European Geomorphology Conference, Bayreuth, October 9th-13th 2017}, editor = {Holzheu, Stefan and Thies, Birgit}, address = {Bayreuth}, pages = {117 -- 118}, language = {en} } @incollection{HirschRaabSchneideretal., author = {Hirsch, Florian and Raab, Alexandra and Schneider, Marcus and Raab, Thomas and Schneider, Anna and Bonhage, Alexander}, title = {Landschaftsgeschichtliche Untersuchungen am Eilenzfließ bei Taubendorf}, series = {Ausgrabungen im Niederlausitzer Braunkohlenrevier : 2015/2016}, booktitle = {Ausgrabungen im Niederlausitzer Braunkohlenrevier : 2015/2016}, editor = {Schopper, Franz}, publisher = {Brandenburgisches Landesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Landesmuseum}, address = {W{\"u}nsdorf}, isbn = {978-3-910011-87-8}, pages = {199 -- 204}, language = {de} } @inproceedings{RaabRaabHirschetal., author = {Raab, Thomas and Raab, Alexandra and Hirsch, Florian and Schneider, Anna and Bonhage, Alexander}, title = {Late Quaternary landscape development and legacies of human-induced land use changes in Lower Lusatia, South Brandenburg, Germany}, series = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, booktitle = {ICLEA Final Symposium 2017, Human Impact and Landscape Evolution in the Southern Baltic Lowlands, Abstract Volume \& Excursion Guide}, editor = {Schwab, Markus and Błaszkiewicz, Mirek and Raab, Thomas and Wilmking, Martin and Brauer, Achim}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-17037}, pages = {182 -- 198}, language = {en} } @inproceedings{RaabHirschVassermanetal., author = {Raab, Thomas and Hirsch, Florian and Vasserman, Oleksandr and Raab, Alexandra and Naeth, M. Anne}, title = {Influence of relief and vegetation on soil properties in a disturbed chernozem soil landscape}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {In central and southeastern Alberta, chernozems dominate the soil landscape and are divided into several groups that follow the climate gradient from Northwest to Southeast: Dark Grey Chernozems, Black Chernozems, Dark Brown Chernozems; Brown Chernozems. Principles controlling development and distribution of these chernozem subtypes along the ecotone transect are quite well known. However, intensive land use over the last century has affected soils that originally have formed under natural conditions during the Holocene in more than 10,000 years. There is a lack of knowledge regarding soil development in these landscapes on the decadal to centennial time scale. Within this time frame the most important factor of soil formation may be relief, although this has not been properly studied. This study aims to compare soil properties in a typical chernozem landscape where soils have been highly disturbed and parent materials have been re-arranged by surface coal mining.We hypothesize that within 50 years, soils develop with significant differences based on vegetation type and slope aspect. Our study site is the former Diplomat Mine near Forestburg, Alberta where spoils form a small scale ridge and graben topography. The south facing slopes of the piles are covered by grassland, whereas on the north exposition has trees and shrubs. Samples were taken from six sites with differences in topography and vegetation type. Diplomate T1 is at the top of the ridge with grassland, Diplomate S1 is on the southern slope with grassland, Diplomate N1 is on the northern slope with trees, and Diplomate N2 is on the northern slope with shrubs. For comparison we took samples from two sites without slope aspect. One site was an undisturbed grassland (Diplomate Z1) and the other sites were reclaimed piles (Diplomate R1). At each site, five soil profiles were examined and volumetrically sampled (250 cm3 steel ring) in steps of five centimeters to a depth of 30 centimeters. We present first results of basic physical and chemical soil parameters (bulk density, water content, pH, Cstock, N-stock).}, language = {en} } @inproceedings{SchneiderHirschWechleretal., author = {Schneider, Anna and Hirsch, Florian and Wechler, Klaus-Peter and Raab, Alexandra and Raab, Thomas}, title = {Mapping a paleosurface and archaeological site location in an inland dune area in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {Mapping and visualizing the position of archaeological remains in the surface relief provides important basic information for archaeological survey design and interpretation. Geomorphological processes in (pre)history can have resulted in a modification of the local relief around archaeological sites, especially in areas that are prone to sediment erosion and relocation, so that models of past surfaces are necessary for a correct interpretation of archaeological survey results. In this study, we combined terrestrial survey and remote sensing methods to reconstruct the palaeorelief around two archaeological excavation sites in an inland dune area in southern Brandenburg, Germany. Remains from two Mesolithic hunter-gatherer camps were documented in archaeological excavations and found to be associated with a buried soil horizon. To gather information on the relief of the buried soil surface, we used a combination of sedimentological and pedological profile description of archaeological survey trenches and geophysical prospection with Ground-Penetrating Radar; supplemented by microdrone photography and photogrammetry, GPS surveys and analysis of LIDAR-based elevation models. A digital elevation model of the buried surface was created by combining point data from these sources. The buried surface morphology and the position of the archeological remains within the reconstructed landscape were analyzed in GIS. The comparison of the generated paleosurface model with the recent surface elevation model shows that sand remobilization resulted in a considerable reshaping of the relief. Analysis of the buried surface model further shows that the relief position of the two archaeological sites in the study area was considerably more prominent in relation to the corresponding buried soil surface than in relation to the recent surface morphology. Results affirm the importance of considering Holocene relief modifications in archaeological surveys.}, language = {en} } @inproceedings{RaabSchneiderBonhageetal., author = {Raab, Alexandra and Schneider, Anna and Bonhage, Alexander and Raab, Thomas and Hirsch, Florian}, title = {Extensive historical charcoal production in Brandenburg (Germany) - identification of potential areas by GIS analysis}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {We used a GIS analysis of environmental and historical data to identify potential areas of extensive charcoal production in Brandenburg. The analysis was based on three assumptions (i to iii). Large charcoal kiln fields can be found in areas that i) are close to historical industrial sites, ii) are close to bog iron ore deposits, and iii) have been continuously covered by forest during the last centuries. Information on theses parameters was gathered in an archive and literature study and from historical and recent maps. Areas with a high probability of kiln site occurrence were then determined using a simple binary additive model. In the last step, shaded-relief maps (SRMs) were visually checked for clearly visible kiln sites and soil properties were analysed in the determined areas. In total, eight areas with a high probability of kiln site occurrence are identified for the state of Brandenburg. By visual interpretation of SRMs, high kiln site densities in these areas are confirmed. The analysis of soil maps shows that kiln fields are predominantly located on sandy soils with a low yield potential. Although further parameters and study areas need to be considered in the model in order to explain the spatial distribution patterns of charcoal production, the results indicate correlations between the location of bog iron ore deposits, historic ironworks and charcoal kiln fields.}, language = {en} } @inproceedings{HirschMaatenTheunissenMaatenetal., author = {Hirsch, Florian and Maaten-Theunissen, Marieke van der and Maaten, Ernst van der and Schneider, Anna and Raab, Alexandra and Raab, Thomas}, title = {Soil physics and chemistry at a medieval ridge and furrow site in northeastern Germany}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {The usage of non-reversible ploughs, mainly during the Middle Ages and until historic times, led to the formation of ridge and furrow systems. Due to improvements of agricultural techniques, these historic agricultural sites were often abandoned and are now marginal land. The parallel ridges and furrows are usually, if not destroyed by later conventional ploughing, preserved in present-day forests. In northeastern Germany ridge and furrow systems are normally several decameters long and up to ten meters wide. The height difference between ridge top and furrow bottom is up to 50 centimeters and is expected to cause significant contrasts of soil properties and vegetation. Furthermore, due to the abandonment of sites with ridges and furrows, soils on these sites are unique archives for studies on fertilization, soil carbon dynamics and soil development. Therefore, we are characterizing soil physics (bulk density, saturated soil hydraulic conductivity, texture) and soil chemistry (soil acidity, carbon and nitrogen content) on a type location of historic ridges and furrows about 100 km northwest of Berlin.