Changes of SOC Content in China's Shendong Coal Mining Area during 1990-2020 Investigated Using Remote Sensing Techniques

被引:13
|
作者
Yang, Xuting [1 ,2 ]
Yao, Wanqiang [1 ,2 ]
Li, Pengfei [1 ,2 ]
Hu, Jinfei [1 ,2 ]
Latifi, Hooman [3 ,4 ]
Kang, Li [2 ]
Wang, Ningjing [1 ]
Zhang, Dingming [1 ]
机构
[1] Xian Univ Sci & Technol, Coll Geomat, Xian 710054, Peoples R China
[2] Minist Nat Resources, Key Lab Coal Resources Explorat & Comprehens Util, Xian 710021, Peoples R China
[3] KN Toosi Univ Technol, Fac Geodesy & Geomat Engn, Dept Photogrammetry & Remote Sensing, Tehran 1996715433, Iran
[4] Univ Wurzburg, Inst Geog & Geol, Dept Remote Sensing, D-97074 Wurzburg, Germany
基金
中国国家自然科学基金;
关键词
loess plateau; coal mining area; SOC content prediction; human disturbance; vegetation restoration; climate change; SOIL ORGANIC-CARBON; RECLAIMED MINE SOILS; LAND-USE CHANGE; SPATIAL VARIABILITY; LOESS PLATEAU; NITROGEN POOLS; FOREST SOILS; STOCKS; SEQUESTRATION; EROSION;
D O I
10.3390/su14127374
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Coal mining, an important human activity, disturbs soil organic carbon (SOC) accumulation and decomposition, eventually affecting terrestrial carbon cycling and the sustainability of human society. However, changes of SOC content and their relation with influential factors in coal mining areas remained unclear. In the study, predictive models of SOC content were developed based on field sampling and Landsat images for different land-use types (grassland, forest, farmland, and bare land) of the largest coal mining area in China (i.e., Shendong). The established models were employed to estimate SOC content across the Shendong mining area during 1990-2020, followed by an investigation into the impacts of climate change and human disturbance on SOC content by a Geo-detector. Results showed that the models produced satisfactory results (R-2 > 0.69, p < 0.05), demonstrating that SOC content over a large coal mining area can be effectively assessed using remote sensing techniques. Results revealed that average SOC content in the study area rose from 5.67 gC center dot kg(-1) in 1990 to 9.23 gC center dot kg(-1) in 2010 and then declined to 5.31 gC center dot Kg(-1) in 2020. This could be attributed to the interaction between the disturbance of soil caused by coal mining and the improvement of eco-environment by land reclamation. Spatially, the SOC content of farmland was the highest, followed by grassland, and that of bare land was the lowest. SOC accumulation was inhibited by coal mining activities, with the effect of high-intensity mining being lower than that of moderate- and low-intensity mining activities. Land use was found to be the strongest individual influencing factor for SOC content changes, while the interaction between vegetation coverage and precipitation exerted the most significant influence on the variability of SOC content. Furthermore, the influence of mining intensity combined with precipitation was 10 times higher than that of mining intensity alone.
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页数:21
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