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    <id>25096</id>
    <completedYear/>
    <publishedYear>2019</publishedYear>
    <thesisYearAccepted/>
    <language>deu</language>
    <pageFirst>S. 502</pageFirst>
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    <completedDate>2020-01-17</completedDate>
    <publishedDate>--</publishedDate>
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    <title language="deu">Aged biochar enriched substrate increases SOM stocks of forest soils in the North German Lowland</title>
    <abstract language="deu">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.</abstract>
    <parentTitle language="deu">Abstract-Band, Jahrestagung der Bodenkundlichen Gesellschaft der Schweizund der Deutschen Bodenkundlichen GesellschaftBern, 24.–29. August 2019</parentTitle>
    <identifier type="url">https://www.dbges.de/de/system/files/Bern2019/Programmheft/abstractband.dbg2019_2.pdf</identifier>
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    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <submitter>
      <firstName>Ulrike</firstName>
      <lastName>Schwarz</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>25082</id>
    <completedYear/>
    <publishedYear>2020</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber>11</pageNumber>
    <edition/>
    <issue/>
    <volume>459</volume>
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    <completedDate>2020-01-16</completedDate>
    <publishedDate>--</publishedDate>
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    <title language="eng">Long term anthropogenic enrichment of soil organic matter stocks in forest soils – detecting a legacy of historical charcoal production</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">Forest Ecology and Management</parentTitle>
    <identifier type="doi">10.1016/j.foreco.2019.117814</identifier>
    <identifier type="issn">0378-1127</identifier>
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    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Sally</firstName>
      <lastName>Donovan</lastName>
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  </doc>
  <doc>
    <id>26320</id>
    <completedYear/>
    <publishedYear>2020</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber>14</pageNumber>
    <edition/>
    <issue/>
    <volume>195</volume>
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    <completedDate>2020-11-12</completedDate>
    <publishedDate>--</publishedDate>
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    <title language="eng">Characteristics of small anthropogenic landforms resulting from historical charcoal production in western Connecticut, USA</title>
    <parentTitle language="eng">Catena</parentTitle>
    <identifier type="doi">10.1016/j.catena.2020.104896</identifier>
    <identifier type="issn">0341-8162</identifier>
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    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
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    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
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    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>William</firstName>
      <lastName>Ouimet</lastName>
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  </doc>
  <doc>
    <id>26322</id>
    <completedYear/>
    <publishedYear>2020</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber>15</pageNumber>
    <edition/>
    <issue/>
    <volume>366</volume>
    <type>articler</type>
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    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2020-11-12</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">The soil moisture regime of charcoal-enriched land use legacy sites</title>
    <parentTitle language="eng">Geoderma</parentTitle>
    <identifier type="doi">10.1016/j.geoderma.2020.114241</identifier>
    <identifier type="issn">0016-7061</identifier>
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    <enrichment key="Artikelnummer">114241</enrichment>
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    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
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    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
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      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
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    <id>26323</id>
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    <publishedYear>2020</publishedYear>
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    <language>eng</language>
    <pageFirst>545</pageFirst>
    <pageLast>561</pageLast>
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    <issue>4</issue>
    <volume>35</volume>
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    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2020-11-12</completedDate>
    <publishedDate>--</publishedDate>
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    <title language="eng">Large‐scale mapping of anthropogenic relief features—legacies of past forest use in two historical charcoal production areas in Germany</title>
    <parentTitle language="eng">Geoarchaeology</parentTitle>
    <identifier type="doi">10.1002/gea.21782</identifier>
    <identifier type="issn">1520-6548</identifier>
    <identifier type="issn">0883-6353</identifier>
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    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
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  </doc>
  <doc>
    <id>26326</id>
    <completedYear/>
    <publishedYear>2020</publishedYear>
