Natural Attenuation of Groundwater Uranium in Post-Neutral-Mining Sites Evidenced from Multiple Isotopes and Dissolved Organic Matter.

导出 LinkOut

翻译打印收藏纠错

作者： Chongsheng,Lu ^[1] ; Wei,Xiu ^[2] ; Bing,Yang ^[1] ; Haoyan,Zhang ^[2] ; Guoxi,Lian ^[3] ; Tianjing,Zhang ^[4] ; Erping,Bi ^[4] ; Huaming,Guo ^[4]

作者单位： State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences Beijing, Beijing 100083, China. ^[1] MOE Key Laboratory of Groundwater Circulation and Environment Evolution, School of Water Resources and Environment, China University of Geosciences (Beijing), Beijing 100083, China. ^[2] Institute of Earth Sciences, China University of Geosciences (Beijing), Beijing 100083, China. ^[3] The Fourth Research and Design Engineering Corporation of CNNC, Shijiazhuang 050021, China. ^[4]

关键词 Fe(III) reduction isotope labile organic matter natural attenuation rate sulfate reduction

主题词铀(Uranium);采矿(Mining);水污染物, 放射性(Water Pollutants, Radioactive);有机化学品(Organic Chemicals);同位素(Isotopes);生物降解, 环境(Biodegradation, Environmental);硫酸盐类(Sulfates)

DOI 10.1021/acs.est.4c04498

PMID 38965983

发布时间 2024-07-16

翻译满意度评价：

准确一般字义偏差语意偏离译文作用小提交