An analysis of groundwater circulation in the Pingyu mining area based on hydrochemical and isotopic characteristics of groundwater

SU Huimeng; ZHANG Fawang; HOU Suyu; ZHAO Baoyin; YANG Bo; WANG Yulong; ZUO Wei; LU Guihai; LI Honggang

doi:10.16030/j.cnki.issn.1000-3665.202306010

Volume 50 Issue 5

Sep. 2023

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Hydrogeology & Engineering Geology > 2023 > 50(5): 53-67. > DOI: 10.16030/j.cnki.issn.1000-3665.202306010

SU Huimeng, ZHANG Fawang, HOU Suyu, et al. An analysis of groundwater circulation in the Pingyu mining area based on hydrochemical and isotopic characteristics of groundwater[J]. Hydrogeology & Engineering Geology, 2023, 50(5): 53-67. DOI: 10.16030/j.cnki.issn.1000-3665.202306010

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An analysis of groundwater circulation in the Pingyu mining area based on hydrochemical and isotopic characteristics of groundwater

SU Huimeng^1,,
ZHANG Fawang^{1, 2, ,},
HOU Suyu³,
ZHAO Baoyin⁴,
YANG Bo^{5, 6},
WANG Yulong^{5, 6},
ZUO Wei^{5, 6},
LU Guihai⁴,
LI Honggang⁴

1.
School of Environmental Studies, China University of Geosciences （Wuhan）, Wuhan，Hubei　430074, China
2.
Center for Hydrogeology and Environmental Geology, China Geological Survey, Baoding, Hebei　071051, China
3.
China Nuclear Dadi Exploration and Technical Design Co. Ltd., Beijing　100013, China
4.
Henan Branch, China South-to-North Water Diversion Middle Route Co. Ltd., Zhengzhou, Henan　450016, China
5.
The Fifth Geological Survey Institute, Henan Provincial Bureau of Geology and Mineral Resources, Zhengzhou, Henan　450001, China
6.
Natural Resources Science and Technology Innovation Center of Henan Province （Research on Eco-Environmental Assessment and Restoration Technology）, Zhengzhou, Henan　450001, China

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Received Date: June 01, 2023
Revised Date: July 27, 2023
Available Online: August 21, 2023
Published Date: September 18, 2023

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Abstract

Abstract

Groundwater in mining areas play an important supporting role in the surrounding residents' living and the construction of coal industries. Mine drainage during coal mining will change the original groundwater circulation process in mining areas, leading to changes in the groundwater environment. Therefore, clarifying the mutual transformation relationship between the “three waters” is the key to the scientific utilization of water resources in mining areas. Chemical components and hydrogen and oxygen isotopes of the groundwater in the Pingyu mining area are combined to determine the characteristics of groundwater circulation after large-scale drainage of the mine, identify the origin and controlling factors of the major components in the groundwater. Hydrohemical analyses show that most of the groundwater are of HCO₃—Ca·Mg type, The hydrochemical components are controlled by the weathering and dissolution of silicate, and the ions in the groundwater mainly come from water-rock interactions and the waste generated by human activities, with concentration of ${\rm{NO}}_3^-$ exceeding the standard. The hydrogen and oxygen isotopic data demonstrates that the groundwater in the study area receives recharge from modern precipitation, and there is a close hydraulic relationship between the groundwater in the unconsolidated aquifers and the groundwater in the karst aquifer. After the mine drainage, the groundwater circulation process in the mining area changes, the karst groundwater changes from supporting the upper pore groundwater to accepting the leakage recharge of the upper pore groundwater, and then discharges to the surface water by the mine drainage. The mine drainage becomes the main groundwater drainage way in the mine area. The research results can provide scientific and effective basis for groundwater development management and land subsidence prevention in mining areas.

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An analysis of groundwater circulation in the Pingyu mining area based on hydrochemical and isotopic characteristics of groundwater

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An analysis of groundwater circulation in the Pingyu mining area based on hydrochemical and isotopic characteristics of groundwater

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