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    <language>eng</language>
    <pageFirst>974</pageFirst>
    <pageLast>983</pageLast>
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    <issue>6</issue>
    <volume>35</volume>
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    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2020-11-12</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">An initiative for a morphologic‐genetic catalog of relict charcoal hearths from Central Europe</title>
    <parentTitle language="eng">Geoarchaeology</parentTitle>
    <identifier type="doi">10.1002/gea.21799</identifier>
    <identifier type="issn">1520-6548</identifier>
    <identifier type="issn">0883-6353</identifier>
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    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
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    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Patrick J.</firstName>
      <lastName>Drohan</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>26330</id>
    <completedYear/>
    <publishedYear>2020</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>29</pageFirst>
    <pageLast/>
    <pageNumber/>
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    <publisherName/>
    <publisherPlace>Cottbus</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation>BTU Cottbus-Senftenberg</contributingCorporation>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2020-11-12</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Stratigraphy and shape of relict charcoal hearths in Connecticut, USA</title>
    <parentTitle language="eng">Anthropogenetische Geomorphologie - Geomorophologie im Anthropozän : Virtuelle Jahrestagung des Arbeitskreises für Geomorphologie 2020, 28./29. September 2020, BTU Cottbus - Senftenberg</parentTitle>
    <identifier type="doi">10.26127/BTUOpen-5363</identifier>
    <identifier type="issn">2196-4122</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="UBICOseries">Geopedology and Landscape Development Research Series ; 9</enrichment>
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    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
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    <author>
      <firstName>William</firstName>
      <lastName>Ouimet</lastName>
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    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Anthropogenetische Geomorphologie; Anthropozän; BTU; Geopedologie Anthropocene; Anthropogenic geomorphology; Geopedology</value>
    </subject>
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    <id>26533</id>
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    <publishedYear>2020</publishedYear>
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    <completedDate>2020-12-15</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Fingerprints from past charcoal burning - lessons learned and future perspective studying Relict Charcoal Hearths (RCH)</title>
    <parentTitle language="eng">EGU General Assembly 2020, Online | 4–8 May 2020</parentTitle>
    <identifier type="doi">https://doi.org/10.5194/egusphere-egu2020-2949</identifier>
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    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
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  </doc>
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    <id>26534</id>
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    <publishedYear>2020</publishedYear>
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    <completedDate>2020-12-15</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">The temperature and moisture regime of charcoal-enriched land use legacy soils</title>
    <parentTitle language="eng">EGU General Assembly 2020</parentTitle>
    <identifier type="doi">https://doi.org/10.5194/egusphere-egu2020-2339</identifier>
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    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
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    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
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    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
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    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
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    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
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    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
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    <publishedYear>2020</publishedYear>
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    <language>deu</language>
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    <completedDate>2021-01-18</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="deu">Relikte historischer Kohlenmeier ini der Oberpfalz - Verbreitung und Erhaltung in Abhängigkeit vom Naturraum</title>
    <parentTitle language="deu">Beiträge zur Archäologie in der Oberpfalz und in Regensburg</parentTitle>
    <identifier type="issn">1617-4461</identifier>
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    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
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    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
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    <author>
      <firstName>Florian</firstName>
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      <firstName>Alexandra</firstName>
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    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>27412</id>
