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Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield
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Yan-na LI1, 2, Lei HUANG1, 2, *, Jun-li GAN3, Xuan HAN1, 2, Jiang XU1, 2, Meng-fan YANG1, 2, Guang-yan ZHU1, 2
China Environmental Science | 2025, 45(8) : 4538 - 4550
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China Environmental Science | 2025, 45(8): 4538-4550
• Environmental Ecology •
Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield
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Yan-na LI1, 2, Lei HUANG1, 2, *, Jun-li GAN3, Xuan HAN1, 2, Jiang XU1, 2, Meng-fan YANG1, 2, Guang-yan ZHU1, 2
Affiliations
  • 1.State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Inner Mongolia Agricultural University, Autonomous Region Collaborative Innovation Center for Integrated Management of Water Resources and Water Environment in the Inner Mongolia Reaches of the Yellow River, Hohhot 010018, China
  • 2.Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Inner Mongolia Key Laboratory of Ecohydrology and High Efficient Utilization of Water Resources, Hohhot 010018, China
  • 3.Zhungeer Banner Water Conservancy Development Center, Ordos 010321, China
Published: 2025-08-20
Outline
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To explore the hydrochemical characteristics and hydraulic connections of different aquifers in the northern mining area of the Zhungeer Coalfield, and to reveal the regional water circulation patterns under coal mining activities, a total of 39water samples were collected from different aquifers in the mining area. The hydrochemical characteristics, controlling factors, and hydraulic connection degrees were analyzed using methods such as Piper trilinear diagrams, Gibbs diagrams, ion ratio analysis, chloride-alkalinity index, factor analysis, and connectivity index. The results show that the water in the mining area is generally weakly alkaline. The main hydrochemical type of the Quaternary and Shiqianfeng Formation aquifers is HCO--Ca type water, which is mainly influenced by silicate weathering and mining activities, with positive cation exchange occurring. The main hydrochemical type of the Zhidan Group aquifer is HCO3-Ca type water, followed by HCO3-Na and Cl-Ca types. Its sources are mainly influenced by the weathering dissolution of silicate rock minerals and the impacts of mining and agricultural activities, with positive cation exchange occurring. The main hydrochemical type of mine water is Cl-Ca type water, which is influenced by the weathering dissolution of silicate and evaporite minerals and mining activities, with reverse cation exchange occurring. The hydraulic connectivity indices between the Quaternary aquifer and the Zhidan Formation, and between the Zhidan Formation aquifer and the Shiqianfeng Formation are 27% and 20%, respectively, indicating the presence of hydraulic connections. The hydraulic connectivity index between the Shiqianfeng Formation aquifer and the mine water is 39%, indicating a weak hydraulic connection.

aquifer  /  hydrochemical characteristics  /  hydroaction  /  hydrogen and oxygen stable isotopes  /  hydraulic connection
李艳娜, 黄磊, 甘俊礼, 韩萱, 许江, 杨梦凡, 朱廣岩. 准格尔煤田北部矿区含水层水文地球化学特征及水力联系辨识. 中国环境科学, 2025 , 45 (8) : 4538 -4550 .
Yan-na LI, Lei HUANG, Jun-li GAN, Xuan HAN, Jiang XU, Meng-fan YANG, Guang-yan ZHU. Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield[J]. China Environmental Science, 2025 , 45 (8) : 4538 -4550 .
Year 2025 volume 45 Issue 8
79
13
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Article Info
  • Receive Date:2025-01-02
  • Online Date:2026-10-08
  • Published:2025-08-20
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  • Received:2025-01-02
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Affiliations
    1.State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Inner Mongolia Agricultural University, Autonomous Region Collaborative Innovation Center for Integrated Management of Water Resources and Water Environment in the Inner Mongolia Reaches of the Yellow River, Hohhot 010018, China
    2.Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Inner Mongolia Key Laboratory of Ecohydrology and High Efficient Utilization of Water Resources, Hohhot 010018, China
    3.Zhungeer Banner Water Conservancy Development Center, Ordos 010321, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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