ArticleEnvironmental science and pollution research international2022
Insight into the water-rock interaction process and purification mechanism of mine water in underground reservoir of Daliuta coal mine in China.
Article in Environmental science and pollution research international, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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5 citing papers in PubMed, 34 citations in OpenAlex.
- Water-Rock Interaction Mechanisms and Hydrochemical Evolution in the Underground Reservoirs of Coal Mines.ACS omega · 2024Article
- Water Quality Characteristics and Water-Rock Interaction Mechanisms of Coal Mine Underground Reservoirs.ACS omega · 2024Article
- The construction of mine water recycling performance evaluation index system under the Internet of Things environment.Scientific reports · 2023Article
- Research on Temporal Patterns of Water-Rock Interaction in the Coal Mine Underground Reservoir Based on the Dynamic Simulation Test.ACS omega · 2023Article
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5 authors at 1 institution in 1 country.
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Abstract
The water quality of mine water is obviously improved after being stored in underground reservoir, but the process of water-rock interaction and the purification mechanism of mine water quality are not clear. In this study, the water samples and rock samples collected in the underground reservoir of Daliuta coal mine were taken as the research object. Based on the analysis of the hydrochemical characteristics of the reservoir water samples and the characterization of the rock samples, combined with PHREEQC analysis, the mechanism of water quality purification of mine water was discussed. The results showed that the rocks in the underground reservoir had layered silicate structure and flaky kaolinite structure, with some irregular edges and microcracks, and higher specific surface area and total pore volume. These characteristics made the rocks have a certain adsorption and removal capacity for heavy metal ions and other pollutants in the mine water. The water-rock interaction, such as the dissolution of albite and halite, the precipitation of gypsum and kaolinite, and the cation exchange, resulted in the increase of the concentration of Na
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