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Article Navigation >  CARSOLOGICA SINICA  > 2025  > Accepted Manuscript
HUANG Qibo, KANG Zhiqiang, DENG Zhong, TANG Yongchen, WU Huaying, ZOU Changpei, LI Tengfang, LIAO Hongwei, MA Junfei, LIANG Jian. Mechanism of karst Waterlogging formation and effective control[J]. CARSOLOGICA SINICA. doi: 10.11932/karst2025y020
Citation: HUANG Qibo, KANG Zhiqiang, DENG Zhong, TANG Yongchen, WU Huaying, ZOU Changpei, LI Tengfang, LIAO Hongwei, MA Junfei, LIANG Jian. Mechanism of karst Waterlogging formation and effective control[J]. CARSOLOGICA SINICA. doi: 10.11932/karst2025y020
shu

Mechanism of karst Waterlogging formation and effective control

doi: 10.11932/karst2025y020
  • 1.

    Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR & GZAR/International Research Center on Karst under the Auspices of UNESCO, Guilin, Guangxi 541004, China

  • 2.

    Pingguo Guangxi, Karst Ecosystem, National Observation and Research Station, Pingguo, Guangxi 531406, China

  • 3.

    Guangxi Bureau of Geology & Mineral Prospecting & Exploitation, Nanning, Guangxi 530023, China

  • 4.

    Guangxi Institute of Hydrogeology and Engineering Geology Survey, Liuzhou, Guangxi 545006, China

  • Received Date: 2025-01-05
  • Accepted Date: 2025-05-06
  • Rev Recd Date: 2025-04-24
    • Available Online: 2025-10-20
    Abstract
  • The global karst area is about 22 million km2, accounting for 15% of the global land area. The people in karst areas are threatened to varying degrees by droughts and floods. Waterlogging is a geological hazard formed by the superposition of karst geological and geomorphological environment and human activities. The closed karst terrain combined with strong human engineering activities causes serious soil erosion. Soil leaks into the lower karst pipeline through the sinkhole, causing underground pipeline blockage , drainage obstruction, and frequent occurrence of waterlogging; With the increase of extreme weather, human activities, soil erosion in low-lying areas, and blockage of karst pipelines, if left untreated for a long time, the waterlogging time in low-lying areas will become more frequent and severe.Karst Waterlogging disasters have caused significant losses to people in karst areas, seriously threatening their production and life. The comprehensive management of these disasters has a major national demand. The characteristics of Waterlogging disasters are periodicity, group occurrence, and suddenness. The enclosed karst landform and the special "binary" structure of the karst aquifer are the internal factors that cause karst Waterlogging. The subtropical monsoon climate with concentrated rainfall is the external condition for the occurrence of karst Waterlogging. Unreasonable engineering activities have caused a large amount of soil and water loss, blocking underground karst channels, which is the human factor leading to increasingly karst Waterlogging. Severe karst Waterlogging mainly occurs in karst valleys and depressions where underground rivers and pipelines are developed. The recharge area, runoff area, and discharge area of an underground river have different mechanisms for causing internal Waterlogging.At present, there is a lack of systematic research and characterization of the "binary" structure of karst aquifers. Soil erosion leads to a decrease in the rainfall threshold for causing Waterlogging, and no relevant studies have been conducted on the impact of soil erosion on degeneration of underground pipeline water conveyance capacity. There is a lack of in-depth research on the formation mechanism of karst Waterlogging disasters, and it is even more impossible to predict the extent of karst Waterlogging disasters and the losses caused under extreme climate events, which seriously affects the effectiveness of karst Waterlogging control. In the later stage, systematic observations of the hydrological dynamics and soil erosion dynamics that lead to urban Waterlogging should be carried out, characterize the karst aquifer fracture-cave "dual" structure in detail, clarify the rainfall threshold and its changing characteristics that cause urban Waterlogging, elucidate the hydrological processes and soil erosion processes and their controlling factors that lead to the formation of karst Waterlogging disasters, analyze the relationship between reduction coefficient of outlet flow and the amount of soil erosion in low-lying areas, and systematically reveal the mechanism, evolution laws, and principles of karst Waterlogging formation, and then propose scientifically effective countermeasures for karst Waterlogging regulation.

     

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