|
Spatial Distribution and Driving Factors of Karst Rocky Desertification in Lijiang River Basin
ZHU Bailu, YANG Qiyong, XIE Yunqiu, DENG Yan, TANG Meirong, LIU Dacun, ZENG Hongchun
Journal of Guangxi Normal University(Natural Science Edition). 2021, 39 (3):
139-150.
DOI: 10.16088/j.issn.1001-6600.2020052702
Karst rocky desertification of land is the most serious ecological problem in Southwest China, which threatens and restricts the sustainable development of the region. Taking the typical karst landform-Lijiang River basin as the study area, combining 6 natural environmental factors with 3 social environmental factors, based on GIS method and geographical detector method, the spatial distribution and key driving factors of karst rocky desertification in Lijiang River basin were analyzed. The results show that the total area of karst rocky desertification in Lijiang River basin is 1 547.6 km2, accounting for 8.9% of the total land area of the Lijiang River basin, and the proportion of light, medium and severe karst rocky desertification in the total area of karst rocky desertification is 50.0%, 34.2% and 15.8%, respectively. In terms of space, Yangshuo County and Qixing District have the most extensive karst rocky desertification distribution, accounting for more than 18% of the total land area of their respective administrative regions. The middle and lower reaches of the Lijiang River are significantly more karst rocky desertification than the upper reaches. The contribution of natural environmental factors to karst rocky desertification is greater than that of social environmental factors. The influences of environmental factors from large to small are lithology, geomorphology, NDVI, elevation, road distance, population density, average annual precipitation, slope, and GDP. Lithology (0.34) and geomorphology (0.28) are the key driving factors of karst rocky desertification, and their explanatory power for the interaction of karst rocky desertification reaches 0.45.
References |
Related Articles |
Metrics
|