Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Patrick Wordell-Dietrich"'
Autor:
Sebastian Preusser, Georg Guggenberger, Robert Mikutta, Ole Mewes, Patrick Liebmann, Timo Leinemann, Bernd Marschner, Patrick Wordell-Dietrich, Axel Don, Ellen Kandeler, Eike Perrin, Jörg Bachmann, Karsten Kalbitz, Frank Schaarschmidt
Publikováno v:
Journal of Plant Nutrition and Soil Science. 185:35-43
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34c3a92286d515788d27a836b074c763
https://doi.org/10.1002/jpln.202100295
https://doi.org/10.1002/jpln.202100295
Autor:
Robert Mikutta, Bernd Marschner, Timo Leinemann, Georg Guggenberger, Frank Schaarschmidt, Patrick Liebmann, Ellen Kandeler, Jörg Bachmann, Sebastian Preusser, Karsten Kalbitz, Patrick Wordell-Dietrich, Axel Don
Formation of mineral-associated organic matter (MAOM) is a decisive process in the stabilization of OM against rapid microbial decomposition and thus in the soils’ role as global carbon (C) sink. Sorption experiments of dissolved OM (DOM) repeatedl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2902fcf633cf3f0fc3ec1a8a194f7ce2
https://doi.org/10.5194/egusphere-egu21-14580
https://doi.org/10.5194/egusphere-egu21-14580
Autor:
Sebastian Preußer, Ellen Kandeler, Patrick Liebmann, Patrick Wordell-Dietrich, Axel Don, Karsten Kalbitz, Chiara Cerli, Fabian Kalks, Robert Mikutta, Georg Guggenberger, Timo Leinemann
Dissolved organic matter (DOM) can be a major source of organic carbon (OC) stocks in mineral soils of high-leaching forest ecosystems due to its high affinity towards reactive mineral phases, thus forming mineral-associated organic matter (MAOM). Ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bbcd5c56c6431383d549ec929e9df89
https://doi.org/10.5194/egusphere-egu2020-19907
https://doi.org/10.5194/egusphere-egu2020-19907
Autor:
Georg Guggenberger, Patrick Wordell-Dietrich, Axel Don, Sebastian Preusser, Bernd Marschner, Robert Mikutta, Stefanie Heinze, Mirjam Helfrich, Dietrich Hertel, Timo Leinemann, Kristina Kirfel, Hans-Peter Piepho, Bernard Ludwig, Christoph Leuschner, Ellen Kandeler
Publikováno v:
Geoderma. 311:37-44
Organic carbon in subsoils amounts to 40–60% of the global soil carbon pool and is generally characterized by apparent turnover times of hundreds to thousands of years and an increasing spatial variability with depth. The objective of this study wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4c82fc0662155ef024277321f968f497
https://doi.org/10.1016/j.geoderma.2017.09.028
https://doi.org/10.1016/j.geoderma.2017.09.028
Publikováno v:
Geoderma. 304:40-48
Subsoils store > 50 % of the total global soil organic carbon (SOC), and low SOC content and high mean residence times indicate that subsoils have the potential to sequester additional C on the long-term. Nevertheless, the mechanisms controlling the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::82e848a74a8690adeae41213004c01cc
https://doi.org/10.1016/j.geoderma.2016.08.023
https://doi.org/10.1016/j.geoderma.2016.08.023
Publikováno v:
Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms. 400:65-73
Radiocarbon (14C) analysis on CO2 can provide valuable information on the carbon cycle as different carbon pools differ in their 14C signature. While fresh, biogenic carbon shows atmospheric 14C concentrations, fossil carbon is 14C free. As shown in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::219257fa1f6b6d6f4f7d15f71a078e20
https://doi.org/10.1016/j.nimb.2017.04.019
https://doi.org/10.1016/j.nimb.2017.04.019
Autor:
Patrick Liebmann, Patrick Wordell-Dietrich, Karsten Kalbitz, Robert Mikutta, Fabian Kalks, Axel Don, Susanne K. Woche, Leena R. Dsilva, Georg Guggenberger
Publikováno v:
Biogeosciences, Vol 17, Pp 3099-3113 (2020)
Biogeosciences 17 (2020)
Biogeosciences 17 (2020)
In contrast to mineral topsoils, in subsoils the origin and processes leading to the formation and stabilization of organic matter (OM) are still not well known. This study addresses the fate of litter-derived carbon (C) in whole soil profiles with r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fb38712b70c882f32cee2ace05f074e0
https://doi.org/10.5194/bg-2019-465
https://doi.org/10.5194/bg-2019-465
Autor:
Patrick Liebmann, Patrick Wordell-Dietrich, Karsten Kalbitz, Robert Mikutta, Fabian Kalks, Axel Don, Susanne K. Woche, Leena R. Dsilva, Georg Guggenberger
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83f50eee09e449e0d072e464a2bdf0c8
https://doi.org/10.5194/bg-2019-465-supplement
https://doi.org/10.5194/bg-2019-465-supplement