Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000

Spatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year 1980 to 2000 in an area of 2.97 × 106 km2 in eastern China were investigated using a land use dataset from a recent soil geochemical survey. A map of soil carbon sources/sinks has been prepared based...

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Main Authors: Xueqi Xia, Zhongfang Yang, Yuan Xue, Xin Shao, Tao Yu, Qingye Hou
Format: Article
Language:English
Published: Elsevier 2017-05-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987116300573
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author Xueqi Xia
Zhongfang Yang
Yuan Xue
Xin Shao
Tao Yu
Qingye Hou
author_facet Xueqi Xia
Zhongfang Yang
Yuan Xue
Xin Shao
Tao Yu
Qingye Hou
author_sort Xueqi Xia
collection DOAJ
description Spatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year 1980 to 2000 in an area of 2.97 × 106 km2 in eastern China were investigated using a land use dataset from a recent soil geochemical survey. A map of soil carbon sources/sinks has been prepared based on a spatial analysis scheme with GIS. Spatial statistics showed that land use changes had caused 30.7 ± 13.64 Tg of surface soil organic carbon loss, which accounts for 0.33% of the total carbon storage of 9.22 Pg. The net effect of the carbon source was estimated to be ∼71.49 Tg soil carbon decrease and ∼40.80 Tg increase. Land use changes in Northeast China (NE) have the largest impact on soil organic carbon storage compared with other regions. Paddy fields, which were mainly transformed into dry farmland in NE, and constructed land in other regions, were the largest carbon sources among the land use types. Swamp land in NE was also another large soil carbon source when it was transformed into dry farmland or paddy fields. Dry farmland in the NE region formed the largest soil organic carbon sink, as some were transformed into paddy fields, forested land, and other land use types with high SOCD.
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spelling doaj.art-fed40597a4fc4186bae184f59a0925f52023-09-02T10:24:43ZengElsevierGeoscience Frontiers1674-98712017-05-018359760310.1016/j.gsf.2016.06.003Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000Xueqi Xia0Zhongfang Yang1Yuan Xue2Xin Shao3Tao Yu4Qingye Hou5School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaSchool of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaChongqing Institute of Land Surveying and Planning, Chongqing 404000, ChinaSchool of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaSchool of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaSchool of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaSpatial distributions of 0–20 cm soil carbon sources/sinks caused by land use changes from the year 1980 to 2000 in an area of 2.97 × 106 km2 in eastern China were investigated using a land use dataset from a recent soil geochemical survey. A map of soil carbon sources/sinks has been prepared based on a spatial analysis scheme with GIS. Spatial statistics showed that land use changes had caused 30.7 ± 13.64 Tg of surface soil organic carbon loss, which accounts for 0.33% of the total carbon storage of 9.22 Pg. The net effect of the carbon source was estimated to be ∼71.49 Tg soil carbon decrease and ∼40.80 Tg increase. Land use changes in Northeast China (NE) have the largest impact on soil organic carbon storage compared with other regions. Paddy fields, which were mainly transformed into dry farmland in NE, and constructed land in other regions, were the largest carbon sources among the land use types. Swamp land in NE was also another large soil carbon source when it was transformed into dry farmland or paddy fields. Dry farmland in the NE region formed the largest soil organic carbon sink, as some were transformed into paddy fields, forested land, and other land use types with high SOCD.http://www.sciencedirect.com/science/article/pii/S1674987116300573Land use changeSoil organic carbonGISEastern China
spellingShingle Xueqi Xia
Zhongfang Yang
Yuan Xue
Xin Shao
Tao Yu
Qingye Hou
Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
Geoscience Frontiers
Land use change
Soil organic carbon
GIS
Eastern China
title Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
title_full Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
title_fullStr Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
title_full_unstemmed Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
title_short Spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of China between 1980 and 2000
title_sort spatial analysis of land use change effect on soil organic carbon stocks in the eastern regions of china between 1980 and 2000
topic Land use change
Soil organic carbon
GIS
Eastern China
url http://www.sciencedirect.com/science/article/pii/S1674987116300573
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