}, language = {en} } @inproceedings{HirschRaabOuimetetal., author = {Hirsch, Florian and Raab, Thomas and Ouimet, William and Dethier, David and Schneider, Anna and Raab, Alexandra}, title = {Soils on historic charcoal hearths - chemical properties and terminology}, series = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2017, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, url = {http://nbn-resolving.de/http://meetingorganizer.copernicus.org/EGU2017/EGU2017-4009-1.pdf}, abstract = {Charcoal hearths are a unique archive for the long term interaction between biochar, soil development and plant growth. Charcoal as raw material was crucial for the production of iron in iron works and hence numerous charcoal hearths can be found in the forests near historic iron works in Europe as well as the Eastern United States. Charcoal hearths are round to elliptical forms often around 10 m in diameter, and consisting of a several decimeter thick layer containing charcoal fragments, ash, and burnt soil. We studied the soil chemistry of 24 charcoal hearths and compared them to the surrounding 'natural' soils in Litchfield County, Connecticut. The thickness of the organic rich horizons on the charcoal hearths and their carbon content is remarkably higher than in the surrounding topsoils. The wide distribution of charcoal hearths, their usually high quantity, and their occurrence in different ecosystems underlines their importance for further pedological research.}, language = {en} } @incollection{RaabHirschSchneideretal., author = {Raab, Thomas and Hirsch, Florian and Schneider, Anna and Raab, Alexandra}, title = {Geo{\"o}kologische Folgen historischer Landnutzung}, series = {Geoarch{\"a}ologie}, booktitle = {Geoarch{\"a}ologie}, editor = {Stolz, Christian and Miller, Christopher E.}, publisher = {Springer Spektrum}, address = {Berlin, Heidelberg}, doi = {10.1007/978-3-662-62774-7_8}, pages = {71 -- 77}, abstract = {Seit dem Neolithikum wirkt sich die Nutzung der Landschaft auf unterschiedliche Weise auf Relief, B{\"o}den, Gew{\"a}sser, Flora, Fauna und Klima aus. Insbesondere die Folgen land- und forstwirtschaftlicher Wirtschaftsweisen waren daf{\"u}r ausschlaggebend. Grunds{\"a}tzlich reagieren {\"O}kosysteme auf anthropogene Eingriffe, wie die Umwandlung von Wald in andere Nutzungsformen, mit einer schrittweisen Degradation sowie reversiblen oder irreversiblen Ver{\"a}nderungen. Beispiele sind Bodenerosion und eine ver{\"a}nderte Artenzusammensetzung. Die Absch{\"a}tzung des Ausmaßes im globalen Maßstab gestaltet sich generell schwierig. F{\"u}r die Geoarch{\"a}ologie bedeutsam sind daher haupts{\"a}chlich lokale Spuren fr{\"u}herer Bewirtschaftung und Formen im Kleinrelief, die sich im Gel{\"a}nde wiederfinden lassen und als Geoarchive fungieren. Denn sie geben Aufschluss {\"u}ber (pr{\"a}-)historische Bewirtschaftungsformen. So zeugen W{\"o}lb{\"a}cker, Hochbeete, Plaggenesche und die Relikte der historischen Teichwirtschaft, Moorkultivierung und K{\"o}hlerei von fr{\"u}heren Formen der Land- und Forstwirtschaft.}, language = {de} } @misc{RaabRaabHirschetal., author = {Raab, Thomas and Raab, Alexandra and Hirsch, Florian and Bonhage, Alexander and Schneider, Anna}, title = {Fingerprints from past charcoal burning - lessons learned and future perspective studying Relict Charcoal Hearths (RCH)}, series = {EGU General Assembly 2020, Online | 4-8 May 2020}, journal = {EGU General Assembly 2020, Online | 4-8 May 2020}, doi = {https://doi.org/10.5194/egusphere-egu2020-2949}, language = {en} } @misc{SchneiderHirschRaabetal., author = {Schneider, Anna and Hirsch, Florian and Raab, Alexandra and Bonhage, Alexander and Raab, Thomas}, title = {Relikte historischer Kohlenmeier ini der Oberpfalz - Verbreitung und Erhaltung in Abh{\"a}ngigkeit vom Naturraum}, series = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, journal = {Beitr{\"a}ge zur Arch{\"a}ologie in der Oberpfalz und in Regensburg}, number = {13}, issn = {1617-4461}, pages = {531 -- 546}, language = {de} } @inproceedings{HirschNicolaySchneideretal., author = {Hirsch, Florian and Nicolay, Alexander and Schneider, Anna and Błaszkiewicz, Mirosław and Kordowski, Jarosław and Noryskiewicz, Agnieszka M. and Tyszkowski, Sebastian and Raab, Alexandra and Raab, Thomas}, title = {Late Quaternary soil genesis and geomorphodynamics in Northern Poland}, series = {2nd Annual ICLEA Workshop 2013, Dynamics of climate and landscape evolution of cultural landscapes in the Northern Central European Lowlands since the last ice age, Abstract volume \& Excursion guide}, booktitle = {2nd Annual ICLEA Workshop 2013, Dynamics of climate and landscape evolution of cultural landscapes in the Northern Central European Lowlands since the last ice age, Abstract volume \& Excursion guide}, publisher = {Deutsches GeoForschungsZentrum GFZ}, address = {Potsdam}, doi = {10.2312/GFZ.b103-13047}, pages = {S. 43}, language = {en} } @book{HirschRaabRaab, author = {Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Beitr{\"a}ge zur Landnutzungsgeschichte in der Niederlausitz und im Erzgebirge}, publisher = {Brandenburg University of Technology}, address = {Cottbus ; Senftenberg}, issn = {2196-4122}, doi = {10.26127/BTUOpen-5388}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:co1-opus4-53887}, pages = {101}, abstract = {In diesem Band sind verschiedene Beitr{\"a}ge zur Landnutzungsgeschichte in der Niederlausitz und im Erzgebirge zusammengefasst. Die ersten vier Beitr{\"a}ge befassen sich mit historischen Ackerfluren und W{\"o}lb{\"a}ckern in der Niederlausitz. Arch{\"a}ologische Untersuchungen, in Kontext gestellt mit archivalischen Quellen und historischen Karten, geben gemeinsam mit dem Einsatz naturwissenschaftlicher Methoden und Visualisierungen hochaufl{\"o}sender LiDAR-Daten neue Einblicke in die ehemalige Landnutzung. Der f{\"u}nfte Beitrag aus dem Erzgebirge beschreibt die Nutzung von ehemaligen Meilerpl{\"a}tzen als Quellengattung der Montanarch{\"a}ologie.}, language = {de} } @inproceedings{TaklaRaabRaabetal., author = {Takla, Melanie and Raab, Alexandra and Raab, Thomas and R{\"o}sler, Horst and B{\"o}nisch, Eberhard}, title = {Modeling the past - a GIS-based study for the reconstruction of past land use and human impact on the environment}, series = {2010 GSA Annual Meeting in Denver Colorado, USA 2010, 31 October - 3 November}, booktitle = {2010 GSA Annual Meeting in Denver Colorado, USA 2010, 31 October - 3 November}, publisher = {Geological Society of America}, address = {Boulder, Colo.}, pages = {S. 579}, language = {en} } @inproceedings{BoenischRoeslerSchopperetal., author = {B{\"o}nisch, Eberhard and R{\"o}sler, Horst and Schopper, Franz and Raab, Thomas and Raab, Alexandra}, title = {Pre-industrial charcoal production in southern Brandenburg - A landscape laboratory for studies on the fate of terrestrial organic carbon}, series = {EGU General Assembly 2010, held Vienna, Austria, 02 - 07 May 2010}, booktitle = {EGU General Assembly 2010, held Vienna, Austria, 02 - 07 May 2010}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{SchneiderHirschFritschetal., author = {Schneider, Anna and Hirsch, Florian and Fritsch, Simone and Raab, Alexandra and Raab, Thomas}, title = {Hydraulische Eigenschaften von B{\"o}den an historischen Holzkohlemeilerpl{\"a}tzen in Brandenburg}, series = {Unsere B{\"o}den - unser Leben, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, 2. - 10. September 2015, M{\"u}nchen}, booktitle = {Unsere B{\"o}den - unser Leben, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, 2. - 10. September 2015, M{\"u}nchen}, publisher = {Deutsche Bodenkundliche Gesellschaft}, address = {G{\"o}ttingen}, language = {de} } @misc{RaabRaabNicolayetal., author = {Raab, Thomas and Raab, Alexandra and Nicolay, Alexander and Takla, Melanie and Hirsch, Florian and R{\"o}sler, Horst and Bauriegel, Albrecht}, title = {Opencast mines in South Brandenburg (Germany) - archives of Late Quaternary landscape development and human-induced land use changes}, series = {Archaeological and Anthropological Sciences}, volume = {8}, journal = {Archaeological and Anthropological Sciences}, number = {3}, issn = {1866-9565}, doi = {10.1007/s12520-015-0227-6}, pages = {453 -- 466}, abstract = {This study outlines the opportunities for geoarchaeological research in active opencast lignite mines in southern Brandenburg (Germany). Studies on extensive outcrops that address both archaeology and soil geomorphology, combined with a geographical information system (GIS) approach, provide unique insights into human-induced environmental changes in Lower Lusatia and generally improve our understanding of landscape dynamics. We present the most recent results from three case studies and review important findings from the last several years. Studies conducted in opencast mines of Cottbus-Nord and J{\"a}nschwalde focus on (i) Late Quaternary geomorphodynamics and soil development and (ii) past land use and the legacy of agriculture and woodland use. Our results are similar to those in other regions in Central Europe, but we also observe regional differences caused by the local setting, e.g. intensification of soil erosion coinciding with the expansion of farming of cultivated lands in the Slavic Middle Ages. Our research reveals the largest archaeologically investigated area of historical charcoal production in the Northern European Lowland (NEL). We are clearly only beginning to understand the massive dimensions of charcoal production in the region.