中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Profile storage of organic/inorganic carbon in soil: From forest to desert

文献类型:期刊论文

作者Wang ; Yugang ; Li ; Yan ; Ye ; Xuehua ; Chu ; Yu ; Xinping
刊名SCIENCE OF THE TOTAL ENVIRONMENT
出版日期2010
卷号408期号:8页码:1925-1931
关键词ORGANIC-CARBON LAND-USE INORGANIC CARBON CLIMATE-CHANGE CHINA ECOSYSTEMS SEQUESTRATION RESPONSES NITROGEN CYCLE
ISSN号0048-9697
通讯作者Li, Y, Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Key Lab Oasis Ecol & Desert Environm, 818 S Beijing Rd, Urumqi 830011, Xinjiang, Peoples R China
中文摘要Understanding the distribution of organic/inorganic carbon storage in soil profile is crucial for assessing regional, continental and global soil C stores and predicting the consequences of global change. However, little is known about the organic/inorganic carbon storages in deep soil layers at various landscapes. This study was conducted to determine the soil organic/inorganic carbon storage in soil profile of 0-3 m at 5 sites of natural landscape from forest to desert. Landscapes are temperate forest, temperate grassland, temperate shrub-grassland, temperate shrub desert, and temperate desert. Root mass density and carbon contents at the profile were determined for each site. The results showed that considerable decrease in root biomass and soil organic carbon content at the soil profile of 0-3 m when landscape varied from forest to desert along a precipitation gradient, while soil inorganic carbon content increased significantly along the precipitation gradient. Namely, for density of soil organic carbon: forest > grassland > shrub-grassland > shrub desert > desert; for density of soil inorganic carbon: forest, grassland < shrub-grassland < shrub desert < desert (P<0.05 in all cases). In landscapes other than forest, more than 50% soil carbon storage was found in 1-3 m depth. For grassland and shrub-grassland, the contribution from 1-3 m was mainly in the form of organic carbon, while for shrub desert and desert the contribution from this depth was mainly in the form of inorganic carbon. The comparison of soil C storage between top 0-1 m and 1-3 m showed that the using top 1 m of soil profile to estimate soil carbon storages would considerably underestimate soil carbon storage. This is especially true for organic soil carbon at grassland region, and for soil inorganic carbon at desert region. (C) 2010 Elsevier B.V. All rights reserved.
学科主题自然地理学
收录类别SCI
公开日期2011-08-19
源URL[http://ir.xjlas.org/handle/365004/9964]  
专题新疆生态与地理研究所_中国科学院新疆生态与地理研究所(2010年以前数据)
推荐引用方式
GB/T 7714
Wang,Yugang,Li,et al. Profile storage of organic/inorganic carbon in soil: From forest to desert[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2010,408(8):1925-1931.
APA Wang.,Yugang.,Li.,Yan.,Ye.,...&Xinping.(2010).Profile storage of organic/inorganic carbon in soil: From forest to desert.SCIENCE OF THE TOTAL ENVIRONMENT,408(8),1925-1931.
MLA Wang,et al."Profile storage of organic/inorganic carbon in soil: From forest to desert".SCIENCE OF THE TOTAL ENVIRONMENT 408.8(2010):1925-1931.

入库方式: OAI收割

来源:新疆生态与地理研究所

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