中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Effects of soil erosion and deposition on soil organic carbon dynamics at a sloping field in black soil region, northeast china

文献类型:期刊论文

作者Cheng, Shulan2; Fang, Huajun1; Zhu, Tianhong2; Zheng, Jiaojiao2; Yang, Xueming3; Zhang, Xiaoping4; Yu, Guirui1
刊名Soil science and plant nutrition
出版日期2010-08-01
卷号56期号:4页码:521-529
关键词13c natural abundance Black soils Physical separation Soil organic carbon Soil redistribution
ISSN号0038-0768
DOI10.1111/j.1747-0765.2010.00492.x
通讯作者Fang, huajun(huajunfang@yahoo.com.cn)
英文摘要Soil erosion transports light density and fine particle soil material from hills down to low-lying land areas, which can lead to carbon loss and subsequent sequestration. in the present paper, the profile distribution of soil organic carbon (soc) and soil 13c natural abundance (delta 13c) were analyzed across five geomorphic positions, distributed along a typical rolling farmland in the black soil region of northeast china. the contents of particulate organic carbon (poc) and mineral-associated organic carbon (moc) at each geomorphic position were measured with physical fraction method. the results showed that soil erosion decreased 5.3-22.4% of soc and increased 4.0-6.1% of delta 13c of surface soils at the eroding sites. at the typical depositional sites, soc content and delta 13c value in the buried surface layer were 1.5 times and 1.1 times as much as those of the current plough layer, respectively. soil erosion did not change the poc content, but moc content decreased by 9.3-35.2%. at the eroding sites, the coefficient of determination between soil delta 13c and moc (r2 = 0.52) was higher than that between soil delta 13c and poc (r2 = 0.37). our study indicated that soil erosion decreased soc content and increased delta 13c(soc) in surface layer mainly through transferring fine sized and 13c-depleted soc fraction. deep burial and re-aggregation of eroded materials at depositional sites were in favor of stabilization and sequestration of soc.
WOS关键词MATTER DYNAMICS ; WATER EROSION ; SEQUESTRATION ; CULTIVATION ; TILLAGE ; IMPACT ; FRACTIONS ; AGGREGATE ; ABUNDANCE ; TURNOVER
WOS研究方向Plant Sciences ; Environmental Sciences & Ecology ; Agriculture
WOS类目Plant Sciences ; Environmental Sciences ; Soil Science
语种英语
WOS记录号WOS:000281638300002
出版者WILEY-BLACKWELL
URI标识http://www.irgrid.ac.cn/handle/1471x/2407860
专题中国科学院大学
通讯作者Fang, Huajun
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
3.Agr & Agri Food Canada, Greenhouse & Proc Crops Res Ctr, Harrow, ON N0R 1G0, Canada
4.Chinese Acad Sci, NE Inst Geog & Agr Ecol, Changchun 130012, Peoples R China
推荐引用方式
GB/T 7714
Cheng, Shulan,Fang, Huajun,Zhu, Tianhong,et al. Effects of soil erosion and deposition on soil organic carbon dynamics at a sloping field in black soil region, northeast china[J]. Soil science and plant nutrition,2010,56(4):521-529.
APA Cheng, Shulan.,Fang, Huajun.,Zhu, Tianhong.,Zheng, Jiaojiao.,Yang, Xueming.,...&Yu, Guirui.(2010).Effects of soil erosion and deposition on soil organic carbon dynamics at a sloping field in black soil region, northeast china.Soil science and plant nutrition,56(4),521-529.
MLA Cheng, Shulan,et al."Effects of soil erosion and deposition on soil organic carbon dynamics at a sloping field in black soil region, northeast china".Soil science and plant nutrition 56.4(2010):521-529.

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