}, language = {en} } @inproceedings{BurasHirschMaatenetal., author = {Buras, Allan and Hirsch, Florian and Maaten, Ernst van der and Takla, Melanie and R{\"a}biger, Christin and Cruz-Garc{\´i}a, Roberto and Schneider, Anna and Raab, Alexandra and Raab, Thomas and Wilmking, Martin}, title = {Charcoal kiln relicts - a favorable site for tree growth?}, series = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, booktitle = {European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, language = {en} } @inproceedings{TaklaMuellerRoesleretal., author = {Takla, Melanie and M{\"u}ller, Frank and R{\"o}sler, Horst and Raab, Alexandra and Raab, Thomas}, title = {Forestry and charcoal burning in the vicinity of the ironwork Peitz (South Brandenburg, Germany) - What do we know from historical and archaeological data?}, series = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, booktitle = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, editor = {Schwab, Markus J. and Theuerkauf, Martin and Brauer, Achim and Wilmking, Martin and Lampe, Reinhard}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-14028}, pages = {51}, language = {en} } @inproceedings{HirschNicolayPoetzschetal., author = {Hirsch, Florian and Nicolay, Alexander and P{\"o}tzsch, Bastian and Fritzsche, Marie and Raab, Alexandra and Raab, Thomas}, title = {Influence of charcoal burning induced pyrolysis on soils}, series = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, booktitle = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, editor = {Schwab, Markus J. and Theuerkauf, Martin and Brauer, Achim and Wilmking, Martin and Lampe, Reinhard}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-14028}, pages = {41}, language = {en} } @misc{RaabHirschSchneideretal., author = {Raab, Thomas and Hirsch, Florian and Schneider, Anna and Bonhage, Alexander and Raab, Alexandra}, title = {Geoecological legacies of pre-industrial charcoal burning - Research questions and approaches}, series = {European Geosciences Union, General Assembly 2019, Vienna, Austria}, journal = {European Geosciences Union, General Assembly 2019, Vienna, Austria}, address = {Katlenburg-Lindau}, language = {de} } @inproceedings{NicolayRaabRaab, author = {Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Evidence of (pre-) historic to modern landscape development and land use history in Lower Lusatia (Brandenburg, Germany)}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {In the apron of three active lignite opencast pits in Lower Lusatia (Brandenburg, Germany), archaeological survey trenches were investigated in areas where Quaternary aeolian sand deposits are widespread. The investigated palaeoenvironmental archives in J{\"a}nschwalde, Cottbus-Nord and Welzow contain evidence of fluvial and aeolian morphodynamics, soil formation and agricultural land use from (pre-)historic to modern times. To study the age and the causes of sand drifting and landform stabilization, standard soil physical and chemical laboratory analyses as well as optically stimulated luminescence (OSL) and radiocarbon dating (14C) were carried out. Two main sedimentological units were identified: Unit 1 consists of glacio-fluvial and Late Weichselian aeolian sands representing the parent material for the native Podsol-Braunerde and Podsol development, while Unit 2 represents the Late Holocene aeolian deposits. Four periods of Late glacial and Holocene aeolian activity and three phases of geomorphological stability have been identified: (i) Aeolian sedimentation during the Late glacial, (ii) Mesolithic reactivation of aeolian processes, (iii) soil formation until Late Roman Iron Age settlers intensified the agricultural land use, (iv) intensive drift sand formation during the High Middle Ages due to agricultural expansion, (v) stabilization of the drift sands and weak soil formation, (vi) reactivation of aeolian processes due to the increasing wood consumption and charcoal production from the early 16th until the mid-19th century, (vii) surface stabilization and formation of Regosols since the mid-19th century due to afforestation.}, language = {en} } @inproceedings{HirschNicolayPoetzschetal., author = {Hirsch, Florian and Nicolay, Alexander and P{\"o}tzsch, Bastian and Fritzsche, Marie and Raab, Alexandra and Raab, Thomas}, title = {Influence of charcoal burning induced pyrolysis on soils}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {In Lusatia, Northeastern Germany, the production of ironware between the 16th and 19th century left behind a remarkable amount of charcoal kilns in the forests north of Cottbus. Remote sensing surveys, underpinned by archaeological studies, show that charcoal was gained around Cottbus from several thousand charcoal kilns which had internal diameters up to 20 m. For the study site with 35 km2 area, the until now prospected total ground area below the charcoal kilns which was potentially affected by the pyrolysis is about 0,5 km2. Historic data indicates that the pyrolysis in the charcoal kiln took up to several weeks, for the kilns with a diameter of 20 m about 20 days. To characterize the depth of thermal alteration of soils below the kiln our current focus is on the differentiation of the iron hydroxides by small-scale vertical analysis of soil profiles.}, language = {en} } @inproceedings{NicolaySchulzRaabetal., author = {Nicolay, Alexander and Schulz, Deborah and Raab, Thomas and Raab, Alexandra}, title = {Landscape and soil development in Lower Lusatia - results from archaeological and soil-geomorphological investigations on a small dune field nearby J{\"a}nschwalde (Brandenburg, Germany)}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {Within the apron of the opencast mine J{\"a}nschwalde (SE Brandenburg, Germany) archaeological excavations on a multiple populated small dune were complemented with soil-geomorphological investigations in the vicinity. Archaeological findings in the dune stratigraphy (especially cremation graves) are intercalated within aeolian sediments and/or buried soils and thus give a record of the Late Quaternary geomorphodynamic and soil development.}, language = {en} } @inproceedings{TaklaRaabRaab, author = {Takla, Melanie and Raab, Thomas and Raab, Alexandra}, title = {Die fr{\"u}hindustrielle K{\"o}hlerei in der J{\"a}nschwalder Heide (Tagebau J{\"a}nschwalde, Niederlausitz). Eine GIS-basierte Rekonstruktion des Wald- und Landschaftszustandes mithilfe historischer Karten ab dem 18. Jahrhundert}, series = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie - Jahrestagung 2013, 2.-4.5.2013, BTU Cottbus}, booktitle = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie - Jahrestagung 2013, 2.-4.5.2013, BTU Cottbus}, editor = {Raab, Thomas and Hirsch, Florian and Raab, Alexandra and Schopper, Franz and Freytag, Klaus}, publisher = {BTU Cottbus}, address = {Cottbus}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:co1-opus4-40619}, pages = {S. 47}, language = {de} } @misc{SchneiderDonovanHirschetal., author = {Schneider, Anna and Donovan, Sara and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Der Einfluss von Relikten der historischen K{\"o}hlerei auf Bodentemperatur und -w{\"a}rmeleitf{\"a}higkeit}, series = {Abstract-Band, Jahrestagung der Bodenkundlichen Gesellschaft der Schweizund der Deutschen Bodenkundlichen GesellschaftBern, 24.-29. August 2019}, journal = {Abstract-Band, Jahrestagung der Bodenkundlichen Gesellschaft der Schweizund der Deutschen Bodenkundlichen GesellschaftBern, 24.-29. August 2019}, pages = {S. 350}, abstract = {Die Beimengung von Holzkohle in B{\"o}den kann deutlichen Einfluss auf die physikalischen Bodeneigenschaften haben. Solche Effekte treten nicht nur in gezielt mit Holzkohle („biochar") angereicherten Ackerb{\"o}den auf, sondern auch auf den Standorten historischer Holzkohlemeiler (HKM), die in vielen Waldgebieten in großer Zahl vorkommen. Die pr{\"a}gendste Eigenschaft solcher B{\"o}den auf HKM ist eine technogene, kohlereiche Substratschicht, die {\"u}ber dem nat{\"u}rlich entwickelten Bodenprofil abgelagert ist. In j{\"u}ngster Zeitwurden in mehreren Studien ein von den umliegenden Waldb{\"o}den abweichendes Vegetationswachstum und eine abweichende C-Dynamik auf HKM festgestellt. Welche Bodeneigenschaften der HKM solche Unterschiede bewirken, ist aber noch unklar. Ein m{\"o}glicher, bisher kaum untersuchter Einflussfaktor ist die Bodentemperatur. Ziel dieser Studie war es, den Einfluss von Holzkohlebeimengungen auf die W{\"a}rmeleitf{\"a}higkeit und das Bodentemperaturregime von HKM-B{\"o}den zu charakterisieren. Untersucht wurden HKM auf sandigem Substrat in der Lausitz (Brandenburg). An zwei Standorten wurden Profile auf HKM und benachbarten Waldb{\"o}den f{\"u}r ein Monitoring der Bodentemperatur {\"u}ber jeweils ein Jahr instrumentiert, die W{\"a}rmeleitf{\"a}higkeit von HKM-Schicht, Ah-, fAh-und Bv-Horizont wurde im Labor bestimmt. In einem Laborexperiment wurde zus{\"a}tzlich die W{\"a}rmeleitf{\"a}higkeit von k{\"u}nstlich hergestellten Proben aus sandigem Substrat und Holzkohlefragmenten in unterschiedlichen Mischungsverh{\"a}ltnissen untersucht. Die Ergebnisse zeigen eine deutlich verringerte W{\"a}rmeleitf{\"a}higkeit des kohlereichen Substrats. Damit verbunden zeigen sich im Monitoring geringere Schwankungen der Bodentemperatur auf den HKM in tiefen Bereichen des Profils, in den obersten Dezimetern wurden hingegen st{\"a}rkere Schwankungen der Bodentemperatur festgestellt. Insgesamt zeigt sich damit ein noch {\"u}ber die technogene Substratschicht hinaus wirksamer Einfluss der typischen Eigenschaften des kohlereichen HKM-Substrats auf die Bodentemperatur.