@misc{EltaherBonhageRaabetal., author = {Eltaher, Mahmoud and Bonhage, Alexander and Raab, Thomas and Breuß, Michael}, title = {A modified Mask R-CNN approach for automated detection of archaeological sites on high resolution LiDAR-derived DEMs}, 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}, publisher = {Cottbus}, issn = {2196-4122}, doi = {10.26127/BTUOpen-5363}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:co1-opus4-53633}, pages = {50}, language = {en} } @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{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{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} } @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{DrohanBayuzickDiefenbachetal., author = {Drohan, Patrick J. and Bayuzick, Samuel and Diefenbach, Duane and McDill, Marc and Raab, Thomas and Hirsch, Florian and Bonhage, Alexander}, title = {Northern Appalachian, USA relic charcoal hearths and their unique Ecological Fingerprint}, series = {EGU General Assembly 2021}, journal = {EGU General Assembly 2021}, doi = {10.5194/egusphere-egu21-13618}, language = {en} } @misc{BayuzickDrohanRaabetal., author = {Bayuzick, Samuel and Drohan, Patrick J. and Raab, Thomas and Hirsch, Florian and Bonhage, Alexander and McDill, Marc and Diefenbach, Duane}, title = {Relic charcoal hearths geomorphology and hydrology in mid-Appalachian region of Pennsylvania}, series = {EGU General Assembly 2021}, journal = {EGU General Assembly 2021}, doi = {10.5194/egusphere-egu21-6243}, language = {en} } @misc{BonhageBayuzickDrohanetal., author = {Bonhage, Alexander and Bayuzick, Samuel and Drohan, Patrick J. and Hirsch, Florian and Raab, Thomas}, title = {Relict charcoal hearth landscape and soil profile characteristics surrounding a mid-19th century Appalachian iron furnace}, series = {EGU General Assembly 2021}, journal = {EGU General Assembly 2021}, doi = {10.5194/egusphere-egu21-5691}, language = {de} } @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{RamezanySutLohmannKlosetal., author = {Ramezany, Shaghayegh and Sut-Lohmann, Magdalena and Klos, Friederike and Bonhage, Alexander and Raab, Thomas}, title = {Using Modified Tessier Scheme to Metal Speciation in a Former Sewage Farm and interpretation of the sequential extraction by FTIR}, series = {EGU General Assembly 2021}, journal = {EGU General Assembly 2021}, doi = {10.5194/egusphere-egu21-6482}, language = {de} } @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} } @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{DrohanBayuzickGuarinetal., author = {Drohan, Patrick J. and Bayuzick, Samuel and Guarin, Daniel and Raab, Thomas and Bonhage, Alexander and Diefenbach, Duane and McDill, Marc}, title = {USA Appalachian relict charcoal hearths have complex landscape and pedologic patterns that are unique from surrounding forest 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-egu22-10315}, abstract = {Understanding how present-day abrupt change may alter forest ecosystem services is becoming more important due to ever-growing anthropogenic stresses. Forest managers trying the adapt to anthropogenic stress can benefit from the study and quantification of past abrupt changes in forests, especially when the legacy of past disturbance is still evident. Across the United Kingdom, Europe, and recently the northeastern United States, the examination of historic forest change due to charcoal manufacturing for the firing of iron or lime furnaces is yielding new insights relative to landscape stability, anthropogenic vs natural soil genesis, and forest evolution. A landscape classification process was used in the Central Appalachians (Pennsylvania) to identify 6,758 RCHs near Greenwood Furnace (Greenwood Furnace State Park) and Pine Grove Furnace (Pine Grove Furnace State Park). Topographic wetness index (TWI), and SAGA wetness index (SWI) were created using ~1m LiDAR data for two study areas to quantify surface hydrology effects and were compared to field soil volumetric water content (VWC) measurements. Modeled TWI and SWI values were different for RCH areas when compared to surrounding non-hearth areas indicating that RCHs were acting as a moisture sink. We also found that RCH platforms have different TWI and SWI values than rim areas. Using field measured volumetric water content, we found that as distance from the center of the RCH increases, the drier the soil becomes. Geomorphic position did not affect wetness. Surface soil samples were collected at 51 RCHs in the