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Analysis on the Causes for Arsenic Enrichment of Deep Groundwater in Costal Tangshan

机译:昂首石唐山深层地下水的原因分析

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In some coastal area of Tangshan,38.5% of the water samples of As from deep groundwater exceed the limit of Quality standard for ground water,10ug/L, and excessive water samples mainly from continued pumping water wells of living water. Continued field pumping water for As testing, we found that arsenic concentrations continued to rise as the pumping time, steady about 24 hours later and declined gradually after the pumping stopped. By the hypothetic-deductive method, we rule out the possibility of man-made pollution. By means of correlation analysis, principal component analysis and other means identify the connection of arsenic and carbonic acid balance,as well as Fe,and draw on previous results properly verified by experiments this time for the analysis. Finally we found dynamic changes concentrations of arsenic caused by the pumping of the deep groundwater,resulting in the rise on Eh in wells which lead to the transform between Fe (OH)_2 and Fe (OH)_3.The differences of their adsorption capacity may be the significant factor accounting for the dynamic changes of arsenic concentration in the relatively open groundwater system.
机译:在唐山的一些沿海地区,从深层地下水作为水样的38.5%,超过质量标准为地下水,为10ug / L,并且主要来自生活用水的持续抽水井过多的水样的限制。续场抽水作为测试,我们发现,砷的浓度后继续上涨的泵送时间,稳定约24小时并逐渐下降泵送停止后。通过假设的演绎方法,我们排除了人为污染的可能性。通过相关性分析的方法,主成分分析等手段鉴定砷和碳酸平衡的连接,以及Fe和吸取通过实验此时为分析正确验证以前的结果。最后,我们发现动态改变所引起的深层地下水的泵送砷的浓度,导致在Eh值上升孔而导致的Fe之间的变换(OH)_2和Fe(OH)的它们的吸附容量_3.The差异可能是占砷浓度在相对开放的地下水系统的动态变化显著因素。

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