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• W2920455956 abstract "This study assesses the hydrochemical characteristics and water quality for irrigation use around the Hard Rock Mining area. The Hydrochemical analysis shows that there are wide variations of ions (e.g. pH, Sp. EC, turbidity, Fe3+, Na+, Cl−, Cd2+, soluble silica and others) which exceeded the acceptable limit of drinking as well as the irrigation uses. The concentration of SiO2 in the water is very high than the natural limit. It indicates a direct impact of granitic rock extracted from the mine. In fact, such rock contains a large quantity (50.17%–74.7% by weight) of silica. The WQI analysis shows that water samples are slightly marginal to excellent quality water. Where, the surface water samples possess comparatively good quality water than groundwater for irrigation purpose. The scatter graph of (Ca2+ + Mg2+) versus total cations (TZ+) plot suggests that some ions are produced due to the weathering of silicate minerals. The Trilinear diagram exhibits that 77.24% of samples are showing the CaHCO3 type of facies where 85.7% of surface water falls within this category. The Durov diagram illustrates the mixing of ion dissolution with reverse ion exchanging water type. The correlation matrix affirms the relationship, strength, and direction of multivariate data. In particular, the various classification of water such as SAR, Na%, salinity, and TDS values confirmed excellent to permissible use of water for agricultural purpose around the mining area." @default.
• W2920455956 created "2019-03-11" @default.
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• W2920455956 date "2019-04-01" @default.
• W2920455956 modified "2023-09-23" @default.
• W2920455956 title "Understanding the hydrogeochemical characteristics of natural water for irrigation use around the hard rock mine in Maddhapara, Northwest Bangladesh" @default.
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• W2920455956 doi "https://doi.org/10.1016/j.gsd.2019.02.007" @default.
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