    <completedYear/>
    <publishedYear>2021</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject_ref</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2021-05-06</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Accumulation patterns of soil organic matter in forests as a legacy of historical charcoal burning</title>
    <parentTitle language="eng">EGU General Assembly 2021</parentTitle>
    <identifier type="doi">10.5194/egusphere-egu21-5161</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="Artikelnummer">EGU21-5161</enrichment>
    <enrichment key="opus.doi.autoCreate">false</enrichment>
    <enrichment key="opus.urn.autoCreate">false</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>28097</id>
    <completedYear/>
    <publishedYear>2022</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume>504</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2021-12-09</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Hot spots and hot zones of soil organic matter in forests as a legacy of historical charcoal production</title>
    <abstract language="eng">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 (&lt; 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.</abstract>
    <parentTitle language="eng">Forest Ecology and Management</parentTitle>
    <identifier type="issn">1872-7042</identifier>
    <identifier type="doi">10.1016/j.foreco.2021.119846</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="Artikelnummer">119846</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="opus.doi.autoCreate">false</enrichment>
    <enrichment key="opus.urn.autoCreate">false</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Anthropogenic soils</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>relict charcoal hearths</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>soil organic matter</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>pyrogenic carbon</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>GIS</value>
    </subject>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>28312</id>
    <completedYear/>
    <publishedYear>2021</publishedYear>
    <thesisYearAccepted/>
    <language>deu</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber>68</pageNumber>
    <edition/>
    <issue/>
    <volume/>
    <type>book</type>
    <publisherName>Brandenburgische Technische Universität Cottbus - Senftenberg, Fachgebiet Geopedologie und Landschaftsentwicklung</publisherName>
    <publisherPlace>Cottbus</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2022-01-03</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="deu">Historische Köhlerei in Südbrandenburg - Begleitband zum Köhlerpfad Waldschule Kleinsee</title>
    <identifier type="issn">2196-4122</identifier>
    <identifier type="urn">urn:nbn:de:kobv:co1-opus4-54883</identifier>
    <identifier type="doi">10.26127/BTUOpen-5488</identifier>
    <enrichment key="UBICOseries">Geopedology and Landscape Development Research Series  ; 11</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <editor>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </editor>
    <submitter>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </submitter>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Markus</firstName>
      <lastName>Aghte</lastName>
    </author>
    <author>
      <firstName>Alf</firstName>
      <lastName>Pommerenke</lastName>
    </author>
    <subject>
      <language>deu</language>
      <type>uncontrolled</type>
      <value>Archäologie</value>
    </subject>
    <subject>
      <language>deu</language>
      <type>uncontrolled</type>
      <value>Holzkohlemeiler</value>
    </subject>
    <subject>
      <language>deu</language>
      <type>uncontrolled</type>
      <value>Lausitz</value>
    </subject>
    <subject>
      <language>deu</language>
      <type>uncontrolled</type>
      <value>Tauerscher Forst</value>
    </subject>
    <subject>
      <language>deu</language>
      <type>uncontrolled</type>
      <value>Umweltwissenschaften</value>
    </subject>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>28738</id>
    <completedYear/>
    <publishedYear>2022</publishedYear>
    <thesisYearAccepted/>
    <language>deu</language>
    <pageFirst>71</pageFirst>
    <pageLast>77</pageLast>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>bookpart</type>
    <publisherName>Springer Spektrum</publisherName>
    <publisherPlace>Berlin, Heidelberg</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2022-04-05</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="deu">Geoökologische Folgen historischer Landnutzung</title>
    <abstract language="deu">Seit dem Neolithikum wirkt sich die Nutzung der Landschaft auf unterschiedliche Weise auf Relief, Böden, Gewässer, Flora, Fauna und Klima aus. Insbesondere die Folgen land- und forstwirtschaftlicher Wirtschaftsweisen waren dafür ausschlaggebend. Grundsätzlich reagieren Ökosysteme auf anthropogene Eingriffe, wie die Umwandlung von Wald in andere Nutzungsformen, mit einer schrittweisen Degradation sowie reversiblen oder irreversiblen Veränderungen. Beispiele sind Bodenerosion und eine veränderte Artenzusammensetzung. Die Abschätzung des Ausmaßes im globalen Maßstab gestaltet sich generell schwierig. Für die Geoarchäologie bedeutsam sind daher hauptsächlich lokale Spuren früherer Bewirtschaftung und Formen im Kleinrelief, die sich im Gelände wiederfinden lassen und als Geoarchive fungieren. Denn sie geben Aufschluss über (prä-)historische Bewirtschaftungsformen. So zeugen Wölbäcker, Hochbeete, Plaggenesche und die Relikte der historischen Teichwirtschaft, Moorkultivierung und Köhlerei von früheren Formen der Land- und Forstwirtschaft.</abstract>