}, language = {de} } @misc{BonhageHirschSchneideretal., author = {Bonhage, Alexander and Hirsch, Florian and Schneider, Anna and Raab, Alexandra and Raab, Thomas}, title = {Aged biochar enriched substrate increases SOM stocks of forest soils in the North German Lowland}, series = {Abstract-Band, Jahrestagung der Bodenkundlichen Gesellschaft der Schweizund der Deutschen Bodenkundlichen GesellschaftBern, 24.-29. August 2019}, journal = {Abstract-Band, Jahrestagung der Bodenkundlichen Gesellschaft der Schweizund der Deutschen Bodenkundlichen GesellschaftBern, 24.-29. August 2019}, pages = {S. 502}, abstract = {Recentfindings of more than 4000 relict charcoal hearths (RCH) in the forest district Tauer (Brandenburg, Germany) raise the question to what extent soil properties are controlled by a legacy effect of historical charcoal burning. RCH sites are characterized bya substantial admixture of charcoal fragments of varying particle sizes constituting an anthropogenic addition of carbon to the natural forest soil. Ages of about 250 years proven by dendrochronological dating of larger charcoal pieces on RCHs allow for assessing long-term effects of biochar application on forest soils. In this study, we measured the geometry and SOM content of 20 RCH sites in a selected part of the forest district. The results are the basis for a projection of RCH SOM stocks on a 40 ha forest plot with 120 RCH sites. In the range of statistical uncertainties it is shown that RCHs add between 13 \% and 32 \% of SOM to the SOM stock of the natural forest soil in the studied plot. These substantial amounts of SOM are so far not recognized by any soil survey or forest soil inventories of SOM and SOC stocks. In light of an increasing amount of studies that detect RCH sites in forests of Europe and the USA in the range of tens-and even hundreds of thousands, the question has to be asked how to address this legacy effect in ongoing scientific discussions about soil carbon stocks, carbon sequestration and the long-term effects of biochar application into soils.}, language = {de} } @inproceedings{HirschNicolaySchneideretal., author = {Hirsch, Florian and Nicolay, Alexander and Schneider, Anna and Błaszkiewicz, Mirosław and Kordowski, Jarosław and Noryskiewicz, Agnieszka M. and Tyszkowski, Sebastian and Raab, Alexandra and Raab, Thomas}, title = {Sp{\"a}tquart{\"a}re Landschaftsentwicklung seit der Pommerschen Phase in Wygonin (Nordpolen)}, series = {Jahrestagung des AK Geomorphologie in Kiel 2014}, booktitle = {Jahrestagung des AK Geomorphologie in Kiel 2014}, editor = {Bork, Hans-Rudolf and Dreibrodt, Stefan and Duttmann, Rainer and Unkel, Ingmar}, publisher = {Christian-Albrechts-Universit{\"a}t}, address = {Kiel}, pages = {S. 66}, language = {de} } @inproceedings{RaabNaethHirschetal., author = {Raab, Thomas and Naeth, M. Anne and Hirsch, Florian and Raab, Alexandra}, title = {Contributing towards a conceptual model of soil-landscape co-evolution: observations from historic mining sites in Alberta, Canada}, series = {European Geosciences Union, General Assembly 2016, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2016, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {At the former Diplomat Mine near Forestburg, Alberta, Canada we find a diverse soil landscape which can help to conceptualize factors and processes controlling initial pedogenesis and soil distribution on very young landforms in prairie environments. Due to differing reclamation practices in the 1950s and landslides occurring after spoil dumping, four areas can be distinguished by GoogleMaps/LiDAR evaluation and onsite field survey: (i) not-mined, (ii) stock piled and unreclaimed, (iii) stock piled and reclaimed and (iv) affected by post-mining geomorphodynamics and quasi-natural redeposition. The parent material for areas (ii) to (iv) was initially dumped by spreaders but only (ii) didn't undergo further change. Landscape (iii) has seen levelling of the piles by heavy machinery. Features of landscape (iv) are formed by reshaping the originally dumped and levelled structures. This last landscape unit marks the rim of the former mine adjacent to the river valley. In practice, mining activities formed new valley slopes. In contrast to the naturally developed slopes the mine slopes were less stable. Vegetation, which could have hindered slope wash erosion, was missing after dumping the spoil slopes. Slopes were very steep (or practically undercut) and therefore, substrates were naturally re-located by mass movements such as sliding and slumping. Characteristic sliding and slumping structures can be identified in the close-ups of the LiDAR images. Both processes, mass movement and slope wash erosion, may have overlapped. Landscape (ii) is the most contrasting one. Dumped stock piles formed elongated, curved and steep ridges. These landforms do not have a natural analogue but clearly show their technological origin. Most interesting are differences in vegetation. South and southwest facing slopes are covered with grassland whereas north and northeast facing slopes are covered with aspen trees. Some of the ditches are filled with water and form small elongated ponds. The characteristic geomorphology of the prairie can be found in landscape (i). Distinct differences are found in properties and types of soils in these four landscapes. Natural soils and pile soils characteristically differ in parent material and soil horizons. No information is gathered yet for the reclaimed soils and the landslides soils due to prohibited access. However, based on what we find at the former Diplomat Mine we can conclude that distribution, development and properties of unreclaimed soils in historical open cast mines in Alberta are primarily controlled by parent material and topography. The geomorphological set-up is dominating the trajectory of vegetation development and post-mining geomorphodynamics. Contrasting slope aspects determine micro climatic conditions and lead to different vegetation types. This has likely had an effect on soil development and soil properties (especially carbon stocks). Further studies will be conducted to quantify these differing soil properties to refine this conceptual model of initial pedogenesis and soil distribution on very young landforms in the prairie landscapes.}, language = {en} } @inproceedings{NicolayRaabRaab, author = {Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Evidence pf (pre-) historic to modern landscape development and land use history in Lower Lusatia (Brandenburg, Germany)}, series = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, booktitle = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, editor = {Schwab, Markus J. and Theuerkauf, Martin and Brauer, Achim and Wilmking, Martin and Lampe, Reinhard}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-14028}, pages = {47}, language = {en} } @misc{SchneiderHirschBonhageetal., author = {Schneider, Anna and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Soil moisture monitoring on land use legacy soils - a study on relict charcoal hearth sites in Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, journal = {European Geosciences Union, General Assembly 2019, Vienna, Austria, 7-12 April 2019}, address = {Katlenburg-Lindau}, language = {de} } @inproceedings{SchneiderTaklaNicolayetal., author = {Schneider, Anna and Takla, Melanie and Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Automated detection of small-scale anthropogenic relief features from high-resolution ALS-data}, series = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, booktitle = {3rd Annual ICLEA Workshop 2014, Dynamics of Climate and Landscape Evolution of Cultural Landscapes in the Northern Central European Lowlands since the Last Ice Age}, editor = {Schwab, Markus J. and Theuerkauf, Martin and Brauer, Achim and Wilmking, Martin and Lampe, Reinhard}, publisher = {GFZ German Research Centre for Geosciences}, address = {Potsdam}, doi = {10.2312/GFZ.b103-14028}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:b103-14028}, pages = {S. 49}, language = {en} } @inproceedings{TaklaMuellerRoesleretal., author = {Takla, Melanie and M{\"u}ller, Frank and R{\"o}sler, Horst and Raab, Alexandra and Raab, Thomas}, title = {Forestry and charcoal burning in the vicinity of the ironwork Peitz (South Brandenburg, Germany) - What do we know from historical and archaeological data?}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {The former royal forest districts around Peitz (South Brandenburg, Germany) were used to produce charcoal for the ironwork Peitz (1554 to 1856). More than 800 archaeologically excavated ground plans of charcoal kilns give evidence of the burning activity in the study area "J{\"a}nschwalde Heide" which is only a small part of the whole forest district. The study area in the apron of the active lignite mine J{\"a}nschwalde comprises the royal forest "J{\"a}nschwalder Heide" and the surrounding community forests. Our study approach combines archaeological research, a GIS-based approach (historical maps, airborne laser scanning (ALS) data, etc.) and archival studies.