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首页> 外文期刊>Science of the total environment >Study on the groundwater quality and its influencing factor in Songyuan City,Northeast China,using integrated hydrogeochemical method
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Study on the groundwater quality and its influencing factor in Songyuan City,Northeast China,using integrated hydrogeochemical method

机译:地下水质量及其影响因素在中国东北部宋元市,采用综合水力造物理方法研究

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Clean groundwater resources are important for the health of human.In Songyuan City,Northeast China,anthropogenic activities have led to changes in groundwater circulation,thereby depleting the aquifer system and causing water quality deterioration.To evaluate the genesis of water quality,we analyzed the hydrochemical and stable isotope compositions of shallow and deep groundwater.According to drinking water quality standards,the concentrations of Ca~(2+),Mg~(2+),and NO_3~-in 23.0,30.2 and 35.4% of the samples,respectively,exceeded the acceptable ranges.The groundwater chemistry in these samples was related to geochemical processes and agricultural pollution.The hydrochemical analysis explained the reaction mechanisms in each aquifer,showing that the main source of ions in both deep and shallow groundwater is the weathering of silicate rock.In addition,the dissolution of carbonate minerals and artificial pollutants is greater in the shallow groundwater.The stable isotope results showed that long-term extraction is the cause of the diffusion of pollutants in shallow aquifers.Moreover,because most of the well-drilling techniques are backward,the aquifer structure is destroyed,and the deep groundwater is mixed with the shallow groundwater during the process of artificial extraction.The study also analyzed the conditions of the water-rock reaction.Combined with the geological background,it was found that the deep CO_2 gas reservoir could provide the necessary material source for the reactions.Owing to frequent tectonic activities,deep CO_2 could be discharged to the surface through the fault zone,which promotes the water-rock reaction in this area.
机译:清洁地下水资源对于人类的健康很重要。在中国东北地区松原市,人为活动导致地下水循环发生变化,从而耗尽含水层系统并导致水质恶化。评估水质的成因,我们分析了浅层和深层地下水的水化学和稳定同位素组成。根据饮用水质量标准,Ca〜(2 +),mg〜(2 +)和NO_3〜-in 23.0,30.2和35.4%的样品的浓度,分别超过可接受的范围。这些样品中的地下水化学与地球化学方法和农业污染有关。水化学分析解释了每种含水层中的反应机制,表明深层和浅地下水中的离子主要来源是风化硅酸盐岩。此外,碳酸盐矿物和人工污染物的溶解在浅地下水中更大。稳定的同位素结果显示长期提取是污染物在浅层含水层中扩散的原因。由于大多数钻井技术都是向后的,含水层结构被破坏,并且在过程中,深层地下水与浅地下水混合在一起人工提取。该研究还分析了与地质背景中的水岩反应的条件,发现深Co_2气体储层可以为反应提供必要的材料来源。常急的构造活动,深度CO_2可以通过断层区域排出到表面,促进该区域的水岩反应。

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