    <parentTitle language="deu">Geoarchäologie</parentTitle>
    <identifier type="doi">10.1007/978-3-662-62774-7_8</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="opus.doi.autoCreate">false</enrichment>
    <enrichment key="opus.urn.autoCreate">false</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <editor>
      <firstName>Christian</firstName>
      <lastName>Stolz</lastName>
    </editor>
    <submitter>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <editor>
      <firstName>Christopher E.</firstName>
      <lastName>Miller</lastName>
    </editor>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>28958</id>
    <completedYear/>
    <publishedYear>2022</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber>16</pageNumber>
    <edition/>
    <issue/>
    <volume>413</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2022-06-14</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Do small landforms have large effects? A review on the legacies of pre-industrial charcoal burning</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">Geomorphology</parentTitle>
    <identifier type="doi">10.1016/j.geomorph.2022.108332</identifier>
    <identifier type="issn">0169-555X</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="Artikelnummer">108332</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="opus.doi.autoCreate">false</enrichment>
    <enrichment key="opus.urn.autoCreate">false</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </submitter>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Klaus</firstName>
      <lastName>Birkhofer</lastName>
    </author>
    <author>
      <firstName>Patrick J.</firstName>
      <lastName>Drohan</lastName>
    </author>
    <author>
      <firstName>Martin</firstName>
      <lastName>Wilmking</lastName>
    </author>
    <author>
      <firstName>Jürgen</firstName>
      <lastName>Kreyling</lastName>
    </author>
    <author>
      <firstName>Ireneusz</firstName>
      <lastName>Malik</lastName>
    </author>
    <author>
      <firstName>Małgorzata</firstName>
      <lastName>Wistuba</lastName>
    </author>
    <author>
      <firstName>Ernst van der</firstName>
      <lastName>Maaten</lastName>
    </author>
    <author>
      <firstName>Marieke van der</firstName>
      <lastName>Maaten-Theunissen</lastName>
    </author>
    <author>
      <firstName>Tim</firstName>
      <lastName>Urich</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Soil</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Ecosystem</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Forestry</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Land Use</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Anthropocene</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Relict Charcoal Hearth (RCH)</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>Charcoal Kiln Remain (CKR)</value>
    </subject>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2407">FG Ökologie</collection>
  </doc>
  <doc>
    <id>29223</id>
    <completedYear/>
    <publishedYear>2022</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>1</pageFirst>
    <pageLast>16</pageLast>
    <pageNumber/>
    <edition/>
    <issue>4</issue>
    <volume>73</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2022-08-15</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Vertical SOC distribution and aromatic carbon in centuries old charcoal-rich Technosols</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">European Journal of Soil Science</parentTitle>
    <identifier type="url">https://bsssjournals.onlinelibrary.wiley.com/doi/10.1111/ejss.13293</identifier>
    <identifier type="doi">10.1111/ejss.13293</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="Artikelnummer">e13293</enrichment>
    <enrichment key="opus.source">publish</enrichment>
    <enrichment key="Fprofil">2 Gesundheit und Lifes Sciences / Health and Life Sciences</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <submitter>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </submitter>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Fischer</lastName>
    </author>
    <author>
      <firstName>Shaghayegh</firstName>
      <lastName>Ramezany</lastName>
    </author>
    <author>
      <firstName>William</firstName>
      <lastName>Ouimet</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2051">Zentrale Analytik der BTU Cottbus-Senftenberg (ZA-BTU) / Zentrales Analytisches Labor</collection>
  </doc>
  <doc>
    <id>31417</id>
    <completedYear/>
    <publishedYear>2023</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>417</pageFirst>
    <pageLast>427</pageLast>
    <pageNumber>11</pageNumber>
    <edition/>
    <issue>4</issue>
    <volume>186</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2023-08-02</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Soil properties and tree growth at medieval ridge and furrow sites in Brandenburg, northeastern Germany</title>
    <abstract language="eng">Background&#13;
&#13;
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.&#13;
Aims&#13;
&#13;
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.&#13;
Methods&#13;
&#13;
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.&#13;
Results&#13;
&#13;
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.&#13;
Conclusions&#13;
&#13;
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.</abstract>
    <parentTitle language="eng">Journal of Plant Nutrition and Soil Science</parentTitle>
    <identifier type="issn">1436-8730</identifier>
    <identifier type="issn">1522-2624</identifier>
    <identifier type="doi">10.1002/jpln.202200345</identifier>
