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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:韩国鄂东鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂鄂东区

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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的水文特征和地表水和地下水的地区潜在污染的黑色页岩和其他metasedi-mentary岩Okchon区,韩国伏。地表水和地下水样品从鸭-坪,储卜,博恩,I-元和Okchon区的今-关区域收集,并进行原位测量和溶解组分的化学分析。所有的水样本具有的Ca〜(2 +) - HCO_(3〜 - )和Ca〜(2 +) - (CL〜--SO_(4-(2-)))的组合物由于方解石和Mg的溶出碳酸盐和硫化物矿物的黑页岩和板岩氧化溶解。的Ca〜(2+),镁〜(2+),HCO_的浓度的升高(3〜 - ),钠〜+和SiO_2从地表水到地下水表示逐行水岩相互作用通过水文建模和相稳定性所支持相关的矿物质。高浓度的K +,氯〜的 - 和NO_(3〜 - )也以地下水由于外部污染物的流入找到。从统计分析的结果,可以得出结论的是控制地表水和地下水的水文特性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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