用户名: 密码: 验证码:
Chromium Isotope Fractionation During Reduction of Cr(VI) Under Saturated Flow Conditions
详细信息    查看全文
文摘
Chromium isotopes are potentially useful indicators of Cr(VI) reduction reactions in groundwater flow systems; however, the influence of transport on Cr isotope fractionation has not been fully examined. Laboratory batch and column experiments were conducted to evaluate isotopic fractionation of Cr during Cr(VI) reduction under both static and controlled flow conditions. Organic carbon was used to reduce Cr(VI) in simulated groundwater containing 20 mg L鈥? Cr(VI) in both batch and column experiments. Isotope measurements were performed on dissolved Cr on samples from the batch experiments, and on effluent and profile samples from the column experiment. Analysis of the residual solid-phase materials by scanning electron microscopy (SEM) and by X-ray absorption near edge structure (XANES) spectroscopy confirmed association of Cr(III) with organic carbon in the column solids. Decreases in dissolved Cr(VI) concentrations were coupled with increases in 未53Cr, indicating that Cr isotope enrichment occurred during reduction of Cr(VI). The 未53Cr data from the column experiment was fit by linear regression yielding a fractionation factor (伪) of 0.9979, whereas the batch experiments exhibited Rayleigh-type isotope fractionation (伪 = 0.9965). The linear characteristic of the column 未53Cr data may reflect the contribution of transport on Cr isotope fractionation.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700