ArticleScientific reports2021
Hydrochemical analysis and identification of open-pit mine water sources: a case study from the Dagushan iron mine in Northeast China.
Article in Scientific reports, 2021. 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, 17 citations in OpenAlex.
- Identification of water sources of mine water bursts based on the FPS-DT model.Scientific reports · 2025Article
- Research on an identification model for mine water inrush sources based on the HBA-CatBoost algorithm.Scientific reports · 2024Article
- Experimental study on comprehensive detection technology of shallow gas in deep soft soil layer.Heliyon · 2024Article
- Identification of origin and runoff of karst groundwater in the glacial lake area of the Jinsha River fault zone, China.Scientific reports · 2022Article
- Changes in Reconstructed Soil Physicochemical Properties in an Opencast Mine Dump in the Loess Plateau Area of China.International journal of environmental research and public health · 2022Article
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Authors and funding
7 authors at 2 institutions in 1 country.
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Abstract
The identification of open-pit mine water sources is of great significance in preventing water disasters. Combined with hydrochemistry and multivariate statistical analysis, this paper systematically analyzed the hydraulic connections between aquifers and the complex seepage water sources in the pit and roadway of Dagushan iron mine through qualitative analysis and quantitative calculation. According to the hydrochemical characteristics of the study area, the causes of seepage water at different positions in the mining area were reasonably explained. The results show that there is a possible hydraulic connection or similar source of water body between the bedrock fissure aquifer and the eluvium pore aquifer. The water seepage of 2# roadway mainly comes from bedrock fissure aquifer in the north of mining area. The reason for serious water seepage in the 3# roadway and the western side of the pit is that the fault connects the shallow alluvial pore aquifer and bedrock fissure aquifer. The source of water on the southern side pit comes from the river and groundwater on the southern side of the mine. The results presented here provide significant guidance for the management of mine water seepage problems.
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