    <enrichment key="opus.import.date">2023-10-10T17:24:26+00:00</enrichment>
    <enrichment key="opus.source">sword</enrichment>
    <enrichment key="opus.import.user">deepgreen</enrichment>
    <enrichment key="opus.import.file">attachment; filename=deposit.zip</enrichment>
    <enrichment key="opus.import.checksum">4976dcd127b24bb2d2e6311566a24a32</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="Publikationsweg">Open Access</enrichment>
    <enrichment key="Fprofil">3 Globaler Wandel und Transformationsprozesse / Global Change and Transformation Processes</enrichment>
    <enrichment key="Fprofil">4 Künstliche Intelligenz und Sensorik / Artificial Intelligence and Sensor Technology</enrichment>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Marieke van der</firstName>
      <lastName>Maaten-Theunissen</lastName>
    </author>
    <author>
      <firstName>Ernst van der</firstName>
      <lastName>Maaten</lastName>
    </author>
    <author>
      <firstName>Christin</firstName>
      <lastName>Räbiger</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>anthropogenically modified soils</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>climate sensitivity</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>dendroecology</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>historic agriculture</value>
    </subject>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>land‐use legacies</value>
    </subject>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
    <collection role="Import" number="import">Import</collection>
  </doc>
  <doc>
    <id>14066</id>
    <completedYear/>
    <publishedYear>2015</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2015-04-13</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Towards an inventory of historic charcoal production fields in Brandenburg, Germany</title>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015</parentTitle>
    <identifier type="url">http://meetingorganizer.copernicus.org/EGU2015/EGU2015-3949.pdf</identifier>
    <note>EGU2015-3949</note>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 17</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Petra</firstName>
      <lastName>Klammer</lastName>
    </submitter>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Horst</firstName>
      <lastName>Rösler</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>historic charcoal production</value>
    </subject>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="old_institute" number="04033">LS Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>20238</id>
    <completedYear/>
    <publishedYear>2019</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>153</pageFirst>
    <pageLast>165</pageLast>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume>Vol. 511</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2017-08-28</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Spatial distribution of relict charcoal hearths in the former royal forest district Tauer (SE Brandenburg, Germany)</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">Quaternary International</parentTitle>
    <identifier type="doi">10.1016/j.quaint.2017.07.022</identifier>
    <identifier type="issn">1040-6182</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Werner</firstName>
      <lastName>Gerwin</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Horst</firstName>
      <lastName>Rösler</lastName>
    </author>
    <author>
      <firstName>Karl-Uwe</firstName>
      <lastName>Heußner</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>18926</id>
    <completedYear/>
    <publishedYear>2017</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>297</pageFirst>
    <pageLast>310</pageLast>
    <pageNumber/>
    <edition/>
    <issue>4</issue>
    <volume>24</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2017-03-02</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Reconstruction of a Paleosurface and Archaeological Site Location in an Anthropogenic Drift Sand Area</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">Archaeological Prospection</parentTitle>
    <identifier type="doi">10.1002/arp.1571</identifier>
    <identifier type="issn">1099-0763</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Werner</firstName>
      <lastName>Gerwin</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Klaus-Peter</firstName>
      <lastName>Wechler</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>21797</id>
    <completedYear/>
    <publishedYear>2018</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2018-04-17</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Spatial and temporal variability of soil physical properties on legacies of historic charcoal production</title>
    <abstract language="deu">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&#13;
&#13;
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.</abstract>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2018, Vienna, Austria</parentTitle>
    <identifier type="url">https://meetingorganizer.copernicus.org/EGU2018/EGU2018-10115.pdf</identifier>
    <note>EGU2018-10115</note>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 20</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <submitter>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>16024</id>
    <completedYear/>
    <publishedYear>2016</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2016-04-30</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Spatial analysis of charcoal kiln remains in the former royal forest district Tauer (Lower Lusatia, North German Lowlands)</title>
