Soil profile description from the research site Grinderwald, part of the research unit SubSOM
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We conducted a litter manipulation experiment with 13C enriched beech litter at the Grinderwald research site, 40 km north of Hannover, Germany. The study site contains a more than 100 years old beech forest on a Dystric Cambisol. At 2 time points (11.2016, 05.2018), we took soil cores down to 180 cm soil depth and divided them in 15 depth increments. These data serve as a basis for interpretation of the field experiments conducted at this site. Data were adapted from Leinemann et al. 2016. Research domain: Soil Sciences Research question: We studied the contribution of litter-derived carbon (C) in the formation of subsoil organic matter (OM). Literature: Leinemann, T., Mikutta, R., Kalbitz, K. et al. Small scale variability of vertical water and dissolved organic matter fluxes in sandy Cambisol subsoils as revealed by segmented suction plates. Biogeochemistry 131, 1–15 (2016). https://doi.org/10.1007/s10533-016-0259-8
本研究于德国汉诺威以北40公里的格林德瓦尔德(Grinderwald)研究样地,开展了一项采用13C富集山毛榉凋落物的凋落物操控实验。该研究样地位于不饱和雏形土(Dystric Cambisol)之上,发育有一片树龄逾百年的山毛榉林。分别于2个时间节点(2016年11月、2018年5月)采集深度达180 cm的土壤岩芯,并按15个深度梯度对岩芯进行分层。本数据集为该样地开展的野外实验解译提供了基础依据,数据改编自Leinemann等人2016年的研究成果。
研究领域:土壤科学
研究问题:本研究旨在探究凋落物来源碳(Carbon,简称C)在亚表层土壤有机质(Organic Matter,简称OM)形成过程中的贡献。
参考文献:Leinemann, T., Mikutta, R., Kalbitz, K. 等. 分段吸力板法揭示的砂质雏形土亚表层垂直水分与溶解性有机质通量的微尺度变异. 生物地球化学, 131, 1–15 (2016). https://doi.org/10.1007/s10533-016-0259-8
提供机构:
BonaRes Data Centre (ZALF)
创建时间:
2020-06-05



