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Hydrogeochemical characteristics of surface water and groundwater in areas underlain by black shales and slates of the Okchon zone, Korea

机译:韩国Okchon区黑色页岩和板岩覆盖地区的地表水和地下水的水文地球化学特征

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The purpose of this study is to investigate the hydrogeochemical characteristics and the potential contamination of surface water and groundwater in areas underlain by black shales and other metasedi-mentary rocks in the Okchon zone, Korea. Surface water and groundwater samples were collected from the Duk-Pyung, Chu-Bu, Bo-Eun, I-Won and Geum-Kwan areas of the Okchon zone, and the in-situ measurement and chemical analysis of dissolved constituents were performed. All water samples have Ca~(2+)-HCO_(3~-) and Ca~(2+)-(Cl~--SO_(4~(2-))) compositions due to the dissolution of calcite and Mg-carbonates and the oxidative dissolution of sulfide minerals from black shale and slates. The increase of concentrations of Ca~(2+), Mg~(2+), HCO_(3~-), Na~+ and SiO_2 from surface water to groundwater indicates progressive water-rock interaction as supported by hydrogeochemical modeling and phase stabilities of related minerals. High concentrations of K~+, Cl~- and NO_(3~-) are also found in groundwater due to the inflow of external contaminants. From the results of statistical analysis, it could be concluded that the factors controlling the hydrogeochemical characteristics of surface water and groundwater are the inflow of external contaminants, the dissolution of carbonates, the weathering of silicates and the oxidation of sulfides.
机译:这项研究的目的是调查韩国Okchon地区黑色页岩和其他准沉积岩层下的地区的水文地球化学特征以及地表水和地下水的潜在污染。从Okchon区的Duk-Pyung,Chu-Bu,Bo-Eun,I-Won和Geum-Kwan地区收集了地表水和地下水样品,并进行了溶解成分的现场测量和化学分析。由于方解石和Mg-的溶解,所有水样均具有Ca〜(2 +)-HCO_(3〜-)和Ca〜(2 +)-(Cl〜--SO_(4〜(2-)))组成。碳酸盐和硫化物矿物从黑页岩和板岩的氧化溶解。从地表水到地下水,Ca〜(2 +),Mg〜(2 +),HCO_(3〜-),Na〜+和SiO_2的浓度增加表明水-岩石相互作用是由水地球化学模型和相稳定性支持的相关矿物质。由于外部污染物的流入,地下水中还发现了高浓度的K〜+,Cl〜-和NO_(3〜-)。从统计分析结果可以得出结论,控制地表水和地下水的水文地球化学特征的因素是外部污染物的流入,碳酸盐的溶解,硅酸盐的风化和硫化物的氧化。

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