    <abstract language="eng">Archaeological excavations have revealed more than thousand charcoal kiln remains (CKRs) in the prefield of&#13;
the active opencast lignite mine Jänschwalde, situated about 150 km SE of Berlin (SE Brandenburg, Germany).&#13;
The charcoal was mainly produced for the ironwork Peitz nearby, which operated from the 16th to the mid-19th&#13;
centuries. In a first approach, to estimate the dimension of the charcoal production, CKRs were mapped on&#13;
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&#13;
field. This survey showed a considerably number of falsely detected sites. Therefore, the data was critically&#13;
re-evaluated using additional relief visualisations. Further, we extended the CKR mapping to areas which are not&#13;
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.</abstract>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2016, Vienna, Austria</parentTitle>
    <identifier type="url">http://meetingorganizer.copernicus.org/EGU2016/EGU2016-5610.pdf</identifier>
    <note>EGU2016-5610</note>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 18</enrichment>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </submitter>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Frank</firstName>
      <lastName>Müller</lastName>
    </author>
    <author>
      <firstName>Horst</firstName>
      <lastName>Rösler</lastName>
    </author>
    <author>
      <firstName>Karl-Uwe</firstName>
      <lastName>Heußner</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>17985</id>
    <completedYear/>
    <publishedYear>2016</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>S. 152</pageFirst>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>Department of archaeology and ancient history, Uppsala university,</publisherName>
    <publisherPlace>Uppsala</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation>Deutsches Archäologisches Institut, Berlin</contributingCorporation>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2017-01-23</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Reconstructing anthropogenic landscape transformation in the surroundings of the ironwork Peitz (SE Brandenburg, Germany) - 16th to mid-19th centuries</title>
    <abstract language="eng">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.</abstract>
    <parentTitle language="eng">4th International Landscape Archaeology Conference, Uppsala, 22nd - 25th August 2016</parentTitle>
    <identifier type="url">http://www.arkeologi.uu.se/digitalAssets/447/c_447246-l_1-k_20160816_lac_booklet.pdf</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </submitter>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Nicolay</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Frank</firstName>
      <lastName>Müller</lastName>
    </author>
    <author>
      <firstName>Karl-Uwe</firstName>
      <lastName>Heußner</lastName>
    </author>
    <author>
      <firstName>Horst</firstName>
      <lastName>Rösler</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>14068</id>
    <completedYear/>
    <publishedYear>2015</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2015-04-13</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Late Quaternary landscape development at the margin of the Pomeranian phase (MIS 2) near Lake Wygonin (Northern Poland)</title>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015</parentTitle>
    <identifier type="url">http://meetingorganizer.copernicus.org/EGU2015/EGU2015-3547-1.pdf</identifier>
    <note>EGU2015-3547-1</note>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 17</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <submitter>
      <firstName>Petra</firstName>
      <lastName>Klammer</lastName>
    </submitter>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Nicolay</lastName>
    </author>
    <author>
      <firstName>Mirosław</firstName>
      <lastName>Błaszkiewicz</lastName>
    </author>
    <author>
      <firstName>Jarosław</firstName>
      <lastName>Kordowski</lastName>
    </author>
    <author>
      <firstName>Agnieszka M.</firstName>
      <lastName>Noryskiewicz</lastName>
    </author>
    <author>
      <firstName>Sebastian</firstName>
      <lastName>Tyszkowski</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>late quaternary landscape development</value>
    </subject>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="old_institute" number="04033">LS Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>14062</id>
    <completedYear/>
    <publishedYear>2015</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2015-04-13</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Effects of historic charcoal burning on soil properties</title>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April - 17 May 2015</parentTitle>
    <identifier type="url">http://meetingorganizer.copernicus.org/EGU2015/EGU2015-3574-2.pdf</identifier>
    <note>EGU2015-3574-2</note>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 17</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <submitter>
      <firstName>Petra</firstName>
      <lastName>Klammer</lastName>
    </submitter>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Allan</firstName>
      <lastName>Buras</lastName>
    </author>
    <author>
      <firstName>Ernst van der</firstName>
      <lastName>Maaten</lastName>
    </author>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Christin</firstName>
      <lastName>Räbiger</lastName>
    </author>
    <author>
      <firstName>Roberto</firstName>
      <lastName>Cruz-García</lastName>
    </author>
    <author>
      <firstName>Martin</firstName>
      <lastName>Wilmking</lastName>
    </author>
    <subject>
      <language>eng</language>
      <type>uncontrolled</type>
