ZHANG Shanshan1, 2, ZHOU Zhongfa1, et al. Based on the Slope Grade of Rocky Desertification and Water and Soil Loss Correlation Study in Karst Mountain Area: A Case in Panxian County, Guizhou[J]. 2017, 31(2): 79-86.
DOI:
ZHANG Shanshan1, 2, ZHOU Zhongfa1, et al. Based on the Slope Grade of Rocky Desertification and Water and Soil Loss Correlation Study in Karst Mountain Area: A Case in Panxian County, Guizhou[J]. 2017, 31(2): 79-86. DOI: 10.13870/j.cnki.stbcxb.2017.02.015.
Based on the Slope Grade of Rocky Desertification and Water and Soil Loss Correlation Study in Karst Mountain Area: A Case in Panxian County, Guizhou
The aims of this study were to analyze the correlation between rocky desertification at different slopes and water and soil loss quantitatively
and provide the scientific theoretical basis for the ecological environment management and restoration in the county area. Takeing Panxian County of Guizhou Province as the research area
with the support of RS and GIS technology
based on ALOS remote sensing images
lithology and 1∶50 000 topographic maps
using Remote sensing interpretation method
Surface analysis and Map Algebra principle
the index factors of rocky desertification and water and soil loss were extracted. Through ArcGIS spatial analysis and correlation analysis model
analysis of the correlation between rocky desertification at different slopes and water and soil loss in Panxian County. The results showed that: Panxian County had a rocky desertification area of 1 008.45 km2
accounting for 24.9% of the total area
the degree of rocky desertification was mainly mild
moderate and strong
accounting for 45.47%
29.67% and 20.29% of the total area of rocky desertification
respectively. Water and soil loss area of 521.05 km2
accounting for 12.85% of the total area
the degree of water and soil loss was maily mild and moderate
and 67.75% and 17.36% of the area of water and soil loss
respectively. Rocky desertification and water and soil loss occurred in the place where the slopes were 5 and 35 degrees
accounting for 85.08% and 82.45% of the area of rocky desertification and water and soil loss
respectively. When the slopes were less than 8 degrees
there was a negative correlation between rocky desertification and grade of water and soil loss
and between water and soil loss and grade of rocky desertification. When the slopes were between 8 and 35 degrees
the area of rocky desertification and water and soil loss decreased first
then increased
and later decreased again. When the slopes were greater than 35 degrees
rocky desertification and water and soil loss grade were negatively correlated under strong erosion
but the correlation became positive when the erosion went beyond strong erosion. Water and soil loss and rocky desertification grade were positively correlated under mild rocky desertification
but they were negatively correlated when the rocky desertification went beyond mild rocky desertification.
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Related Institution
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