中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Decomposition of Organic Carbon in Fine Soil Particles Is Likely More Sensitive to Warming than in Coarse Particles: An Incubation Study with Temperate Grassland and Forest Soils in Northern China

文献类型:期刊论文

作者Ding, Fan1; Huang, Yao; Sun, Wenjuan; Jiang, Guangfu1; Chen, Yue1
刊名PLOS ONE
出版日期2014
卷号9期号:4
ISSN号1932-6203
DOI10.1371/journal.pone.0095348
文献子类Article
英文摘要It is widely recognized that global warming promotes soil organic carbon (SOC) decomposition, and soils thus emit more CO2 into the atmosphere because of the warming; however, the response of SOC decomposition to this warming in different soil textures is unclear. This lack of knowledge limits our projection of SOC turnover and CO2 emission from soils after future warming. To investigate the CO2 emission from soils with different textures, we conducted a 107-day incubation experiment. The soils were sampled from temperate forest and grassland in northern China. The incubation was conducted over three short-term cycles of changing temperature from 5 degrees C to 30 degrees C, with an interval of 5 degrees C. Our results indicated that CO2 emissions from sand (>50 mu m), silt (2-50 mu m), and clay (<2 mu m) particles increased exponentially with increasing temperature. The sand fractions emitted more CO2 (CO2-C per unit fraction-C) than the silt and clay fractions in both forest and grassland soils. The temperature sensitivity of the CO2 emission from soil particles, which is expressed as Q(10), decreased in the order clay>silt>sand. Our study also found that nitrogen availability in the soil facilitated the temperature dependence of SOC decomposition. A further analysis of the incubation data indicated a power-law decrease of Q(10) with increasing temperature. Our results suggested that the decomposition of organic carbon in fine-textured soils that are rich in clay or silt could be more sensitive to warming than those in coarse sandy soils and that SOC might be more vulnerable in boreal and temperate regions than in subtropical and tropical regions under future warming.
学科主题Multidisciplinary Sciences
出版地SAN FRANCISCO
WOS关键词LAND-USE ; MATTER DECOMPOSITION ; MICROBIAL BIOMASS ; SIZE FRACTIONS ; WATER-CONTENT ; RESPIRATION ; CLIMATE ; DEPENDENCE ; STABILIZATION ; TEXTURE
WOS研究方向Science & Technology - Other Topics
语种英语
WOS记录号WOS:000336922600172
出版者PUBLIC LIBRARY SCIENCE
资助机构National Natural Science Foundation of China [41075108] ; Ministry of Science and Technology of China [2010CB950604] ; CAS Strategic Priority Research Program [XDA05050507]
源URL[http://ir.ibcas.ac.cn/handle/2S10CLM1/27354]  
专题植被与环境变化国家重点实验室
作者单位1.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Ding, Fan,Huang, Yao,Sun, Wenjuan,et al. Decomposition of Organic Carbon in Fine Soil Particles Is Likely More Sensitive to Warming than in Coarse Particles: An Incubation Study with Temperate Grassland and Forest Soils in Northern China[J]. PLOS ONE,2014,9(4).
APA Ding, Fan,Huang, Yao,Sun, Wenjuan,Jiang, Guangfu,&Chen, Yue.(2014).Decomposition of Organic Carbon in Fine Soil Particles Is Likely More Sensitive to Warming than in Coarse Particles: An Incubation Study with Temperate Grassland and Forest Soils in Northern China.PLOS ONE,9(4).
MLA Ding, Fan,et al."Decomposition of Organic Carbon in Fine Soil Particles Is Likely More Sensitive to Warming than in Coarse Particles: An Incubation Study with Temperate Grassland and Forest Soils in Northern China".PLOS ONE 9.4(2014).

入库方式: OAI收割

来源:植物研究所

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