Characteristics of soil and water loss in the Lijiang River Basin and soil erosion factors in typical karst small watersheds

QIN Xingming; HE Binghui; SHEN Lina; WANG Kui; YU Qiwen; ZHANG Luyao

doi:10.11932/karst20180305

Volume 37 Issue 3

Jun. 2018

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Article Navigation > CARSOLOGICA SINICA > 2018 > 37(3): 351-360

QIN Xingming, HE Binghui, SHEN Lina, WANG Kui, YU Qiwen, ZHANG Luyao. Characteristics of soil and water loss in the Lijiang River Basin and soil erosion factors in typical karst small watersheds[J]. CARSOLOGICA SINICA, 2018, 37(3): 351-360. doi: 10.11932/karst20180305

Citation:

QIN Xingming, HE Binghui, SHEN Lina, WANG Kui, YU Qiwen, ZHANG Luyao. Characteristics of soil and water loss in the Lijiang River Basin and soil erosion factors in typical karst small watersheds[J]. CARSOLOGICA SINICA, 2018, 37(3): 351-360. doi: 10.11932/karst20180305

Citation:

QIN Xingming, HE Binghui, SHEN Lina, WANG Kui, YU Qiwen, ZHANG Luyao. Characteristics of soil and water loss in the Lijiang River Basin and soil erosion factors in typical karst small watersheds[J]. CARSOLOGICA SINICA, 2018, 37(3): 351-360. doi: 10.11932/karst20180305

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Characteristics of soil and water loss in the Lijiang River Basin and soil erosion factors in typical karst small watersheds

doi: 10.11932/karst20180305

1.
School of Resources and Environment, Southwest University/Institute of Karst Geology, Chinese Academy of Geological Sciences/Key Laboratory of Karst Ecosystem and Treatment of Rocky Desertification, MNR
2.
School of Resources and Environment, Southwest University
3.
Institute of Karst Geology, Chinese Academy of Geological Sciences/Key Laboratory of Karst Ecosystem and Treatment of Rocky Desertification, MNR

Publish Date: 2018-06-25

Abstract

Abstract

The purpose of this study is to determine the characteristics of soil erosion in the Lijiang River Basin and the relationship between soil erosion and impact factors in the Zhaidi karst underground river watershed. The distribution feature of soil and water loss on a medium scale in the Lijiang River Basin and the influencing factors of soil erosion on a large scale are analyzed based on remote sensing interpretations and field investigations. Research reveals that the soil erosion in the basin is dominated by moderate and medium degrees, which account for 29.9% of the total drainage area. There are obvious differences in soil and water loss between karst area and non-karst areas in the basin, where soil and water losses in the karst area are moderate , extremely strong and medium, accounting for 53% of the entire karst area; while moderate and medium soil erosion in the non karst area accounts for 12.4% and 10.4% of the total non-karst area respectively. The Zhaidi karst underground river is located in the southeast of Guilin, Guangxi Zhuang Autonomous Region, which belongs to the Caotian river, a tributary of the Lijiang River. The relationships between the soil erosion amount, soil erosion area, influencing factors including elevation, slope, vegetation coverages and land utilization are also analyzed. The results show that the 300-500 m elevations, 15-25 degree slopes, less than 20% vegetation coverage and industrial and mining lands pose the largest influences on soil erosion in the karst small watersheds.
- Lijiang River Basin,
- soil erosion,
- Zhaidi karst watershed,
- influencing factor of soil erosion,
- influence ratio

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