}, language = {en} } @inproceedings{SchneiderTaklaNicolayetal., author = {Schneider, Anna and Takla, Melanie and Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Quantitative analysis of anthropogenic relief features: automated mapping of charcoal kiln sites from high-resolution ALS data}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {High-resolution digital elevation data from airborne laser scanning (ALS) allow for identification and mapping of so far unknown small-scale relief features that are hidden by forest cover. Especially as a result of historic land use, small anthropogenic landforms can occur, e.g., remains of charcoal kilns on sites that were used for charcoal production or ridge and furrow systems in former farmland areas. Mapping such relief features and analyzing their spatial distribution patterns can help to understand past land-use systems and their effects on landscapes. To efficiently detect and quantify small-scale relief features from high-resolution DEMs for larger areas, (semi-) automated mapping routines are required.}, language = {en} } @inproceedings{RaabFrantiucBrademannetal., author = {Raab, Alexandra and Frantiuc, Alexandru and Brademann, Brian and Ott, Florian and Hirsch, Florian and Brauer, Achim and Raab, Thomas}, title = {Proxies of pre-industrial charcoal production and land use in lake sediments from South Brandenburg, Germany}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {During the last decades, archaeological research has revealed that large-scale charcoal burning was carried out in Lower Lusatia (South Brandenburg) situated within the North Germany Lowland. From the 17th to the 19th century, charcoal was mainly produced for the ironwork in Peitz. Within the framework of the ICLEA project lake sediments from two lakes, Byhleguhrer See and Großsee, are investigated to study the impact of pre-industrial charcoal production on the environment.}, language = {en} } @inproceedings{RaabRaabNicolayetal., author = {Raab, Thomas and Raab, Alexandra and Nicolay, Alexander and Takla, Melanie and Hirsch, Florian and Schneider, Anna and R{\"o}sler, Horst and B{\"o}nisch, Eberhard}, title = {Human-induced landscape dynamics in South Brandenburg - findings from different geoarchives}, series = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, booktitle = {European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April - 02 May 2014}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {South Brandenburg is the central part of the North European Lowland (NEL) extending as a plain landscape from the North and Baltic Sea to the foothills of the Central European Highlands and reaching from the Netherlands to Poland. Since many decades lignite opencast mines have been operating in this region which is known as the Lusatian mining district. The total land demand in Lusatia is about 852 square kilometres and mining will continue for many more years or even decades. Large-scale outcrops resulting from these mining activities are excellent archives to study the younger Earth's history. The scope of our research in open cast mines is to reconstruct the Late Quaternary landscape development and to distinguishing natural from anthropogenic forcing and processes. In more detail, the aims are to identify and to quantify the impact of past land uses, i.e. changes of vegetation, landforms and soils induced by agriculture and/or forestry. Here, we are presenting latest results from our research and review important findings giving novel insights into man-induced environmental changes in Lusatia within the past thousands years and thus improving the general understanding of Late Quaternary landscape dynamics.}, language = {en} } @misc{SchneiderBonhageHirschetal., author = {Schneider, Anna and Bonhage, Alexander and Hirsch, Florian and Raab, Alexandra and Raab, Thomas}, title = {Accumulation patterns of soil organic matter in forests as a legacy of historical charcoal burning}, series = {EGU General Assembly 2021}, journal = {EGU General Assembly 2021}, doi = {10.5194/egusphere-egu21-5161}, language = {en} } @misc{SchneiderRaabRaabetal., author = {Schneider, Anna and Raab, Thomas and Raab, Alexandra and Sekhri, Simran and Bonhage, Alexander}, title = {Spatial distribution patterns and soil properties of lynchet systems in Northeastern Bavaria, Germany}, series = {EGU General Assembly 2023, Vienna, Austria, 24-28 Apr 2023}, journal = {EGU General Assembly 2023, Vienna, Austria, 24-28 Apr 2023}, doi = {10.5194/egusphere-egu23-6090}, pages = {2}, abstract = {Former field systems (FFS) in recent forest areas of Central and Northern Europe are often discernible by their characteristic morphology with slightly flattened slope areas and intermediary ridges formed by tillage and water erosion. Soils of such lynchet systems feature distinctly modified stratigraphy and properties and thereby constitute a memory of past land use. At the same time, the legacies of past agriculture affect recent forest ecosystems. High-resolution digital elevation models (DEMs) allow to identify lynchets over large areas and open up new opportunities to study the spatial distribution patterns and soils of FFS. Within our research on different land use legacy features in forest areas, we study FFS in Northeastern Bavaria (Germany) in a geopedological approach, combining large-scale mapping and spatial analysis with the description and analysis of soil properties for specific sites. Lynchet areas (and other remnants of pre-industrial FFS) in recent forests were mapped from LIDAR DEMs for an area of 2045 km2 (972 km2 forest area). The mapping results show more than 100 km2 of abandoned field systems within the study area, mostly appearing as lynchet systems. Their spatial distribution patterns differ within the study area, mainly depending on parent material and landform. In the limestone region of the Franconian Jura, FFS occur spatially dispersed, often as considerably small, irregularly shaped parcels, presumably reflecting proceeding abandonment of less productive and accessible fields with intensification of agriculture. In contrast, FFS in the Bohemian Massif in the eastern part of our study area were often found in compounds of many regularly shaped parcels, frequently associated with deserted settlement areas. Soil stratigraphy and properties were studied for FFS and reference positions (forest areas with no indications of former agricultural use) in six study sites, combining detailed characterization of principal soil profiles and an assessment of spatial variations of soil properties in a near-surface sampling approach. First results show that FFS soils are characterized by truncated profiles over most parts of the treads and accumulation of colluvium confined to relatively small areas upslope of lynchet risers. The depth of soil profile truncation and height of lynchet risers differ, mainly related to slope and erodibility of the initial soils. Stratigraphy of the lynchet soils indicates a gradually proceeding formation. Carbon and nitrogen contents were found to differ between FFS and reference soils and to be more homogeneous within the FFS. Carbon contents were mainly lower in the FFS, while both lower and higher nitrogen contents were observed for FFS soils, presumably related to different duration and intensity of agricultural use. Overall, the results show that the legacy effects of past agriculture affect large fractions of recent forest areas, and can be of different quality depending on lithology of the soils' parent material and land use history.}, language = {en} } @misc{SchneiderBonhageRaabetal., author = {Schneider, Anna and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Spatial and temporal variability of soil moisture in land-use legacy forest soils in Brandenburg, Germany}, series = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, journal = {EGU General Assembly 2022, Vienna, Austria, 23-27 May 2022}, doi = {10.5194/egusphere-egu22-2182}, abstract = {Soil physical properties can show high heterogeneity in forest soils, implying a high spatial variability of soil moisture and plant water availability. Legacy effects of past land use, resulting in a small-scale mosaic of anthropogenically modified and unmodified soils in forest areas, further increase this spatial heterogeneity. The soils associated with relict charcoal hearths (RCH), most prominently characterized by a technogenic layer rich in charcoal fragments, are a widespread example for such land use legacy soils in forest areas. The objective of our study was to characterize the soil moisture regime of forest soils and RCH soils on sandy substrates in the northeastern German lowlands; and in particular to assess the long-term effect of the prolonged summer drought period in 2018 on spatial and temporal variability of soil moisture. We monitored matric potentials, soil water contents and soil temperature from June 2018 in forest soils in the Tauersche Forst (Brandenburg, Germany). Three soil profiles (one reference forest soil profile and two characteristic RCH soil profiles) were instrumented, sampled for laboratory analyses of bulk density, pore size distribution, saturated hydraulic conductivity, and persistence of water repellency; and root density distribution in the profiles was recorded. The soils in all profiles show low porosity and plant available water contents. On RCH soils, overall porosity is clearly higher compared with the reference soils, mainly related to larger volumes of coarse and fine pores. Soil moisture monitoring shows very high spatial and temporal variability of the recorded data after the prolonged dry period in 2018, with gradual rewetting over the winter periods and only short-term fluctuations of soil moisture in reaction to high-intensity precipitation events in the summer periods. The comparison of in-situ and laboratory-based water retention data shows strong hysteresis effects during the rewetting, with increasingly clear reactions of soil water contents to precipitation events over the years following the dry period, especially in the charcoal-rich substrates. The differences in soil moisture between the dry and the wetter periods were clearly higher in the RCH soils, which, compared with the reference soils, showed higher water contents under wet conditions and lower water contents under dry conditions. The results affirm that land use legacies can clearly increase the spatial and temporal variations of soil moisture in forest areas.