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变化中的土壤有机碳
引用本文:JIA Zhongjun,Yakov KUZYAKOV,David MYROLD,James TIEDJE. 变化中的土壤有机碳[J]. 土壤圈, 2017, 27(5): 789-791. DOI: 10.1016/S1002-0160(17)60489-2
作者姓名:JIA Zhongjun  Yakov KUZYAKOV  David MYROLD  James TIEDJE
作者单位:State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008 China,Agro-Technology Institute, RUDN University, Moscow 115419 Russia;Institute of Physicochemical and Biological Problems in Soil Science, RAS, Pushchino 142290 Russia,Department of Crop and Soil Science, Oregon State University, Corvallis OR 97331 USA,Center for Microbial Ecology, Michigan State University, East Lansing MI 48824-1325 USA
摘    要:<正>Soil contains more than three times as much carbon (C) as either the atmosphere or terrestrial vegetation.Soil organic C (SOC) is essentially derived from inputs of plant and animal residues,which are processed by the microbiota (bacteria,archaea,protists,fungi and viruses) that dominates SOC transformation and turnover in complex terrestrial environments.A tiny

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Soil organic carbon in a changing world
JIA Zhongjun,Yakov KUZYAKOV,David MYROLD and James TIEDJE. Soil organic carbon in a changing world[J]. Pedosphere, 2017, 27(5): 789-791. DOI: 10.1016/S1002-0160(17)60489-2
Authors:JIA Zhongjun  Yakov KUZYAKOV  David MYROLD  James TIEDJE
Affiliation:1. State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008 China;2. Agro-Technology Institute, RUDN University, Moscow 115419 Russia;Institute of Physicochemical and Biological Problems in Soil Science, RAS, Pushchino 142290 Russia;3. Department of Crop and Soil Science, Oregon State University, Corvallis OR 97331 USA;4. Center for Microbial Ecology, Michigan State University, East Lansing MI 48824-1325 USA
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