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Discussion on Groundwater Genesis and Fault Water Source in Huibaoling Iron Mine Area
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Jun LI1, 2, Jikun BAI3, Yang SONG3, Dutao YU3, Shixiao ZUO3, Yanhong CHEN4, Shuangyuan HAN1, Ruxue BAI1
Mining Research and Development | 2025, 45(8) : 162 - 169
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Mining Research and Development | 2025, 45(8): 162-169
Discussion on Groundwater Genesis and Fault Water Source in Huibaoling Iron Mine Area
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Jun LI1, 2, Jikun BAI3, Yang SONG3, Dutao YU3, Shixiao ZUO3, Yanhong CHEN4, Shuangyuan HAN1, Ruxue BAI1
Affiliations
  • 1.Shandong Provincial Lunan Geo-engineering Exploration Institute (Shandong Provincial Bureau of Geology and Mineral Resources No.2 Geological Brigade), Jining, Shandong 272100, China
  • 2.Key Laboratory of Karst Geology, Shandong Geological and Mineral Exploration and Development Bureau, Jining, Shandong 272100, China
  • 3.Linyi Huibaoling Iron Mine Co., Ltd., Lanling County, Shandong 277700, China
  • 4.Shandong Geological and Mineral Construction Co., Ltd., Jining, Shandong 272100, China
Published: 2025-08-25
Outline
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In order to reveal the hydrochemical characteristics and genesis of groundwater under different buried depths in Huibaoling Iron Mine area, and analyze the recharge source of deep fault water, a total of 37 groundwater samples were collected from the fissure water of the Liguan Formation-Tongjiazhuang Formation, the karst fissure water of the Erqingshan Formation, the metamorphic rock fissure water and the fault water. The characteristics and genesises of groundwater hydrochemical components and the recharge source of fault water in this area were discussed by statistical analysis, Piper three-line diagram, Gibbs diagram and ion combination ratio method. The results show that the TDS of groundwater in each layer increases significantly with the increase of buried depth, and the dominant anions and cations gradually evolves from and Ca2+ to , Cl- and Na+. Because the hydrochemical components of each groundwater show obvious zoning in Piper three-line diagram and Gissb diagram, it can be seen that the hydraulic connection between each aquifer is poor. The formation of hydrochemical components of Liguan water and Erqingshan water is mainly controlled by rock weathering, and the ion components are mainly derived from the dissolution of carbonate, sulfate minerals and salt rocks. Metamorphic rock water is controlled by evaporation and concentration. Na+ and K+ are derived from the dissolution of silicate minerals and the alternating adsorption of cations. Ca2+, Mg2+, and are mainly derived from the dissolution of carbonate and sulfate and the oxidation of pyrite. The fault water is affected by both rock weathering and evaporation and concentration, and its main recharge sources are Liguan water and Erqingshan water, the prevention and control measures of water disaster should be put forward with emphasis on this source. The research results can provide reference for mine water disaster prevention and control.

Groundwater  /  Hydrochemical characteristic  /  Fault water  /  Water source analysis  /  Water disaster prevention and control
李军, 白继坤, 宋阳, 于杜涛, 左世晓, 陈艳红, 韩双元, 白茹雪. 会宝岭铁矿区地下水成因及断层水源探讨. 矿业研究与开发, 2025 , 45 (8) : 162 -169 .
Jun LI, Jikun BAI, Yang SONG, Dutao YU, Shixiao ZUO, Yanhong CHEN, Shuangyuan HAN, Ruxue BAI. Discussion on Groundwater Genesis and Fault Water Source in Huibaoling Iron Mine Area[J]. Mining Research and Development, 2025 , 45 (8) : 162 -169 .
Year 2025 volume 45 Issue 8
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  • Receive Date:2024-09-28
  • Online Date:2026-10-28
  • Published:2025-08-25
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  • Received:2024-09-28
Affiliations
    1.Shandong Provincial Lunan Geo-engineering Exploration Institute (Shandong Provincial Bureau of Geology and Mineral Resources No.2 Geological Brigade), Jining, Shandong 272100, China
    2.Key Laboratory of Karst Geology, Shandong Geological and Mineral Exploration and Development Bureau, Jining, Shandong 272100, China
    3.Linyi Huibaoling Iron Mine Co., Ltd., Lanling County, Shandong 277700, China
    4.Shandong Geological and Mineral Construction Co., Ltd., Jining, Shandong 272100, 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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