Greenwood Furnace study area. Laboratory analyses revealed that RCH soils have higher C content than surrounding native soils. Furthermore, while the pH of RCH soils is like native soils, the acidity is greater in RCHs. RCH soils at Greenwood Furnace were found to have lower Mehlich 3 P concentrations and lower K potentially effecting plant growth. RCH soils were found to have higher Ca concentration when compared to native soils. To examine within RCH differences in soil chemistry and morphology more closely, 8 of the 51 RCHs were sampled intensely along a topographic gradient. Control pits were excavated directly upslope from the RCHs. The RCHs were sampled in 5 positions across the hearth from the upslope to down slope position (A upslope rim of the RCH; B halfway point between A and C; C RCH center; D halfway C and E; E downslope rim of the RCH). Soil profiles were described and sampled at each position. The soil samples were analyzed for trace and rare earth element content (Aqua Regia digestion), soil pH (water) and fertility (Mehlich 3 extraction). Results indicated that RCHs are potentially a unique location of refugia for forest flora and perhaps fauna due to the unique geochemistry with higher bases and C and some concentrated metals and a higher soil water content hypothesized to be due to an observed restrictive morphology. Future research should more closely investigate whether RCHs support unique species assemblages and how they may play a role in enhancing today's forest biodiversity.}, 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} } @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{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{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{RamezanyBonhageRaab, author = {Ramezany, Shaghayegh and Bonhage, Alexander and Raab, Thomas}, title = {Comparing prediction algorithms in FTIR-based chemometric analysis to predict soil variables within centuries-old charcoal rich Technosols}, 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-egu22-5507}, abstract = {As an alternative to the costly wet chemical analysis of soil, Machine Learning (ML) algorithms can be applied for the quantification of soil properties through prediction models. In this study, we evaluate the performances of the Random Forest (RF) algorithm and Partial Least Square Regression (PLSR), in the prediction of soil variables, including CEC, pH, total contents of C and N as wells as other elements (Al, Fe, Ca, Mn, Mg, K, and Na) based on FTIR-spectra of Relict Charcoal Hearth (RCH) soils and reference forest soils (Non-RCH). We investigate the effect of high quantities of charcoal in the soil on the prediction models. Preliminary results suggest that there is no significant difference in the results of prediction models for total N, C, and Fe contents, while the accuracy of PLSR in the prediction of pH, Mg, and Ca, and RF performance in prediction of pH and C decreased for RCH soils. Both algorithms demonstrate higher accuracies in the prediction of Al within the RCH soils. Prediction of CEC, Na, K, Mg (RF) within the RCH soils, Al (PLSR) for Non-RCH soils, and Mn and Ca (RF) for both soil types resulted in lower quality of predictions. It can be inferred from the results that the performance of FTIR-based prediction models can be affected by the presence of charcoal in soil due to the nature of spectral features reflecting the soil composition. The presence of charcoal in soil likely alters the absorption interference and peak overlaps, which can result in lower accuracy of the prediction models. In addition to the accuracy of the prediction models, we evaluate the reliability of the weighted wavenumbers (as important variables) in each prediction, which provides information about the correlation of spectral features and chemical properties. It can be studied through the Variable Importance Plot in RF and Variable Importance on Projection through PLSR (VIPs), which show high potential for studying soil composition and metal distribution in mineral and organic soil fractions despite the observed weaknesses in weighing wavenumbers in predictions. Therefore, we assess and compare the quality of information gained regarding soil chemical properties from the algorithms besides a sole quantification of soil parameters. Furthermore, we applied the developed prediction models on a large number (n > 600) of FTIR-spectra of RCH soils to investigate the practical application of the models and thereby compare spectral derived chemical properties of the studied Technosols and reference forest soils.