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The Forgotten Nutrient——The Role of Nitrogen in Permafrost Soils of Northern China
作者姓名:Elisabeth RAMM  Chunyan LIU  Xianwei WANG  Hongyu YUE  Wei ZHANG  Yuepeng PAN  Michael SCHLOTER  Silvia GSCHWENDTNER  Carsten W.MUELLER  Bin HU  Heinz RENNENBERG  Michael DANNENMANN
作者单位:1. Institute of Meteorology and Climate Research, Atmospheric Environmental Research(IMK-IFU),Karlsruhe Institute of Technology(KIT);2. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry(LAPC),Institute of Atmospheric Physics, Chinese Academy of Sciences;3. Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences;4. Chair of Soil Science, Science Center Weihenstephan, Department of Ecology and Ecosystem Management,Technical University Munich;6. Department of Geosciences and Natural Resource Management, University of Copenhagen
基金项目:Funding for the project has been provided by the NSFC (Grant No. 41861134029);;DFG (Grant Nos. DA1217/4-1 and SCHL446/41-1);
摘    要:<正>1.Introduction:permafrost carbon and nitrogen feedback to climate change Permafrost refers to any ground, including soils, sediments and rocks, with a temperature at or below the freezing point of water (0℃) for two or more consecutive years (Biskaborn et al., 2019). Permafrost soils of the Northern Hemisphere store vast amounts of both organic carbon (C) and nitrogen (N)(Tarnocai et al., 2009; Harden et al., 2012; Mueller et al.,

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