中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Soil organic carbon storage changes in Yangtze Delta region, China

文献类型:期刊论文

作者Xu Naizheng1,2; Zhang Taolin1; Wang Xingxiang1; Liu Hongying2
刊名ENVIRONMENTAL EARTH SCIENCES
出版日期2011-07-01
卷号63期号:5页码:1021-1028
ISSN号1866-6280
关键词Soil organic carbon storage Soil organic carbon density Soil organic carbon storage change Yangtze Delta Region, China
DOI10.1007/s12665-010-0778-x
通讯作者Xu Naizheng(xzzz100@sina.com)
英文摘要Soil carbon sequestration plays an essential role in mitigating CO(2) increases and the global greenhouse effect. This paper calculates soil organic carbon (SOC) storage changes during the course of industrialization and urbanization in Yangtze Delta region, China, based on the data of the second national soil survey (1982-1985) and the regional geochemical survey (2002-2005), with the help of remote sensing images acquired in periods of 1980, 2000, 2005. The results show that soils in the top 0-20 and 0-100 cm depth in this region demonstrate the carbon sink effect from the early 1980s to the early 2000s. The SOC storage in 0-20 cm depth has resulted in increase from 213.70 to 238.65 Tg, which corresponds to the SOC density increase from 2.94 +/- A 1.08 to 3.28 +/- A 0.92 kg m(-2), and mean carbon sequestration storage and rate are 1.25 Tg a(-1), 17.14 g m(-2) a(-1), respectively. The SOC storage in 0-100 cm depth has resulted in increase from 690.26 to 792.65 Tg, which corresponds to the SOC density increase from 9.48 +/- A 4.22 to 10.89 +/- A 3.42 kg m(-2), and mean carbon sequestration storage and rate are 5.12 Tg a(-1), 70.32 g m(-2) a(-1), respectively. Urban area in Yangtze Delta region, China, increased more than 3,000 km(2) and the urban growth patterns circled the central city region in the past 20 years. The SOC densities in 0-20 cm depth decrease gradually along urban-suburban-countryside and the urban topsoil is slightly enriched with SOC. Compared to the data of the second national soil survey in the early 1980s, the mean SOC density in urban area increased by 0.76 kg m(2), or up 25.85% in the past 20 years. With the characteristics of SOC storage changes offered, land-use changes, farming system transition and ecological city construction are mainly attributed to SOC storage increases. Because of lower SOC content in this region, it is assumed that the carbon sink effect will go on in the future through improved soil management.
收录类别SCI
WOS关键词AGRICULTURAL SOILS ; SEQUESTRATION ; STOCKS
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
语种英语
出版者SPRINGER
WOS记录号WOS:000291486400012
URI标识http://www.irgrid.ac.cn/handle/1471x/2559082
专题南京土壤研究所
通讯作者Xu Naizheng
作者单位1.Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Peoples R China
2.Nanjing Inst Geol & Mineral Resources, Nanjing 210016, Peoples R China
推荐引用方式
GB/T 7714
Xu Naizheng,Zhang Taolin,Wang Xingxiang,et al. Soil organic carbon storage changes in Yangtze Delta region, China[J]. ENVIRONMENTAL EARTH SCIENCES,2011,63(5):1021-1028.
APA Xu Naizheng,Zhang Taolin,Wang Xingxiang,&Liu Hongying.(2011).Soil organic carbon storage changes in Yangtze Delta region, China.ENVIRONMENTAL EARTH SCIENCES,63(5),1021-1028.
MLA Xu Naizheng,et al."Soil organic carbon storage changes in Yangtze Delta region, China".ENVIRONMENTAL EARTH SCIENCES 63.5(2011):1021-1028.

入库方式: iSwitch采集

来源:南京土壤研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。