TY - GEN A1 - Bonhage, Alexander A1 - Raab, Thomas A1 - Schneider, Anna A1 - Raab, Alexandra A1 - Ouimet, William A1 - Völkel, Jörg A1 - Ramezany, Shaghayegh T1 - From site to state – Quantifying multi-scale legacy effects of historic landforms from charcoal production on soils in Connecticut, USA T2 - Catena Y1 - 2023 U6 - https://doi.org/10.1016/j.catena.2023.107426 SN - 0341-8162 VL - 232 ER - TY - GEN A1 - Hirsch, Florian A1 - Bonhage, Alexander A1 - Bauriegel, Albrecht A1 - Schneider, Anna A1 - Raab, Thomas A1 - Raab, Alexandra A1 - Gypser, Stella T1 - The occurrence, soil parameters and genesis of rubified soils (‘Fuchserden’) of northeastern Germany T2 - Catena Y1 - 2019 U6 - https://doi.org/10.1016/j.catena.2018.11.039 SN - 0008-7769 SN - 1872-6887 VL - 175 SP - 77 EP - 92 ER - TY - GEN A1 - Raab, Alexandra A1 - Raab, Thomas A1 - Takla, Melanie A1 - Nicolay, Alexander A1 - Bönisch, Eberhard A1 - Rösler, H. T1 - Böden als Archive der Landschaftsgeschichte im Vorfeld des Tagebaus Jänschwalde T2 - Exkursionsführer, Jahrestagung der Deutschen Bodenkundlichen Gesellschaft 2011, September 2011, Berlin, Potsdam Y1 - 2011 SP - 84 EP - 96 PB - Deutsche Bodenkundliche Gesellschaft CY - Oldenburg ER - TY - CHAP A1 - Raab, Thomas A1 - Raab, Alexandra ED - Offenhäußer, Dieter ED - Zimmerli, Walther Ch. ED - Albert, Marie-Theres T1 - Imapcts of Early Land Use and Mining on River Landscapes T2 - World Heritage and Cultural Diversity Y1 - 2010 SN - 978-3-940785-20-6 SP - 245 EP - 261 PB - German Comm. for UNESCO CY - Bonn ER - TY - GEN A1 - Raab, Thomas A1 - Drohan, Patrick J. A1 - Raab, Alexandra A1 - Schneider, Anna A1 - Bonhage, Alexander T1 - A novel view in geopedology : how small landforms from past land use affect the pedosphere T2 - Centennial Celebration and Congress of the International Union of Soil Sciences N2 - 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. Y1 - 2024 UR - https://www.researchgate.net/publication/380912417_A_NOVEL_VIEW_IN_GEOPEDOLOGY_HOW_SMALL_LANDFORMS_FROM_PAST_LAND_USE_AFFECT_THE_PEDOSPHERE PB - Florenz ER - TY - CHAP A1 - Raab, Alexandra A1 - Völkel, Jörg ED - Fechner, Kai ED - Devos, Y. ED - Leopold, M. ED - Völkel, Jörg T1 - Holocene soil development and pedgenic clay mineral transformation in Luvisols with different development ages at the Viereckschanze of Poign (Central Bavaria, Germany) T2 - 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' Y1 - 2011 SP - 121 EP - 131 PB - British Archaeological Reports CY - Oxford ER - TY - GEN A1 - Bonhage, Alexander A1 - Schneider, Anna A1 - Raab, Alexandra T1 - Auf den Spuren der Köhlermeister Brandenburgs T2 - arcAKTUELL Y1 - 2015 UR - http://arcaktuell.de/03-2015/#/45 SN - 1617-8394 SN - 1617-8408 IS - 3 SP - 45 ER - TY - GEN A1 - Raab, Alexandra A1 - Takla, Melanie A1 - Nicolay, Alexander A1 - Schneider, Anna A1 - Rösler, Horst A1 - Heußner, Karl-Uwe A1 - Bönisch, Eberhard T1 - 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 T2 - Quaternary International N2 - 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 Jänschwalde. However, the excavations are limited to the mine, which only covers a portion of the Jänschwalder 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 Jänschwalder 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 Jänschwalder Heide, considerably more charcoal kiln relicts exist compared with the surrounding communal areas. Furthermore, the charcoal kiln remains in the Jänschwalder 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. Y1 - 2015 U6 - https://doi.org/10.1016/j.quaint.2014.09.041 VL - Vol. 367 SP - 111 EP - 122 ER - TY - CHAP A1 - Deckers, Katleen A1 - Eckmeier, Eileen A1 - Frenzel, Peter A1 - Fritzsch, Dagmar A1 - Langan, Carolin A1 - Leierer, Lucia A1 - Metzner, Susan M. A1 - Pint, Anna A1 - Raab, Alexandra A1 - Riehl, Simone A1 - Röpke, Astrid A1 - Schlütz, Frank A1 - Shumilovskikh, Lyudmila S. A1 - Wiedner, Katja ED - Stolz, Christian ED - Miller, Christopher E. T1 - Analysemethoden T2 - Geoarchäologie N2 - Die Geoarchäologie verfügt über ein äußerst breites und stetig wachsendes Spektrum an Analysemethoden, die sowohl im Labor als auch im Gelände angewandt werden. Das Kapitel stellt alle gebräuchlichen Methoden vor und soll insbesondere Nachwuchswissenschaftlern als Werkzeugkasten dienen. Zunächst liegt der Fokus auf den bodenkundlich-geomorphologischen Standardmethoden, wie Korngrößenanalyse (Bodenart), Bodenfarbe, Gehalt an organischer Substanz, Carbonatgehalt, Bodenreaktion (pH) und vielfältigen Multielement-Analysen zur Lösung verschiedener Fragestellungen. Für die Paläoumweltforschung haben die Pollenanalyse sowie die Analyse von Nichtpollen-Palynomorphen (NPP) schon seit vielen Jahrzehnten eine große Bedeutung. Für größere biogene Reste stehen die Makrorestanalyse und die Anthrakologie zur Untersuchung von Holzkohlen zur Verfügung. Weiterhin beschreibt das Kapitel die Methode der Mikromorphologie (Dünnschliffe), die Analyse von Biomarkern und stabilen Isotopen sowie die Bestimmung und Einordnung von Foraminiferen und Ostrakoden aus aquatischen Ökosystemen. Beschrieben werden außerdem Ansätze zu Phytolithen und Messungen mithilfe der Fourier-Tranformations-Infrarotspektrometrie (FTIR). Y1 - 2022 U6 - https://doi.org/10.1007/978-3-662-62774-7_15 SP - 287 EP - 335 PB - Springer Spektrum CY - Berlin, Heidelberg ER - TY - CHAP A1 - Raab, Alexandra A1 - Schneider, Anna A1 - Bonhage, Alexander A1 - Takla, Melanie A1 - Hirsch, Florian A1 - Müller, Frank A1 - Rösler, Horst A1 - Heußner, Karl-Uwe T1 - Spatial analysis of charcoal kiln remains in the former royal forest district Tauer (Lower Lusatia, North German Lowlands) T2 - European Geosciences Union, General Assembly 2016, Vienna, Austria N2 - Archaeological excavations have revealed more than thousand charcoal kiln remains (CKRs) in the prefield of the active opencast lignite mine Jänschwalde, 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 Jänschwalde (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 Jänschwalde 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. Y1 - 2016 UR - http://meetingorganizer.copernicus.org/EGU2016/EGU2016-5610.pdf N1 - EGU2016-5610 PB - European Geophysical Society CY - Katlenburg-Lindau ER -