Advances in Earth Science ›› 2018, Vol. 33 ›› Issue (11): 1130-1141. doi: 10.11867/j.issn.1001-8166.2018.11.1130.

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Progresses and Prospects of the Research on Soil Erosion in Karst Area of Southwest China *

Qianhong Ma( ), Keli Zhang *( )   

  1. State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science,Beijing Normal University, Beijing 100875,China
  • Received:2018-06-28 Revised:2018-09-27 Online:2018-11-20 Published:2018-12-21
  • Contact: Keli Zhang;
  • About author:

    First author:Ma Qianhong(1991-), female, Baoding City, Hebei Province, Ph. D student. Research areas include soil erosion in Karst area.

  • Supported by:
    Foundation item:Project supported by the National Natural Science Foundation of China "Multi-scale coupling of soil erosion and sediment transport in yellow soil area of Southwest China"(No.41730748).

Qianhong Ma, Keli Zhang. Progresses and Prospects of the Research on Soil Erosion in Karst Area of Southwest China *[J]. Advances in Earth Science, 2018, 33(11): 1130-1141.

The karst area of Southwest China is suffering from serious ecological and environmental problems due to soil erosion while the research on soil erosion is not sufficient. Primary achievement was systematically reviewed in this paper in three aspects: erosion characteristics, current researches about erosion on different spatial scales, and key scientific problems. Based on the review, the authors figured out the shortcomings of the existing studies and pointed out the directions on erosion study in southwest China karst region. The results showed that: ① Due to the existence of a dual structure in karst environment including ground and underground erosion, the process of runoff and sediment production on slope scale and confluence and sediment transportation processes on catchment scale were more complex under the unique geological and hydrological backgrounds; ② At present, most researches about erosion mechanism in karst area focus on slope scale and some achievements on quantitative evaluation of erosion factors have been made. Continuous data with high quality about relationship between water and sediment on catchment scale is limited. When data is scarce, river sediment data can be used as an effective way to study soil erosion intensity and spatial-temporal variation in karst area; ③ It is more reasonable to use 50 t/(km2·a) as the grading standard of soil loss tolerance than the previous grading standard of soil erosion intensity. Given the complex relationship between rocky desertification and soil erosion, more quantitative studies about the effects of rocky desertification on soil erosion are still necessary. There are different viewpoints on soil leakage definitions, leakage mechanism and leakage ratios, and new breakthroughs could be achieved by combining different methods and matching multi-scales. In conclusion, in order to further reveal soil erosion laws and establish and revise available regional soil erosion forecasting models for Southwest China karst areas, synchronous test and monitoring on slope, watershed, and channel spatial scales are urgently needed. The results can provide theoretical and technical support for promoting soil and water conservation work for the karst area of Southwest China.

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