}, language = {en} } @misc{SchneiderHirschBonhageetal., author = {Schneider, Anna and Hirsch, Florian and Bonhage, Alexander and Raab, Alexandra and Raab, Thomas}, title = {The temperature and moisture regime of charcoal-enriched land use legacy soils}, series = {EGU General Assembly 2020}, journal = {EGU General Assembly 2020}, doi = {https://doi.org/10.5194/egusphere-egu2020-2339}, language = {en} } @misc{BonhageHirschRaabetal., author = {Bonhage, Alexander and Hirsch, Florian and Raab, Thomas and Schneider, Anna and Raab, Alexandra and Ouimet, William}, title = {Stratigraphy and shape of relict charcoal hearths in Connecticut, USA}, series = {Anthropogenetische Geomorphologie - Geomorophologie im Anthropoz{\"a}n : Virtuelle Jahrestagung des Arbeitskreises f{\"u}r Geomorphologie 2020, 28./29. September 2020, BTU Cottbus - Senftenberg}, journal = {Anthropogenetische Geomorphologie - Geomorophologie im Anthropoz{\"a}n : Virtuelle Jahrestagung des Arbeitskreises f{\"u}r Geomorphologie 2020, 28./29. September 2020, BTU Cottbus - Senftenberg}, address = {Cottbus}, issn = {2196-4122}, doi = {10.26127/BTUOpen-5363}, pages = {29}, language = {en} } @inproceedings{HirschNicolaySchneideretal., author = {Hirsch, Florian and Nicolay, Alexander and Schneider, Anna and Blaszkiewicz, Miroslaw and Kordowski, Jarosław and Noryskiewicz, Agnieszka M. and Tyszkowski, Sebastian and Raab, Alexandra and Raab, Thomas}, title = {Late Quaternary geomorphodynamics and soil development in Wygonin (Poland)}, series = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie Jahrestagung 2013, 2. - 4.5.2013 BTU Cottbus}, booktitle = {Tagungsband und Exkursionsf{\"u}hrer, Arbeitskreis Geoarch{\"a}ologie Jahrestagung 2013, 2. - 4.5.2013 BTU Cottbus}, publisher = {Brandenburg Univ. of Technology}, address = {Cottbus}, pages = {S. 50}, language = {en} } @misc{RaabRaabSchopper, author = {Raab, Thomas and Raab, Alexandra and Schopper, Franz}, title = {Erfassung und Bewertung von vorindustriellen Meilerstandorten - Workshop 19. Februar 2019}, editor = {Raab, Thomas and Raab, Alexandra and Schopper, Franz}, publisher = {Brandenburgische Technische Universit{\"a}t Cottbus-Senftenberg, Lehrstuhl Geopedologie und Landschaftsentwicklung}, address = {Cottbus}, issn = {2196-4122}, doi = {10.26127/BTUOpen-4817}, pages = {193}, language = {de} } @inproceedings{RaabRaabSchneideretal., author = {Raab, Thomas and Raab, Alexandra and Schneider, Anna and Hirsch, Florian and Nicolay, Alexander and Takla, Melanie and R{\"o}sler, Horst}, title = {Pre-Industrial Charcoal Kilns in the Northern European Lowland - Hidden Land Use Structures Detected by LIDAR}, series = {2014 GSA Annual Meeting in Vancouver, British Columbia (19-22 October 2014)}, booktitle = {2014 GSA Annual Meeting in Vancouver, British Columbia (19-22 October 2014)}, publisher = {Geological Society of America}, address = {Boulder, Colo.}, pages = {S. 96}, language = {en} } @misc{RaabRaabHirschetal., author = {Raab, Thomas and Raab, Alexandra and Hirsch, Florian and Schneider, Anna and Bonhage, Alexander and Aghte, Markus}, title = {Historische K{\"o}hlerei und ihre Hinterlassenschaft - Ein {\"U}berblick}, series = {Erfassung und Bewertung von vorindustriellen Meilerstandorten - Workshop 19. Februar 2019}, journal = {Erfassung und Bewertung von vorindustriellen Meilerstandorten - Workshop 19. Februar 2019}, editor = {Raab, Thomas and Raab, Alexandra and Schopper, Franz}, publisher = {Brandenburgische Technische Universit{\"a}t Cottbus-Senftenberg, Lehrstuhl Geopedologie und Landschaftsentwicklung}, address = {Cottbus}, doi = {10.26127/BTUOpen-4817}, pages = {1 -- 22}, language = {de} } @misc{RaabBonhageSchneideretal., author = {Raab, Thomas and Bonhage, Alexander and Schneider, Anna and Raab, Alexandra and Verschoof-van der Vaart, Wouter and Malik, Ireneusz and Chauhan, Jai Singh and Thekkethala, Jeenus Joby}, title = {Soil distribution and properties on mining relicts in Upper Silesia, Poland - first results from the Mala Panew River catchment and the UNESCO heritage site Tarnowskie G{\´o}ry}, series = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, journal = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, language = {en} } @misc{SchneiderRaabRaabetal., author = {Schneider, Anna and Raab, Thomas and Raab, Alexandra and Sekhri, Simran and Bonhage, Alexander}, title = {Spatial distribution patterns and soil properties of former field systems in Northeastern Bavaria, Germany}, series = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, journal = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, pages = {88}, abstract = {Former field systems (FFS) in sloped forest areas are often discernible by a characteristic morphology with flattened slope areas and intermediary ridges formed by tillage erosion and colluvial redeposition. Soils of such lynchet field systems feature modified stratigraphy and properties and constitute a memory of past land use. At the same time, the legacies of past agriculture affect recent forest ecosystems. High-resolution digital elevation models (DEMs) allow to identify lynchets over large areas and open up new opportunities to study the FFS. Within our research on different land use legacy features in forest areas, we study FFS in Northeastern Bavaria (Germany) in a geopedological approach, combining large-scale mapping and spatial analysis with the description and analysis of soil properties for specific sites. Lynchet systems (and other remnants of pre-industrial FFS) in recent forests were mapped from LIDAR DEMs for an area of 2045 km2 (972 km2 forest area). The results show more than 100 km2 of FFS, mostly appearing as lynchet systems. Their spatial distribution patterns differ within the study area, mainly depending on parent material and landform. Soil stratigraphy and properties were studied for FFS and reference positions in six study sites, combining a characterization of principal soil profiles and an assessment of spatial soil property variations. The FFS soils are characterized by truncated profiles over most parts of the flattened slope areas and accumulation of colluvium upslope of lynchet risers. The depth of soil profile truncation and height of lynchet risers differ, mainly related to slope and erodibility of the initial soils. Stratigraphy of the lynchet soils indicates a gradually proceeding formation by tillage erosion. First results of soil property analyses show that carbon and nitrogen contents differ between FFS and reference soils and are more homogeneous within the FFS. Furthermore, physical properties of the FFS soils (bulk density, pore size distribution, hydraulic conductivity) are modified compared to unaffected forest soils through profile truncation and accumulation of colluvium. Overall, the results show that the legacy effects of past agriculture affect large fractions of recent forest areas, and can be of different quality depending on lithology of the soils' parent material and land use history.}, language = {en} } @misc{RaabRaabBonhageetal., author = {Raab, Thomas and Raab, Alexandra and Bonhage, Alexander and Schneider, Anna}, title = {Relict Charcoal Hearth (RCH) soils - properties and classification}, series = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, journal = {Jahrestagung der Deutschen Bodenkundlichen Gesellschaft, Einladung und Programm Halle (Saale), 2.-8. September 2023}, pages = {88}, language = {en} } @incollection{NicolayRaabRaab, author = {Nicolay, Alexander and Raab, Alexandra and Raab, Thomas}, title = {Die B{\"o}den im Tagebauvorfeld J{\"a}nschwalde - Ergebnisse bodenkundlich-geomorphologischer Untersuchungen}, series = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2011/2012}, booktitle = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2011/2012}, publisher = {Brandenburgisches Landesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Landesmuseum}, address = {W{\"u}nsdorf}, isbn = {978-3-910011-85-4}, pages = {249 -- 256}, language = {de} } @incollection{RoeslerBoenischSchopperetal., author = {R{\"o}sler, Horst and B{\"o}nisch, Eberhard and Schopper, Franz and Raab, Thomas and Raab, Alexandra}, title = {Pre-industrial Carcoal Production in southern Brandenburg and its impact on the environment}, series = {Landscape Archaeology between Art and Science}, booktitle = {Landscape Archaeology between Art and Science}, editor = {Kluiving, Sjoerd and Guttmann-Bond, Erika}, publisher = {Amsterdam University Press}, address = {Amsterdam}, isbn = {978-90-8964-418-3}, pages = {167 -- 178}, language = {en} } @incollection{RaabBruetzkeChristopheletal., author = {Raab, Alexandra and Br{\"u}tzke, W. and Christophel, Dominik and V{\"o}lkel, J{\"o}rg and Raab, Thomas}, title = {Reconstruction of the fire history in the Siedlungskammer Burgweinting (Bavaria, Germany) in relation to settlement and environmental history}, series = {Human Interactions with the Geosphere: The Geoarchaeological Perspective, Geological Society, London}, booktitle = {Human Interactions with the Geosphere: The Geoarchaeological Perspective, Geological Society, London}, editor = {Wilson, Lucy}, publisher = {Geological Soc.