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2023 Vol. 50, No. 5
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ZHAO Chunhong, LIANG Yongping, WANG Zhiheng, TANG Chunlei, SHEN Haoyong. 2023. Dynamic characteristics and evolution mechanism of 'goaf water' of coal mine in Shandi River Basin, Yangquan, Shanxi Province and its environmental effects on Niangziguan Spring Area[J]. Geology in China, 50(5): 1471-1485. doi: 10.12029/gc20220327001
Citation: ZHAO Chunhong, LIANG Yongping, WANG Zhiheng, TANG Chunlei, SHEN Haoyong. 2023. Dynamic characteristics and evolution mechanism of "goaf water" of coal mine in Shandi River Basin, Yangquan, Shanxi Province and its environmental effects on Niangziguan Spring Area[J]. Geology in China, 50(5): 1471-1485. doi: 10.12029/gc20220327001
shu

Dynamic characteristics and evolution mechanism of "goaf water" of coal mine in Shandi River Basin, Yangquan, Shanxi Province and its environmental effects on Niangziguan Spring Area

  • 1.

    Guangxi Karst Resources and Environment Research Center of Engineering Technology/Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, Guangxi, China

  • 2.

    School of Environment and Spatial Informatics, China University of Mining and Technology, Xuzhou 221116, Jiangsu, China

  • 3.

    International Research Centre on Karst under the Auspices of UNESCO, National Center for International Research on Karst Dynamic System and Global Change, Guilin 541004, Guangxi, China

    • Fund Project: Supported by the National Natural Science Foundation of China (No.41672253), the projects of China Geological Survey (No.DD20230425, No.DD20160242) and the basic research business fee project of the Institute of Karst Geology, Chinese Academy of Geological Science (No.2022007)
More Information
  • Author Bio: ZHAO Chunhong, female, born in 1986, associate researcher, engaged in karst water resources and water environment research; E-mail: chunhong0504@163.com
  • Corresponding author: LIANG Yongping, male, born in 1962, researcher, engaged in the investigation and research on karst groundwater in North China; E-mail: lyp0261@163.com 
Received Date:  27 March 2022
Revised Date:  04 July 2022
Publish Date:  25 October 2023
    Abstract

  • This paper is the result of hydrogeological survey engineering.

     Objective

    With the characteristics of wide distribution, concealment, heavy pollution, slow natural purification and long duration, the "goaf water" of coal mine has become an important restrictive factor that seriously threatens the construction of ecological civilization in China in the post coal mining era.

     Methods

    Taking the goaf water of coal mine in Shandi River Basin of Yangquan City, Shanxi Province as the research object, this paper systematically analyzes the dynamic characteristics and evolution mechanism of water quantity and quality of goaf water in Shandi River Basin by using a long series of systematic monitoring of water quality and quantity, and statistical methods.

     Results

    The results indicate that the average pH of the total outlet of "goaf water" in Shandi River is 3.58, the average TDS is 4744 mg/L, and the average SO42- is 3327 mg/L. After the rise of groundwater level in rainy season, the increase of contact area or volume and the lag of rainfall are the main reasons for the nonlinear correlation between the flow of goaf water and the conductivity and SO42- concentration of hydrochemical characteristic indexes. The strong oxidation reaction of pyrite in coal measure strata mainly occurs in the seasonal variation zone of groundwater level, aeration zone and surface. The certain depth of the gob ponding area of the coal mine is the reduction environment, which has the conditions for microbial treatment. After the "goaf water" flows out, the leakage recharge in the downstream carbonate section is 7247.08 m3/d, and the water quality is poor, which is an important pollution source of karst groundwater in Niangziguan Spring area.

     Conclusions

    The regulation and storage period of "goaf water" flow to rainfall in Shandi river basin is half a year. The hydrochemical characteristic index is nonlinear related to the flow. The strong oxidation reaction of "goaf water" pyrite mainly occurs in the seasonal fluctuation zone of groundwater level, aeration zone and surface. After the "goaf water" flows out, the leakage recharge in the downstream carbonate section is 7247.08 m3/d, SO42-, Fe and Mn exceed the standard seriously, which is an important pollution source of karst groundwater in Niangziguan Spring area. It is urgent to carry out the treatment of "goaf water" in coal mines and the ecological restoration of abandoned coal mines.
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