}, 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{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} } @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} } @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} } @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} } @misc{BayuzickGuarinBonhageetal., author = {Bayuzick, Samuel and Guarin, Daniel and Bonhage, Alexander and Hirsch, Florian and Diefenbach, Duane and McDill, Marc and Raab, Thomas and Drohan, Patrick J.}, title = {Small anthropogenic landforms from past charcoal production control moisture dynamics and chemistry in northcentral Appalachian soils}, series = {Geomorphology}, volume = {415}, journal = {Geomorphology}, issn = {1872-695X}, doi = {10.1016/j.geomorph.2022.108379}, pages = {1 -- 11}, abstract = {Throughout the northeastern United States (U.S.) and Europe, relict charcoal hearths (RCHs) are regularly being discovered in proximity to furnaces once used for the extraction of metal from ore or quick-lime production; charcoal produced in hearths was used as a furnace fuel. Given previous research has shown that topographic and subsurface disturbance can be great when a hearth is constructed, we hypothesize that hearth construction alters surface hydrology and soil chemistry in environments in and near hearths. We used a landscape classification process to identify 6758 hearths near furnaces at Greenwood and Pine Grove Furnace State Park, central and southcentral Pennsylvania, U.S. Two types of digital elevation model wetness indexes were used to quantify surface hydrology effects in and around hearths. Modeled wetness conditions were compared to field soil volumetric water content in RCHs near Greenwood Furnace State Park. Modeled wetness indexes indicate that RCH interiors are significantly wetter than RCH rim areas; RCHs are acting as a landscape moisture sink. Results also indicate that RCHs on slopes result in downslope drier conditions below RCHs. Field measured volumetric water content indicates that as distance from the center of the hearth increases, soil moisture significantly decreases. Geomorphic position was found to not be related to RCH wetness. Soil from RCHs, compared to nearby native soils, has significantly higher total C, a lower Mehlich 3 extractable acidity, higher Ca and P. No trend was evident with RCH soil chemistry and geomorphic position. The high frequency of RCH occurrence, in proximity to the furnace's RCHs supported, suggests that RCHs today could locally be an important niche for understory flora and fauna. Further research could explore how RCHs might be affecting surrounding plant populations and how within RCH patterns, especially on hillslopes, might represent a distinctly different scale of physical and chemical variability.}, language = {en} } @misc{BayuzickGuarinBenavidesetal., author = {Bayuzick, Samuel and Guarin, Daniel and Benavides, Jhony and Bonhage, Alexander and Hirsch, Florian and Diefenbach, Duane and McDill, Marc and Raab, Thomas and Drohan, Patrick J.}, title = {Soil and geomorphic patterns within relict charcoal hearths could represent unique ecosystem niches}, series = {Geomorphology}, volume = {422}, journal = {Geomorphology}, issn = {1872-695X}, doi = {10.1016/j.geomorph.2022.108525}, pages = {1 -- 16}, abstract = {Hearths used for 19th and 20th century charcoal manufacturing have been found to have unique plant communities or to produce unique growth characteristics for some species but not others. Given known differences in hearth morphology, within hearth physical and chemical differences may exist and result in unique ecologic niches. We examined soil stratigraphy across 8 relict charcoal hearths (RCH) and control soils on different landforms near a 19th century furnace complex (Greenwood Furnace, northcentral Appalachians USA). Soils were analyzed for particle size, total and trace elements, and fertility. Platform creation resulted in soils from upslope RCH positions mixed with subsurface materials on the downslope side to create a stabilized platform. The thin, uniform thickness of charcoal surface horizons (Ac) indicate that RCHs were not used more than once for charcoal manufacturing or that charcoal was always removed very efficiently. While rubification of soil or rock from high heat was seen in 6 of 8 sites sampled, it was not extensive across sampled areas of any one hearth, which indicate hearth use may not be