在通过硫化进行非生物降解期间的化物稳定同位素分离过程中使用化
Heather K Shrimpton1, Carol J Ptacek1, David W Blowes1
1University of Waterloo, 200 University Ave West, Waterloo, Ontario N2L 3G1, Canada.
Environmental science & technology
|July 16, 2024
概括
研究了 (IV) 通过硫化 (H2S(g)) 的生物降解. 这一过程对于从地下水中去除很重要,它显示出明显的同位素分离,取决于硫与的比率.
科学领域:
- 环境化学环境化学
- 地质化学 地质化学
- 生物地质化学生物地质化学
背景情况:
- 减少硫的细菌 (SRB) 有助于从地下水中去除.
- 的去除通过直接呼吸或硫化 (H2S(g)) 介导的非生物降解发生.
- 了解非生物降解对于区分微生物和非微生物循环至关重要.
研究的目的:
- 通过H2S(g)对 (IV) 在非生物降解过程中的同位素分离进行研究.
- 为了比较无生物分化与微生物减少过程.
- 为了确定非生物和微生物降解是否可以根据同位素特征进行区分.
主要方法:
- 增加硫化 (Na2S) 的度被添加到 (IV) 溶液 (SeO2-) 中,以诱导减少和沉.
- 使用粉末X射线衍射 (PXRD) 分析沉物,以确定矿物相.
- 在残留溶解的中测量了同位素比率 (δ82Se).
主要成果:
- 观察到三种不同的颜色沉物:色 (SeS8-),红色 (Se(0) 和黄色 (S(0).
- 随着水性的度下降,残留溶解的Se值增加.
- 溶液中硫与的比率受同位素分离的影响,较高的比率产生较低的分离率.
结论:
- 通过H2S(g)对 (IV) 的非生物降解,导致显著的同位素分离.
- 观察到的分化取决于溶液中的S/Se比率.
- 通过分析同位素分离模式,可以区分非生物和微生物减少.
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