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The Influence of Bacterial Reduction on Concentrations of Sulphates in Deep Aquifers in River Drainage Basin

机译:细菌减少对流域深层含水层中硫酸盐浓度的影响

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Our study attempts to determine the influence of bacterial reduction on sulphate concentrations in groundwaters. A buried valley in a southeastern section of the Gwda River drainage basin was selected for fieldwork near the towns of Wysoka and Badecz. Deep aquifers in the area are known for their high sulphate concentrations that result from pyrite oxidation by the Thiobacillus denitrificans bacteria. Isotope compositions of SO_4~(2-) ions show ~(34)S enrichment at lower sulphate concentrations, which might indicate bacterial reduction processes. Theoretical curves of SO_4~(2-) isotope composition and ion concentration change, drawn using a Rayleigh formula and the results of the determination of δ~(lk)O (SO_4~(2-)) and δ~(34)S (SO_4~(2-)) suggest widely varying intensities of the sulphate reduction processes. It can be estimated that bacterial reduction eliminated between 30% and in excess of 50% of the initial concentrations of SO_4~(2-) ions in individual cases.
机译:我们的研究试图确定细菌减少对地下水中硫酸盐浓度的影响。格达河流域东南部的一个被埋没的山谷被选为Wysoka和Badecz城镇附近的野外作业。该地区的深层含水层因其高硫酸盐浓度而闻名,该浓度是由反硝化硫杆菌(Thiobacillus denitrificans)细菌氧化黄铁矿而产生的。 SO_4〜(2-)离子的同位素组成在较低的硫酸盐浓度下显示〜(34)S富集,这可能表明细菌的还原过程。利用瑞利公式绘制了SO_4〜(2-)同位素组成和离子浓度变化的理论曲线以及δ〜(lk)O(SO_4〜(2-))和δ〜(34)S的测定结果( SO_4〜(2-))表明硫酸盐还原过程的强度变化很大。可以估计,在个别情况下,细菌的减少消除了SO_4〜(2-)离子初始浓度的30%至超过50%。

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