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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Long-term stability of dithionite in alkaline anaerobic aqueous solution
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Long-term stability of dithionite in alkaline anaerobic aqueous solution

机译:碱性厌氧水溶液中二硫代钛矿的长期稳定性

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Closed-system experiments were conducted to investigate the decomposition of sodium dithionite in aqueous solutions under varying pH and starting concentrations to simulate the deployment of dithionite as an in-situ redox barrier. Co-determination of dithionite and its degradation products was conducted using UV-Vis spectrometry, iodometric titration, and ion chromatography. In unbuffered solutions, dithionite reacted rapidly, whereas in near-neutral solutions (pH similar to 7), it persisted for similar to 50 days and in alkaline solution (pH similar to 9.5) for > 100 days. These are the longest lifetimes reported to date, which we attribute to not only excluding oxygen but also preventing outgassing of H2S. Thoroughly constraining the reaction products has led to the following hypothesized reaction:
机译:进行闭合系统实验,以研究在不同pH和开始浓度下的水溶液中的二硫代钠的分解,以模拟二硫代钛矿作为原位氧化还原屏障的展开。 使用UV-Vis光谱法,碘量滴定和离子色谱法进行二硫代酮及其降解产物的共测。 在无缓冲的溶液中,DITHIONITE在近中性溶液(pH类似于7)的情况下,它持续到50天和碱性溶液(pH类似于9.5)的溶液中> 100天。 这些是迄今为止报告的最长的寿命,不仅是排除氧气的归因,而且防止了H2S的偏差。 彻底限制反应产物已导致以下假设反应:

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