Volume 48 Issue 1
Feb.  2020
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ZHENG Zhuyan, XU Guangquan, YANG Tingting, YU Shitao, ZHANG Haitao. Hydrochemical formation mechanism and transmissivity-impermeability analysis of karst groundwater on both sides of fault F104 in Gubei coal mine in Huainan[J]. COAL GEOLOGY & EXPLORATION, 2020, 48(1): 129-137. DOI: 10.3969/j.issn.1001-1986.2020.01.017
Citation: ZHENG Zhuyan, XU Guangquan, YANG Tingting, YU Shitao, ZHANG Haitao. Hydrochemical formation mechanism and transmissivity-impermeability analysis of karst groundwater on both sides of fault F104 in Gubei coal mine in Huainan[J]. COAL GEOLOGY & EXPLORATION, 2020, 48(1): 129-137. DOI: 10.3969/j.issn.1001-1986.2020.01.017
shu

Hydrochemical formation mechanism and transmissivity-impermeability analysis of karst groundwater on both sides of fault F104 in Gubei coal mine in Huainan

  • School of Earth and Environment, Anhui University of Science and Technology, Huainan 232001, China

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National Natural Science Foundation of China (41572147)

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  • Received Date: March 10, 2019
  • Revised Date: June 26, 2019
  • Published Date: February 24, 2020
    Graphical Abstract
    • Abstract
  • It is of great practical significance for the prevention and control of groudwater hazards in North China type coalfield to judge transmissivity-impermeability of faults by using karst hydrochemical characteristics of two fault walls. Taking karst groundwater of Taiyuan Formation on both sides of fault F104 in Gubei coal mine as the research object, and based on the analysis of the hydrogeological conditions of two fault walls, main components sources and water-rock interaction differences were analyzed by using Piper trilinear diagram, ion combination ratio and principal component methods. Reverse hydrochemical simulation of karst groundwater was conducted by using PHREEQC software. Research results show that dissolution and precipitation of calcite and dolomite exist in the north and south areas; cation exchange and desulfurization in the south region are stronger than that in the north area; while oxidation of pyrite and dissolution of salt rock in the north area is more obvious than those in the south area; there are significant differences in the hydrochemical environment and water-rock interaction between the two areas. It is inferred that fault F104 has a preferably water-resistance, and affects the oxidation-reduction environment and temperature differences of the two areas, which controlling the direction of groundwater runoff and the degree of water-rock interaction.
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