中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Lateral transport of soil carbon and land-atmosphere CO2 flux induced by water erosion in China

文献类型:期刊论文

作者Borthwick, AGL (Borthwick, Alistair G. L.)4; Li, TH (Li, Tianhong)5; Wang, YC (Wang, Yichu)5; Chappell, A (Chappell, Adrian)3; Van Oost, K (Van Oost, Kristof)2; Ni, JR; Yue, Y (Yue, Yao)5,6; Ni, JR (Ni, Jinren)5; Ciais, P (Ciais, Philippe)7; Piao, SL (Piao, Shilong)1,8,9
刊名PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
出版日期2016
卷号113期号:24页码:6617-6622
关键词Dissolved Organic-carbon Terrestrial Ecosystems Deposition Storage Impact Basin Sequestration Landscapes Croplands Sediment
DOI10.1073/pnas.1523358113
文献子类Article
英文摘要Soil erosion by water impacts soil organic carbon stocks and alters CO2 fluxes exchanged with the atmosphere. The role of erosion as a net sink or source of atmospheric CO2 remains highly debated, and little information is available at scales larger than small catchments or regions. This study attempts to quantify the lateral transport of soil carbon and consequent land-atmosphere CO2 fluxes at the scale of China, where severe erosion has occurred for several decades. Based on the distribution of soil erosion rates derived from detailed national surveys and soil carbon inventories, here we show that water erosion in China displaced 180 +/- 80 Mt C.y(-1) of soil organic carbon during the last two decades, and this resulted a net land sink for atmospheric CO2 of 45 +/- 25 Mt C.y(-1), equivalent to 8-37% of the terrestrial carbon sink previously assessed in China. Interestingly, the "hotspots," largely distributed in mountainous regions in the most intensive sink areas (>40 g C.m(-2).y(-1)), occupy only 1.5% of the total area suffering water erosion, but contribute 19.3% to the national erosion-induced CO2 sink. The erosion-induced CO2 sink underwent a remarkable reduction of about 16% from the middle 1990s to the early 2010s, due to diminishing erosion after the implementation of large-scale soil conservation programs. These findings demonstrate the necessity of including erosion-induced CO2 in the terrestrial budget, hence reducing the level of uncertainty.
学科主题普通生物学
语种英语
WOS记录号WOS:000377948800032
源URL[http://ir.itpcas.ac.cn/handle/131C11/7678]  
专题青藏高原研究所_图书馆
通讯作者Ni, JR
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Alpine Ecol & Biodivers, Beijing 100101, Peoples R China
2.Catholic Univ Louvain, Earth & Life Inst, Georges Lemaitre Ctr Earth & Climate Res, B-1348 Louvain, Belgium
3.CSIRO, Land & Water, Canberra, ACT 2601, Australia
4.Univ Edinburgh, Sch Engn, Edinburgh EH9 3JL, Midlothian, Scotland
5.Peking Univ, Coll Environm Sci & Engn, The Key Lab Water & Sediment Sci, Minist Educ, Beijing 100871, Peoples R China
6.Wuhan Univ, Sch Water Resources & Hydropower Engn, Wuhan 430072, Peoples R China
7.Univ Versailles St Quentin En Yvelines, Commissariat Energie Atom & Energies Alternat, Inst Pierre Simon Laplace, Lab Sci Climat & Envirom,CNRS, F-91191 Gif Sur Yvette, France
8.Peking Univ, Dept Ecol, Beijing 100871, Peoples R China
9.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
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Borthwick, AGL ,Li, TH ,Wang, YC ,et al. Lateral transport of soil carbon and land-atmosphere CO2 flux induced by water erosion in China[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2016,113(24):6617-6622.
APA Borthwick, AGL .,Li, TH .,Wang, YC .,Chappell, A .,Van Oost, K .,...&Huang, MT .(2016).Lateral transport of soil carbon and land-atmosphere CO2 flux induced by water erosion in China.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,113(24),6617-6622.
MLA Borthwick, AGL ,et al."Lateral transport of soil carbon and land-atmosphere CO2 flux induced by water erosion in China".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 113.24(2016):6617-6622.

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来源:青藏高原研究所

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