1. 贵州师范大学喀斯特研究院,贵阳,550001
2. 贵州省喀斯特山地生态环境国家重点实验室培育基地,贵阳,550001
3. 国家喀斯特石漠化防治工程技术研究中心,贵阳,550001
纸质出版:2017
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张珊珊, 周忠发, 孙小涛, 等. 基于坡度等级的喀斯特山区石漠化与水土流失相关性研究——以贵州省盘县为例[J]. 水土保持学报, 2017,31(2):79-86.
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.
张珊珊, 周忠发, 孙小涛, 等. 基于坡度等级的喀斯特山区石漠化与水土流失相关性研究——以贵州省盘县为例[J]. 水土保持学报, 2017,31(2):79-86. DOI: 10.13870/j.cnki.stbcxb.2017.02.015.
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.
为了定量分析不同坡度等级下石漠化与水土流失之间的相关性,为县域生态环境治理与修复提供科学理论依据,以贵州省盘县为研究区,在遥感与地理信息系统技术支持下,以ALOS遥感影像、岩性及1∶50 000地形图等为基础数据源,采用遥感解译方法、表面分析及地图代数原理,提取出石漠化与水土流失的各指标因子。通过ArcGIS空间分析及相关性分析模型,从不同坡度等级下分析盘县石漠化与水土流失的相关性。结果表明:盘县石漠化面积为1 008.45 km2,占总面积的24.9%,已发生石漠化等级以轻度、中度和强度为主,分别占盘县石漠化面积的45.47%,29.67%,20.29%;水土流失面积为521.05 km2,占总面积的12.85%,已发生水土流失等级以轻度和中度为主,分别占盘县水土流失面积的67.75%和17.36%。石漠化与水土流失发生区坡度以5°~35°为主,分别占石漠化与水土流失面积的85.08%与82.45%。当坡度<8°时,石漠化与水土流失等级、水土流失与石漠化等级存在着负相关关系。当坡度为8°~35°时,已石漠化与已水土流失面积均呈现出先减小后增加再减小的趋势。当坡度>35°时,石漠化与水土流失等级在强烈侵蚀等级以下表现为负相关,超过强烈侵蚀为正相关;而水土流失与石漠化等级在轻度石漠化等级以下表现为正相关,超过轻度石漠化为负相关。
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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