}, address = {London}, isbn = {978-1-86239-325-7}, doi = {10.1144/SP352.11}, pages = {137 -- 161}, abstract = {Palaeoenvironmental investigations were carried out in the Siedlungskammer (prehistoric settlement area) Burgweinting (Regensburg, Bavaria, Germany) to reveal past settlement conditions and human impact on the environment. Two sequences were obtained from the Islinger M{\"u}hlbach Fen, in close proximity to the archaeological excavation site in Burgweinting, which documents an almost continuous settlement history since the Neolithic Period. The analyses of the sequences comprise stratigraphic, geochemical and microscopic charcoal analyses. For chronological information, radiocarbon dating was conducted on a total of 10 samples. Thus, the first long-term fire record was reconstructed for the investigation area, and the results were correlated, based on radiocarbon dating, with the available environmental information and settlement history in the Siedlungskammer Burgweinting. The fire record reveals an almost continuous, but alternating fire history. Furthermore, it shows that fire played an important role in the Siedlungskammer Burgweinting and that most probably as early as the Mesolithic hunterer-gatherers deliberately used fire.}, language = {en} } @misc{HirschSchneiderMaatenTheunissenetal., author = {Hirsch, Florian and Schneider, Anna and Maaten-Theunissen, Marieke van der and Maaten, Ernst van der and R{\"a}biger, Christin and Raab, Alexandra and Raab, Thomas}, title = {Soil properties and tree growth at medieval ridge and furrow sites in Brandenburg, northeastern Germany}, series = {Journal of Plant Nutrition and Soil Science}, volume = {186}, journal = {Journal of Plant Nutrition and Soil Science}, number = {4}, issn = {1436-8730}, doi = {10.1002/jpln.202200345}, pages = {417 -- 427}, abstract = {Background Ridge and furrow (RIFU) systems and associated soils are a widespread legacy of medieval agriculture, are archives of historical land use, and might affect recent ecosystems. Open questions about RIFU formation and potential legacy effects still exist, especially related to physical soil properties. Aims Our aims were (1) to characterize the soil properties of RIFU soils and (2) to compare the drought sensitivity and the growth resistance in extremely dry years of trees growing on ridges and furrows, respectively. Methods We studied soil physical (bulk density, saturated soil hydraulic conductivity, and texture) and chemical (soil pH, soil organic matter, and nitrogen content) properties and the climate sensitivity of tree growth on RIFU systems for three study sites in Prignitz, Germany. Results RIFU systems showed a high spatial heterogeneity of soil stratigraphy due to ridge construction and increased accumulation of soil moisture and organic matter in furrows due to post-abandonment pedogenesis. Slight spatial differences in soil physical properties were found, with increased air capacity in ridge soils and higher available water contents in furrow soils. No differences in drought sensitivity were observed for trees growing on ridges and furrows, except for a wet site, where trees in furrows showed a higher sensitivity. Resistance in dry years tended to be similar or increase from furrows to ridges. Conclusions The results reflect a spatial differentiation of stratigraphy and post-abandonment pedogenesis on abandoned RIFU systems and suggest an adaption to different moisture conditions through RIFU construction. Differences in drought sensitivity of tree growth with relative land surface could only be detected for one of the three sites, where trees were found to be less drought sensitive on ridges.}, language = {en} } @misc{BonhageRaabSchneideretal., author = {Bonhage, Alexander and Raab, Thomas and Schneider, Anna and Raab, Alexandra and Ouimet, William and V{\"o}lkel, J{\"o}rg and Ramezany, Shaghayegh}, title = {From site to state - Quantifying multi-scale legacy effects of historic landforms from charcoal production on soils in Connecticut, USA}, series = {Catena}, volume = {232}, journal = {Catena}, issn = {0341-8162}, doi = {10.1016/j.catena.2023.107426}, language = {en} } @misc{HirschBonhageBauriegeletal., author = {Hirsch, Florian and Bonhage, Alexander and Bauriegel, Albrecht and Schneider, Anna and Raab, Thomas and Raab, Alexandra and Gypser, Stella}, title = {The occurrence, soil parameters and genesis of rubified soils ('Fuchserden') of northeastern Germany}, series = {Catena}, volume = {175}, journal = {Catena}, issn = {0008-7769}, doi = {10.1016/j.catena.2018.11.039}, pages = {77 -- 92}, language = {en} } @misc{RaabRaabTaklaetal., author = {Raab, Alexandra and Raab, Thomas and Takla, Melanie and Nicolay, Alexander and B{\"o}nisch, Eberhard and R{\"o}sler, H.}, title = {B{\"o}den als Archive der Landschaftsgeschichte im Vorfeld des Tagebaus J{\"a}nschwalde}, series = {Exkursionsf{\"u}hrer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam}, journal = {Exkursionsf{\"u}hrer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam}, publisher = {Deutsche Bodenkundliche Gesellschaft}, address = {Oldenburg}, pages = {84 -- 96}, language = {de} } @incollection{RaabRaab, author = {Raab, Thomas and Raab, Alexandra}, title = {Imapcts of Early Land Use and Mining on River Landscapes}, series = {World Heritage and Cultural Diversity}, booktitle = {World Heritage and Cultural Diversity}, editor = {Offenh{\"a}ußer, Dieter and Zimmerli, Walther Ch. and Albert, Marie-Theres}, publisher = {German Comm. for UNESCO}, address = {Bonn}, isbn = {978-3-940785-20-6}, pages = {245 -- 261}, language = {en} } @misc{RaabDrohanRaabetal., author = {Raab, Thomas and Drohan, Patrick J. and Raab, Alexandra and Schneider, Anna and Bonhage, Alexander}, title = {A novel view in geopedology : how small landforms from past land use affect the pedosphere}, series = {Centennial Celebration and Congress of the International Union of Soil Sciences}, journal = {Centennial Celebration and Congress of the International Union of Soil Sciences}, publisher = {Florenz}, pages = {1}, abstract = {LiDAR-based high-resolution digital elevation models (DEMs) can now provide a centimetre-accurate image of the Earth's surface. Soil science is still in the early stages of realising how fundamentally this new technology will change our understanding of the formation, properties and functions of the pedosphere and in particular the uppermost part of it, which usually represents A horizons. With the help of high-resolution DEMs, it is possible to identify and classify small topographic features that were previously not considered in soil mapping. Therefore, precise landform analyses will be crucial in assessing variations in soil horizonation and soil stratigraphy and will provide the framework for a new perspective in Geopedology that truly integrates Geomorphology and Pedology from pedon to soil landscapes. In the digital domain, this geopedological approach is growing rapidly by using artificial intelligence (AI) to automatically identify small landforms and visualise the heterogeneity of diverse pedological information. We present the results of the study of different types of relict anthropogenic landforms (RALs) and highlight their characteristics and differences compared to natural, undisturbed soils. The origins of these relict features can vary greatly, as can their distribution, morphology and age. The analysis of high-resolution relief models in Europe and the USA shows that morphological features can be found, particularly in forest that were created in pre-industrial times. Settlement structures (e.g. stone walls, burial sites) or linear relief forms created by soil cultivation (e.g. field terraces, furrow systems) are common. Relict Charcoal Hearths (RCHs), which originate from historic charcoal burning, are usually small circular platforms surrounded by pits or ditches, but can still cover a considerable part of the area. A relatively complex geomorphology can be observed in historic mining areas, which may include different landform types such as mine shafts and spoil heaps, resulting in a very heterogeneous pedological mosaic. To summarise, all studies reveal a high variation of soil properties controlled by small relief structures. Pedology should take this more into account in the future and improve knowledge of the impact of RALs on the pedosphere and other components of ecosystems.