frequent, hot enough, or spatially disparate. Soil fertility characteristics change within RCHs but also by landscape position. Downslope RCH positions are enriched in some parameters compared to control soils (total C, Mehlich 3 Mg, Ca, and Aquia Regia digestion Mn) and that enrichment often is from the surface downward. Downslope enrichment within RCH soils may have occurred from charcoal and released ions, slope erosion and accumulation, or transportation of constructed materials during RCH creation. Landscape position may accentuate or mute soil chemistry differences. Greenwood Furnace RCHs have unique patterns of chemistry, which could result in unique niches for flora and maybe fauna within RCH. Future research could more closely investigate whether hearths support unique species assemblages and how they may play a role in enhancing today's forest biodiversity.}, 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{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} } @misc{SchneiderRaabRaabetal., author = {Schneider, Anna and Raab, Thomas and Raab, Alexandra and Bonhage, Alexander}, title = {Legacies of past land use : mapping anthropogenic landforms in forest areas of eastern Bavaria, Germany}, series = {Geoarchaeology}, volume = {40 (2025)}, journal = {Geoarchaeology}, number = {1}, publisher = {Wiley}, issn = {0883-6353}, doi = {10.1002/gea.22032}, pages = {1 -- 18}, abstract = {Reconstructing (pre-)historic land use distribution is essential for understanding past human societies and their impacts on the environment. Various land use forms result in distinct alterations of surface morphology, which are often well preserved but rarely described within forest areas. The interpretation of LiDAR Digital Elevation Models (DEMs) can greatly enhance our insight into the geoarchaeological records of woodlands. This study examines the legacies of past land use in forested areas of Upper Palatinate, Germany, utilizing LiDAR DEMs to map anthropogenic relief features. We comprehensively mapped land use legacy landforms (LULLs) that occur with considerable frequency in the study area, that is, former agricultural field systems, road remnants, abandoned ponds, relict charcoal hearths, mining legacies, and indicators of anthropogenically induced soil erosion. Results reveal that 17\% of the forested area is affected by LULLs, with the largest areas covered by former field systems, roads, and ponds. Characteristic LULL associations reflect past agricultural and charcoal production landscapes. While erosion indicators often coincide with field systems and roads, natural factors mainly influence their distribution. Comparison with historical maps suggests pre-19th-century abandonment of most LULLs and good preservation of anthropogenic relief modifications. Our results underscore the enduring impact of past land use on present woodland ecosystems and emphasize the importance of considering forest areas in the analysis of past human-landscape interactions.}, language = {en} } @misc{SchneiderRaabRaabetal., author = {Schneider, Anna and Raab, Thomas and Raab, Alexandra and Bonhage, Alexander}, title = {Anthropogene Kleinreliefformen als Relikte fr{\"u}herer Landnutzung - Großfl{\"a}chige Kartierung aus digitalen Gel{\"a}ndemodellen}, series = {Pangeo / DEUQUA 2024 Abstracts}, journal = {Pangeo / DEUQUA 2024 Abstracts}, pages = {159 -- 159}, abstract = {Die direkten Auswirkungen menschlicher Landnutzung auf B{\"o}den und Sedimente betreffen h{\"a}ufig nur wenige Dezimeter Tiefe unter der Erdoberfl{\"a}che, erstrecken sich horizontal aber sehr weitr{\"a}umig. Indirekte anthropogene Einfl{\"u}sse auf geomorphologische und hydrologische Prozesse als ein Merkmal des Anthropoz{\"a}ns ergeben sich als kumulative Auswirkungen solcher wenig intensiven, aber großfl{\"a}chigen Eingriffe. Viele Landnutzungsformen hinterlassen charakteristische anthropogene Reliefver{\"a}nderungen und Kleinreliefformen, die in hochaufl{\"o}senden digitalen Gel{\"a}ndemodellen (DEMs) abgebildet sind. Die Auswertung von DEMs erm{\"o}glicht es damit, anthropogene Kleinreliefformen {\"u}ber große Areale zu erkennen und so (pr{\"a}-)historische Landnutzung zu lokalisieren und hinsichtlich ihrer fl{\"a}chenhaften Verbreitung und Verteilungsmuster zu beschreiben. W{\"a}hrend sich die technischen M{\"o}glichkeiten zur DEM-Auswertung v.a. durch KI-gest{\"u}tzte Methoden rapide weiterentwickeln, bleiben vielfach Unsicherheiten hinsichtlich der zeitlichen Klassifizierung und