Hydrochemical and Isotopic Characteristics and Water Assessment Analysis of Surface Water and Groundwater Near Bolokenu–Aqikekuduke Fault in Xinjiang

YANG Mingyuan; ZHAO Jiayi; MA Chao; LI Xin

doi:10.12401/j.nwg.2023009

Northwestern Geology > 2023 > 56(6): 186-197. > DOI: 10.12401/j.nwg.2023009

YANG Mingyuan, ZHAO Jiayi, MA Chao, et al. Hydrochemical and Isotopic Characteristics and Water Assessment Analysis of Surface Water and Groundwater Near Bolokenu–Aqikekuduke Fault in Xinjiang[J]. Northwestern Geology, 2023, 56(6): 186-197. DOI: 10.12401/j.nwg.2023009

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Hydrochemical and Isotopic Characteristics and Water Assessment Analysis of Surface Water and Groundwater Near Bolokenu–Aqikekuduke Fault in Xinjiang

YANG Mingyuan^1,,
ZHAO Jiayi^{2, 3, ,},
MA Chao¹,
LI Xin¹

1.
The Second Regional Geological Survey Group, Xinjiang Bureau of Geology and Mineral Resources, Changji 831100, Xinjiang, China
2.
The Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, Hebei, China
3.
Technology Innovation Center of Geothermal & Hot Dry Rock Exploration and Development, Ministry of Natural Resources,Zhengding 050800, Hebei, China

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Received Date: June 16, 2022
Revised Date: October 08, 2022
Accepted Date: February 09, 2023
Available Online: February 14, 2023

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Abstract

Abstract

Xinjiang is an arid area in Northwest China, which is short of water resources. In order to study the hydrogeochemical characteristics and water quality of its groundwater, 15 samples including hot spring water, surface water and cold spring water were collected near the Boa fault. The hydrochemistry and hydrogen and oxygen isotope characteristics were analyzed, and the water quality was evaluated. The results show that the hydrochemical types of surface water in the study area are mainly SO₄−Na, Cl·SO₄−Na and HCO₃·SO₄−Ca·Na type. The hydrochemical types of hot spring water are SO₄·HCO₃−Na/HCO₃·SO₄−Na and HCO₃·Cl−Na type. The hydrochemical types of cold spring water are SO₄·HCO₃−Mg·Ca, HCO₃−Ca, HCO₃−Mg·Ca and SO₄·HCO₃−Ca type. The main sources of Mg²⁺, Ca²⁺, HCO₃⁻ in the cold spring water in the study area are dolomite, calcite and gypsum dissolution. Na⁺, K⁺, HCO₃⁻ and Ca²⁺ in hot spring water mainly come from the dissolution of feldspar minerals. The main ion sources in surface water are complex, and their contents are strongly affected by evaporation, and the surface water is in an oxidizing environment. The main supply source of hot spring water and cold spring water is atmospheric precipitation, and the supply elevation varies from 2874.5 m to 4287 m. The water quality of hot spring water and surface water is very poor, which is not suitable for drinking. The study of hydrochemical and isotopic characteristics of surface water and groundwater near Boa fault can provide theoretical support for the rational development, utilization and management of local water resources.
- hydrochemistry,
- hydrogen and oxygen isotopes,
- water quality analysis,
- Bolokenu−Aqikekuduke fault

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Hydrochemical and Isotopic Characteristics and Water Assessment Analysis of Surface Water and Groundwater Near Bolokenu–Aqikekuduke Fault in Xinjiang