      <value>historic charcoal burning</value>
    </subject>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="old_institute" number="04033">LS Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>14057</id>
    <completedYear/>
    <publishedYear>2015</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2015-04-13</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Charcoal kiln relicts - a favorable site for tree growth?</title>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2015, Vienna, Austria, 13 April – 17 May 2015</parentTitle>
    <note>EGU2015-3257</note>
    <enrichment key="UBICOseries">Geophysical Abstracts ; 17</enrichment>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Allan</firstName>
      <lastName>Buras</lastName>
    </author>
    <submitter>
      <firstName>Werner</firstName>
      <lastName>Gerwin</lastName>
    </submitter>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Ernst van der</firstName>
      <lastName>Maaten</lastName>
    </author>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Christin</firstName>
      <lastName>Räbiger</lastName>
    </author>
    <author>
      <firstName>Roberto</firstName>
      <lastName>Cruz-García</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Martin</firstName>
      <lastName>Wilmking</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="old_institute" number="04033">LS Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>10684</id>
    <completedYear/>
    <publishedYear>2014</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst/>
    <pageLast/>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume/>
    <type>conferenceobject</type>
    <publisherName>European Geophysical Society</publisherName>
    <publisherPlace>Katlenburg-Lindau</publisherPlace>
    <creatingCorporation/>
    <contributingCorporation>Brandenburgisches Landesamt für Denkmalpflege und Archäologisches Landesmuseum</contributingCorporation>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2014-05-08</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">Human-induced landscape dynamics in South Brandenburg - findings from different geoarchives</title>
    <abstract language="eng">South Brandenburg is the central part of the North European Lowland (NEL) extending as a plain landscape from&#13;
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&#13;
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&#13;
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.</abstract>
    <parentTitle language="eng">European Geosciences Union, General Assembly 2014, Vienna, Austria, 27 April – 02 May 2014</parentTitle>
    <identifier type="url">http://meetingorganizer.copernicus.org/EGU2014/EGU2014-1852-1.pdf</identifier>
    <note>EGU2014-1852-1</note>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <enrichment key="UBICOseries">Geophysical Research Abstracts ; 16</enrichment>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <submitter>
      <firstName>Werner</firstName>
      <lastName>Gerwin</lastName>
    </submitter>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Nicolay</lastName>
    </author>
    <author>
      <firstName>Melanie</firstName>
      <lastName>Takla</lastName>
    </author>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Horst</firstName>
      <lastName>Rösler</lastName>
    </author>
    <author>
      <firstName>Eberhard</firstName>
      <lastName>Bönisch</lastName>
    </author>
    <collection role="institutes" number="2052">Zentrum für Landschaftstransformation (ZLT)</collection>
    <collection role="old_institute" number="04033">LS Geopedologie und Landschaftsentwicklung</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
  <doc>
    <id>22891</id>
    <completedYear/>
    <publishedYear>2019</publishedYear>
    <thesisYearAccepted/>
    <language>eng</language>
    <pageFirst>77</pageFirst>
    <pageLast>92</pageLast>
    <pageNumber/>
    <edition/>
    <issue/>
    <volume>175</volume>
    <type>articler</type>
    <publisherName/>
    <publisherPlace/>
    <creatingCorporation/>
    <contributingCorporation/>
    <belongsToBibliography>0</belongsToBibliography>
    <completedDate>2018-12-13</completedDate>
    <publishedDate>--</publishedDate>
    <thesisDateAccepted>--</thesisDateAccepted>
    <title language="eng">The occurrence, soil parameters and genesis of rubified soils (‘Fuchserden’) of northeastern Germany</title>
    <parentTitle language="eng">Catena</parentTitle>
    <identifier type="doi">10.1016/j.catena.2018.11.039</identifier>
    <identifier type="issn">0008-7769</identifier>
    <identifier type="issn">1872-6887</identifier>
    <enrichment key="BTU">an der BTU erstellt / created at BTU</enrichment>
    <author>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </author>
    <submitter>
      <firstName>Florian</firstName>
      <lastName>Hirsch</lastName>
    </submitter>
    <author>
      <firstName>Alexander</firstName>
      <lastName>Bonhage</lastName>
    </author>
    <author>
      <firstName>Albrecht</firstName>
      <lastName>Bauriegel</lastName>
    </author>
    <author>
      <firstName>Anna</firstName>
      <lastName>Schneider</lastName>
    </author>
    <author>
      <firstName>Thomas</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Alexandra</firstName>
      <lastName>Raab</lastName>
    </author>
    <author>
      <firstName>Stella</firstName>
      <lastName>Gypser</lastName>
    </author>
    <collection role="institutes" number="2402H01">FG Bodenschutz und Rekultivierung (ehemals)</collection>
    <collection role="institutes" number="2404">FG Geopedologie und Landschaftsentwicklung</collection>
  </doc>
</export-example>
