中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Environmental controls on soil organic carbon and nitrogen stocks in the high-altitude arid western Qinghai-Tibetan Plateau permafrost region

文献类型:期刊论文

作者Wu, Xiaodong1; Zhao, Lin1; Fang, Hongbing1; Zhao, Yuguo2; Smoak, Joseph M.3; Pang, Qiangqiang1; Ding, Yongjian1
刊名JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
出版日期2016
卷号121期号:1页码:176-187
关键词permafrost Qinghai-Tibetan Plateau SOC stocks total nitrogen active layer desert steppe
ISSN号2169-8953
DOI10.1002/2015JG003138
通讯作者Zhao, Lin(linzhao@lzb.ac.cn) ; Ding, Yongjian(dyj@lzb.ac.cn)
英文摘要While permafrost in the circum-Artic has great influence on soil organic carbon (SOC) and total nitrogen (TN) stocks, this might not be the case in low-latitude arid permafrost regions. We test this hypothesis in the western Qinghai-Tibetan Plateau (QTP) permafrost region. Fifty-nine soil profiles were analyzed to examine the SOC and TN distribution and the controlling factors in western QTP, which is a desert steppe ecoregion. Mean stocks of SOC (5.29kgm(-2)) and TN (0.56kgm(-2)) for the top 200cm in this area were lower than those of the east QTP and circum-Arctic regions. The SOC and TN stocks under vegetative cover with permafrost conditions were significantly higher than those of desert conditions. The SOC and TN stocks for the layers of different depths were related to the content of clay, silt, and moisture. Although the active layer thickness (ALT) had a significant negative correlation to soil moisture, the ALT explained little or no variance in the SOC and TN stocks. The results showed that in the vast permafrost regions of the western QTP, the SOC and TN stocks are very low, and the main controlling factors for the SOC and TN are soil texture, moisture, and vegetation type. The SOC pool in this area may not be as vulnerable to degradation associated with climate warming and thus not emit greenhouse gases at the same rate as other permafrost regions. The different response of the SOC in this region should be considered in carbon cycling models.
收录类别SCI
WOS关键词HEIHE RIVER-BASIN ; NORTHWESTERN CHINA ; ARCTIC ALASKA ; UPPER REACH ; CLIMATE ; MATTER ; STORAGE ; TUNDRA ; PRECIPITATION ; VULNERABILITY
WOS研究方向Environmental Sciences & Ecology ; Geology
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000370173100011
出版者AMER GEOPHYSICAL UNION
URI标识http://www.irgrid.ac.cn/handle/1471x/2557393
专题寒区旱区环境与工程研究所
通讯作者Zhao, Lin; Ding, Yongjian
作者单位1.Chinese Acad Sci, Cryosphere Res Stn Qinghai Tibetan Plateau, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou, Peoples R China
2.Chinese Acad Sci, Inst Soil Sci, Nanjing, Jiangsu, Peoples R China
3.Univ S Florida, Dept Environm Sci Policy & Geog, St Petersburg, FL 33701 USA
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GB/T 7714
Wu, Xiaodong,Zhao, Lin,Fang, Hongbing,et al. Environmental controls on soil organic carbon and nitrogen stocks in the high-altitude arid western Qinghai-Tibetan Plateau permafrost region[J]. JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,2016,121(1):176-187.
APA Wu, Xiaodong.,Zhao, Lin.,Fang, Hongbing.,Zhao, Yuguo.,Smoak, Joseph M..,...&Ding, Yongjian.(2016).Environmental controls on soil organic carbon and nitrogen stocks in the high-altitude arid western Qinghai-Tibetan Plateau permafrost region.JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,121(1),176-187.
MLA Wu, Xiaodong,et al."Environmental controls on soil organic carbon and nitrogen stocks in the high-altitude arid western Qinghai-Tibetan Plateau permafrost region".JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 121.1(2016):176-187.

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来源:寒区旱区环境与工程研究所

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