}, language = {en} } @incollection{RaabVoelkel, author = {Raab, Alexandra and V{\"o}lkel, J{\"o}rg}, title = {Holocene soil development and pedgenic clay mineral transformation in Luvisols with different development ages at the Viereckschanze of Poign (Central Bavaria, Germany)}, series = {Archaeology, Soil- and Life-Sciences Applied to Enclosures and Fields, Proceedings of the Session 'From microprobe to spatial analysis - Enclosed and buried surfaces as key sources in Archaeology and Pedology'}, booktitle = {Archaeology, Soil- and Life-Sciences Applied to Enclosures and Fields, Proceedings of the Session 'From microprobe to spatial analysis - Enclosed and buried surfaces as key sources in Archaeology and Pedology'}, editor = {Fechner, Kai and Devos, Y. and Leopold, M. and V{\"o}lkel, J{\"o}rg}, publisher = {British Archaeological Reports}, address = {Oxford}, pages = {121 -- 131}, language = {en} } @misc{BonhageSchneiderRaab, author = {Bonhage, Alexander and Schneider, Anna and Raab, Alexandra}, title = {Auf den Spuren der K{\"o}hlermeister Brandenburgs}, series = {arcAKTUELL}, journal = {arcAKTUELL}, number = {3}, issn = {1617-8394}, pages = {45}, language = {de} } @misc{RaabTaklaNicolayetal., author = {Raab, Alexandra and Takla, Melanie and Nicolay, Alexander and Schneider, Anna and R{\"o}sler, Horst and Heußner, Karl-Uwe and B{\"o}nisch, Eberhard}, title = {Pre-industrial charcoal production in Lower Lusatia (Brandenburg, Germany): Detection and evaluation of a large charcoal-burning field by combining archaeological studies, GIS-based analyses of shaded-relief maps and dendrochronological age determination}, series = {Quaternary International}, volume = {Vol. 367}, journal = {Quaternary International}, doi = {10.1016/j.quaint.2014.09.041}, pages = {111 -- 122}, abstract = {In pre-industrial times, charcoal burning was a common source of energy across Europe. Charcoal production and its related consequences for the upland environment are well known due to historical and palaeoenvironmental research. In recent years, awareness has grown regarding the use of woods in the lowlands for charcoal production. In the last 20 years, a large charcoal-burning field in Lower Lusatia (Brandenburg, North German Lowlands) was discovered by systematic archaeological excavations of the opencast mine of J{\"a}nschwalde. However, the excavations are limited to the mine, which only covers a portion of the J{\"a}nschwalder Heide and the surrounding forests. In this paper, we present the results of our study regarding the spatial extension and timing of charcoal production in the J{\"a}nschwalder Heide and its surrounding areas. We applied a combined approach using archaeological research results, GIS-analyses of shaded-relief maps (SRMs) and tree-ring dating of selected charcoal kiln remains. Approximately 900 excavated charcoal kiln ground plans were analysed, which provided a solid data basis for our GIS analyses. For an extensive evaluation, we enlarged our study area beyond the limits of the lignite mine. We identified and digitised the remains of the charcoal kilns by creating SRMs from digital elevation models (DEMs) that were based on high-resolution airborne laser scanning data (ALS). The data from the excavated and digitised charcoal kiln remains were analysed in terms of their sizes and spatial distributions. In addition, the dendrochronological ages of 16 selected charcoal kiln remains were determined. This study shows that charcoal production was more extensive than initially proven by archaeological excavations. The remains of more than 5000 charcoal kilns were detected on the SRMs across an area that was twice as large as the excavated charcoal-burning field. In the J{\"a}nschwalder Heide, considerably more charcoal kiln relicts exist compared with the surrounding communal areas. Furthermore, the charcoal kiln remains in the J{\"a}nschwalder Heide have larger diameters, suggesting large-scale charcoal production for supplying energy to the nearby ironworks at Peitz. However, the charcoal production on the communal land was most likely for local crafts. The ages of the charcoal kiln remains indicated that charcoal production occurred between the 17th and 19th centuries, corresponding with the main period of charcoal burning. Overall, our study suggested that charcoal production sites are underestimated in the modern landscapes of the North German Lowlands.}, language = {en} } @incollection{DeckersEckmeierFrenzeletal., author = {Deckers, Katleen and Eckmeier, Eileen and Frenzel, Peter and Fritzsch, Dagmar and Langan, Carolin and Leierer, Lucia and Metzner, Susan M. and Pint, Anna and Raab, Alexandra and Riehl, Simone and R{\"o}pke, Astrid and Schl{\"u}tz, Frank and Shumilovskikh, Lyudmila S. and Wiedner, Katja}, title = {Analysemethoden}, series = {Geoarch{\"a}ologie}, booktitle = {Geoarch{\"a}ologie}, editor = {Stolz, Christian and Miller, Christopher E.}, publisher = {Springer Spektrum}, address = {Berlin, Heidelberg}, doi = {10.1007/978-3-662-62774-7_15}, pages = {287 -- 335}, abstract = {Die Geoarch{\"a}ologie verf{\"u}gt {\"u}ber ein {\"a}ußerst breites und stetig wachsendes Spektrum an Analysemethoden, die sowohl im Labor als auch im Gel{\"a}nde angewandt werden. Das Kapitel stellt alle gebr{\"a}uchlichen Methoden vor und soll insbesondere Nachwuchswissenschaftlern als Werkzeugkasten dienen. Zun{\"a}chst liegt der Fokus auf den bodenkundlich-geomorphologischen Standardmethoden, wie Korngr{\"o}ßenanalyse (Bodenart), Bodenfarbe, Gehalt an organischer Substanz, Carbonatgehalt, Bodenreaktion (pH) und vielf{\"a}ltigen Multielement-Analysen zur L{\"o}sung verschiedener Fragestellungen. F{\"u}r die Pal{\"a}oumweltforschung haben die Pollenanalyse sowie die Analyse von Nichtpollen-Palynomorphen (NPP) schon seit vielen Jahrzehnten eine große Bedeutung. F{\"u}r gr{\"o}ßere biogene Reste stehen die Makrorestanalyse und die Anthrakologie zur Untersuchung von Holzkohlen zur Verf{\"u}gung. Weiterhin beschreibt das Kapitel die Methode der Mikromorphologie (D{\"u}nnschliffe), die Analyse von Biomarkern und stabilen Isotopen sowie die Bestimmung und Einordnung von Foraminiferen und Ostrakoden aus aquatischen {\"O}kosystemen. Beschrieben werden außerdem Ans{\"a}tze zu Phytolithen und Messungen mithilfe der Fourier-Tranformations-Infrarotspektrometrie (FTIR).}, language = {de} } @inproceedings{RaabSchneiderBonhageetal., author = {Raab, Alexandra and Schneider, Anna and Bonhage, Alexander and Takla, Melanie and Hirsch, Florian and M{\"u}ller, Frank and R{\"o}sler, Horst and Heußner, Karl-Uwe}, title = {Spatial analysis of charcoal kiln remains in the former royal forest district Tauer (Lower Lusatia, North German Lowlands)}, series = {European Geosciences Union, General Assembly 2016, Vienna, Austria}, booktitle = {European Geosciences Union, General Assembly 2016, Vienna, Austria}, publisher = {European Geophysical Society}, address = {Katlenburg-Lindau}, abstract = {Archaeological excavations have revealed more than thousand charcoal kiln remains (CKRs) in the prefield of the active opencast lignite mine J{\"a}nschwalde, situated about 150 km SE of Berlin (SE Brandenburg, Germany). The charcoal was mainly produced for the ironwork Peitz nearby, which operated from the 16th to the mid-19th centuries. In a first approach, to estimate the dimension of the charcoal production, CKRs were mapped on shaded-relief maps (SRMs) derived from high-resolution LiDAR data (Raab et al. 2015). Subsequently, for a selected test area, identified CKRs on the SRMs were compared with archaeologically excavated CKRs in the field. This survey showed a considerably number of falsely detected sites. Therefore, the data was critically re-evaluated using additional relief visualisations. Further, we extended the CKR mapping to areas which are not archaeologically investigated. The study area, the former royal forest district Tauer, consists of two separate areas: the Tauersche Heide (c. 96 km2 area) N of Peitz and the area J{\"a}nschwalde (c. 32 km2 area) NE of Peitz. The study area is characterized by a flat topography. Different former and current anthropogenic uses (e.g., military training, solar power plant, forestry measures) have affected the study area, resulting in extensive disturbances of the terrain surface. The revised CKR abundance in the study area J{\"a}nschwalde was considerably smaller than the numbers produced by our first approach. Further, the CKR mapping revealed, that a total record of the CKRs is not possible for various reasons. Despite these limitations, a solid database can be provided for a much larger area than before. Basic statistic parameters of the CKR diameters and all comparative statistical tests were calculated using SPSS. To detect underlying spatial relationships in the CKR site distribution, we applied the Getis-Ord Gi* statistic, a method to test for local spatial autocorrelation between neighbouring sites. The test is available as part of the ArcGis 10.1 spatial statistics toolbox. The outcomes are discussed in consideration of our archaeological, archival and dendrochronological research results.}, language = {en} } @incollection{NicolayRaab, author = {Nicolay, Alexander and Raab, Alexandra}, title = {Sedimentabfolge und -merkmale eines Aufschlusses der Dryas-Fundstelle Dissenchen 18}, series = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2011/2012}, booktitle = {Ausgrabungen im Niederlausitzer Braunkohlenrevier 2011/2012}, publisher = {Brandenburgisches Landesamt f{\"u}r Denkmalpflege und Arch{\"a}ologisches Landesmuseum}, address = {W{\"u}ndsdorf}, isbn = {978-3-910011-85-4}, pages = {177 -- 178}, language = {de} }