Repr{\"a}sentativit{\"a}t der erfassten Formen. Wir pr{\"a}sentieren Ergebnisse aus mehreren Fallstudien, in denen anthropogene Kleinreliefformen aus DEMs großfl{\"a}chig kartiert und erg{\"a}nzt durch bodenkundliche und sedimentologische Untersuchung morphogenetisch interpretiert wurden. Diese Studien konzentrieren sich auf Relikte der Holzkohleproduktion, des Bergbaus und der landwirtschaftlichen Nutzung in Untersuchungsgebieten in Brandenburg, Nordbayern, Schlesien, Nordwestirland und dem Nordosten der USA. Unsere Ergebnisse zeigen durchwegs eine große Verbreitung anthropogener Kleinreliefformen in rezenten Waldgebieten und damit einen erheblichen Einfluss fr{\"u}herer Landnutzung auf aktuelle Bodenlandschaften. W{\"a}hrend Relikte der historischen Holzkohleproduktion nur vereinzelt mit Bodenerosion in Verbindung stehen, zeigt sich f{\"u}r Kleinreliefformen aus Bergbau und Ackerbau h{\"a}ufiger ein Zusammenhang mit anthropogen beeinflusster Morphodynamik. Die Fallstudien zeigen auch Effekte der {\"U}berpr{\"a}gung und eine Tendenz zur Abbildung {\"u}berwiegend j{\"u}ngerer Landnutzungsrelikte in DEMs und unterstreichen damit, dass f{\"u}r ein Verst{\"a}ndnis von Mensch-Umwelt Interaktionen die DEM-gest{\"u}tzte Rekonstruktion der vergangenen Landnutzung mit Auswertung weiterer Geoarchive kombiniert werden muss.}, language = {de} } @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{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{VerschoofvanderVaartBonhageSchneideretal., author = {Verschoof-van der Vaart, Wouter and Bonhage, Alexander and Schneider, Anna and Ouimet, William and Raab, Thomas}, title = {Automated large-scale mapping and analysis of relict charcoal hearths in Connecticut (USA) using a Deep Learning YOLOv4 framework}, series = {Archaeological Prospection}, volume = {30}, journal = {Archaeological Prospection}, number = {3}, issn = {1099-0763}, doi = {10.1002/arp.1889}, pages = {251 -- 266}, 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{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{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} } @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{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{BonhageRaabDrohanetal., author = {Bonhage, Alexander and Raab, Thomas and Drohan, Patrick and Schneider, Anna and Raab, Alexandra}, title = {An initial geopedological survey and description of historic raised beds in north-western Ireland}, series = {Geomorphology}, volume = {481}, journal = {Geomorphology}, publisher = {Elsevier}, issn = {1872-695X}, doi = {https://doi.org/10.1016/j.geomorph.2025.109778}, pages = {1 -- 12}, abstract = {Raised Bed (RB) field structures in northwestern Ireland are historical relics of widespread agriculture before and during the Great Famine in the mid-19th century. Their primary purpose was to improve drainage on shallow, waterlogged soils for cultivation of crops. Today, the undulating surface morphology created by the ridges and furrows remains visible in many locations, raising questions about how many of these historic fields actually still exist, whether they are mappable, and if their soils have undergone persistent anthropogenic changes. In this study, we analyse three different RB sites located in varying topographical positions and on different parent materials. High-resolution digital elevation models (DEMs) are created using UAV-based photogrammetry to analyse the surface morphology and model surface flow accumulation and wetness. Soils are analysed using trenches and surface samples taken from ridges and furrows. Our results indicate that satellite or aerial imagery alone is insufficient for reliably detecting RB sites, as the height difference between ridges and furrows is too subtle. Ridge spacing and furrow depth are best observed using high-resolution DEMs (<50 cm cell size). The modelled surface hydrology suggests that the drainage function of RB sites remains, with furrows retaining more moisture than ridges. This can have significant implications for microhabitat structures within RB fields, potentially influencing faunal species composition and abundance. Furthermore, we find significant differences in specific elemental concentrations between soils on ridges and soils on furrows, as well as differences in grain size distributions. These findings indicate a wide range of potential legacy effects present in RB fields that merit further investigation.