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Chinese Journal of Applied Ecology ›› 2021, Vol. 32 ›› Issue (6): 2107-2118.doi: 10.13287/j.1001-9332.202106.013

• Original Articles • Previous Articles     Next Articles

Soil-epikarst structures and their hydrological characteristics on dolomite slopes in karst region of southwest China

ZHANG Jun1,2,3, FU Zhi-yong1,2, CHEN Hong-song1,2*, LIAN Jin-jiao1,2, QIN Chang4   

  1. 1Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China;
    2Huangjiang Observation and Research Station of Karst Ecosystem, Chinese Academy of Sciences, Huangjiang 547100, Guangxi, China;
    3University of the Chinese Academy of Sciences, Beijing 100049, China;
    4Guangxi Hydrogeology and Engineering Geology Institute, Liuzhou 545006, Guangxi, China
  • Received:2020-11-24 Accepted:2021-02-20 Published:2021-12-15
  • Contact: * E-mail: hbchs@isa.ac.cn
  • Supported by:
    National Natural Science Foundation of China (41930866), the Guangxi Natural Science foundation (2018GXNSFGA281003),the National Science Foundation of China (41971048, 41701044).

Abstract: Epikarst is the core area of karst critical zone, with important hydrologic regulation and storage function. However, the effects of karst development degree on hydrologic characteristics of epikasrt is still unclear. We used geophysical exploration and hydrogeological techniques, combined with the dynamic monitoring of moisture and water levels, to quantify the karst development degrees and their hydrologic characteristics on slope lands. We analyzed the responses of soil-epikarst systems to rainfall. Results showed that geophysical exploration technology could be well applied to the detection of surface-subsurface structures in the karst areas. The average thickness of soil and surface karst zone on the slope was less than 0.63 m and 2.60 m, respectively. The slopes of strong-karstification characterized by high apparent resistivity, well-developed joint fractures, and strong permeability (0.73 m·d-1). Such a result indicated that epikarst could regulate precipitation. The responses of soil moisture had a larger rainfall threshold (>20.50 mm·d-1) and the water level was determined by rainfall amount. In contrast, the slope with weak-karstification had low apparent resistivity and weak permeability (0.07 m·d-1). Moisture and water level were sensitive to rainfall. Karst channels were developed locally at 240-300 cm with a permeability coefficient of up to 432 mm·d-1. Obvious preferential flow was observed in extreme rainfall events on this slope, which could induce flood disaster in the adjacent depression. Our results would provide scientific basis for further research on water resources regulation, management, and eco-hydrology in karst areas of southwest China.

Key words: karst critical zone, geophysical exploration, thickness of epikarst, permeability coefficient, water dynamic, groundwater level dynamic