Effects of Increasing Acidity on Metal(loid) Bioprecipitation in Groundwater: Column Studies
详细信息    查看全文
文摘
Large-scale column experiments were carried out over aperiod of 545 days to assess the effect of increasing acidityon bacterial denitrification, sulfate reduction, and metal(loid) bioprecipitation in groundwater affected by acid minedrainage. At a groundwater pH of 5.5, denitrification andCu2+ removal, probably via malachite (Cu2(OH)2CO3)precipitation, were observed in the ethanol-amendedcolumn. Sulfate reduction, sulfide production, and Zn2+removal were also observed, with Zn2+ removal observedin the zone of sulfate reduction, indicating likely precipitationas sphalerite (ZnS). Se6+ removal was also observed in thesulfate reducing zone, probably as direct bioreduction toelemental selenium via ethanol/acetate oxidation or sulfideoxidation precipitating elemental sulfur. A step decreasein groundwater pH from 5.5 to 4.25 resulted in increaseddenitrification and sulfate reduction half-lives, migrationof both these redox zones along the ethanol-amended column,and the formation of an elevated Cu2+ plume. Additionally,an elevated Zn2+ plume formed in the previous sulfatereducing zone of the ethanol-amended column, suggestingdissolution of precipitated sphalerite as a result of thereduction in groundwater pH. As Cu2+ passed through thezone of sphalerite dissolution, SEM imaging and EDSdetection suggested that Cu2+ removal had occurred viachalcocite (Cu2S) or covellite (CuS) precipitation.

© 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