}, language = {en} } @misc{BonhageRaabRaabetal., author = {Bonhage, Alexander and Raab, Thomas and Raab, Alexandra and Schneider, Anna and Malik, Ireneusz and Wistuba, Malgorzata and Verschoof-van der Vaart, Wouter}, title = {Land use legacy landforms at the UNESCO Heritage Site Tarnowskie G{\´o}ry, Upper Silesia, Poland : stratigraphy, soils and age}, series = {Geoarchaeology}, volume = {40}, journal = {Geoarchaeology}, number = {1}, publisher = {Wiley}, issn = {1520-6548}, doi = {https://doi.org/10.1002/gea.22028}, pages = {1 -- 8}, abstract = {Metallurgy in Upper Silesia (Poland) has a long tradition of international significance, which was emphasized in 2017 when the historic silver mine in Tarnowskie G{\´o}ry was inscribed as a UNESCO World Heritage site. The area consists of various anthropogenic landforms, the stratigraphy of which has hardly been studied so far. In this study, we describe five main morphological units: Unit I (RCH) and Unit II (RCH pit), resulting from charcoal production; Unit III (shaft) and Unit IV (shaft heap), resulting from mining; and Unit V (reference forest soil). The first four units are a variation of a Technosol with inherently different properties from the reference forest soil. Unit I exhibits typical properties of a relict charcoal hearth (RCH), whereas Unit II resembles a pit. Unit III consists of a mostly infilled mining shaft remain (MSR), characterized by relocated subsoil. Unit IV consists of material from the adjacent Unit III that has been dumped directly aside. The studied RCH was used no earlier than during the second half of the 17th century, probably between 1725 and 1813. The studied MSR was used most likely between the 3rd and 5th centuries, which is much older than described so far. Together, the units reflect the characteristic heterogeneity of soils in shaft mining and RCH areas.}, 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} } @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} } @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{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} } @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{HolmerBőszeBonhageetal., author = {Holmer, Anna and Bősze, Ildik{\´o} and Bonhage, Alexander and Susanne, Lindauer and G{\"u}nther, Moosbauer and P{\"o}llath, Nadja and Kristina, Reetz and J{\"o}rg, V{\"o}lkel}, title = {Prehistoric slot pits on a loess covered Rissian Danube terrace at Straubing (SE Bavaria) - structures for fat tanning?}, series = {Journal of geomorphology : journal of basic and applied geomorphology}, volume = {2}, journal = {Journal of geomorphology : journal of basic and applied geomorphology}, number = {1}, publisher = {Borntraeger Science Publishers}, address = {Stuttgart}, doi = {10.1127/jgeomorphology/0874}, pages = {67 -- 129}, abstract = {Slot pits are uniquely shaped pits linked to prehistoric settlements in Central Europe, some dating back to the Mesolithic. They are typically long, deep, and narrow, yet their exact function remains unclear despite extensive research. This study aims to synthesize previous archaeological and pedological findings regarding slot pits and refine hypotheses about their function and age. Samples were collected from slot pits, other pit types, and surrounding loess at an excavation site in Straubing-Lerchenhaid, Bavaria, covering periods from the Linear Pottery Culture to the Iron Age. Pedological analysis indicated that the slot pits were not filled with material from nearby chernozemic horizons, and that no measured element was enriched in slot pits but not other pit types. Radiometric dating of bulk sediment samples, charcoal and animal remains, suggested ages ranging from the End Mesolithic to the End Neolithic. Although biomarker analyses showed traces of human faeces, they were not significant enough to suggest that the pits were primarily used as latrines, which was supported by the lack of elevated phosphorus levels in pit samples. A combination of these findings leads to the hypothesis that slot pits may have been utilized in the fat tanning process.}, language = {en} } @misc{SchneiderRaabRaabetal., author = {Schneider, Anna and Raab, Thomas and Raab, Alexandra and Bonhage, Alexander}, title = {Soils of former field systems in Northeastern Bavaria, Germany}, doi = {10.17632/59932w7yct.1}, abstract = {Analytical data for bulk soil samples from former field system and reference areas in forests of Northeastern Bavaria, Germany. Profile samples taken following soil horizons, transect samples taken in fixed 10 cm depth ranges.}, language = {en} }