Liao Wen, Hu Yanxia, Yu Xingxiu, et al. Spatiotemporal Variation and Influence Factors of Soil Conservation Function in Danjiangkou Reservoir Area During 2010-2020[J]. Bulletin of Soiland Water Conservation, 2021, 41(6): 288-294.
DOI:
Liao Wen, Hu Yanxia, Yu Xingxiu, et al. Spatiotemporal Variation and Influence Factors of Soil Conservation Function in Danjiangkou Reservoir Area During 2010-2020[J]. Bulletin of Soiland Water Conservation, 2021, 41(6): 288-294. DOI: 10.13961/j.cnki.stbctb.2021.06.037.
Spatiotemporal Variation and Influence Factors of Soil Conservation Function in Danjiangkou Reservoir Area During 2010-2020
[Objective] The spatial and temporal characteristics of soil conservation function and its influencing factors in Danjiangkou Reservoir area were scientifically evaluated
in order to provide a scientific basis for the establishment of soil erosion control models in the water source area of the middle route of the south-to-north water transfer project and the soil and water conservation and ecosystem safety management in the basin.[Methods] The InVEST model and the geographical detector method were used to quantitatively analyze the temporal and spatial characteristics of soil conservation function and its influencing factors in Danjiangkou Reservoir area in 2010
2015 and 2020.[Results] Firstly
from 2010 to 2020
both of the actual amount of soil erosion and the soil erosion grade in the Danjiangkou Reservoir area decreased
and the spatial distribution trend in each year was basically consistent. Secondly
the conserved soil in Danjiangkou Reservoir area in 2010
2015 and 2020 was 6.25×109 t
6.62×109 t and 7.12×109 t
respectively
which showed a gradual upward trend
indicating that the soil conservation function of the Danjiangkou Reservoir area has been continuously enhanced. Thirdly
the soil conservation function was varied in different altitude ranges. The quantity of soil conservation was larger in higher altitude areas
such as Funiu Mountains in the northeast
Qinling Mountains in the west
and Wudang Mountains in the southwest. The quantity of soil conservation was smaller in lower-altitude areas
such as the area around the Danjiangkou Reservoir. The quantity of soil conservation of different land-use types was also quite different
with wood land being the largest
followed by shrub rangeland
garden land and cultivated land. Last
the geographical detector analysis results showed that the changes in soil conservation function in the Danjiangkou Reservoir area were mainly affected by topographic factors.[Conclusion] In recent years
the soil conservation function in the Danjiangkou Reservoir area has been changed in a positive trend in general
although the quantity of soil conservation in some areas is still small. In the future
the returning farmland to forest land (or grassland) should continue to be promoted
and forest land and shrubland with strong soil conservation capabilities should be focused and protected so as to enhance the soil conservation function of Danjiangkou Reservoir area.
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