Changing recharge pathways within an intensively pumped aquifer with high fluoride concentrations in Central Mexico.

导出 LinkOut

翻译打印收藏纠错

作者： Peter S K,Knappett ^[1] ; Yanmei,Li ^[2] ; Horacio,Hernandez ^[3] ; Rodrigo,Rodriguez ^[2] ; Manuel,Aviles ^[2] ; Chao,Deng ^[2] ; Viri,Piña ^[2] ; J Rick,Giardino ^[4] ; Jurgen,Mahlknecht ^[5] ; Saugata,Datta ^[6]

作者单位： Dept. Geology & Geophysics, Texas A&M University, College Station 77843, USA. Electronic address: knappett@tamu.edu. ^[1] Dept. Mines, Metallurgy and Geology Engineering, University of Guanajuato, 36000, Mexico. ^[2] Dept. Geomatic and Hydraulic Engineering, University of Guanajuato, 36000, Mexico. ^[3] Dept. Geology & Geophysics, Texas A&M University, College Station 77843, USA; Water Management and Hydrologic Sciences Graduate Program, Texas A&M University, College Station 77843, USA. ^[4] Centro del Agua para América Latina y el Caribe, Escuela de Ingenieria y Ciencias, Tecnologico de Monterrey, Monterrey 64849, Mexico. ^[5] Dept. Geology, Kansas State University, Manhattan 66506, USA. ^[6]

关键词 Cl/Br Fluoride Geothermal Groundwater Irrigation Stable isotopes

主题词氟化物(Fluorides);墨西哥(Mexico);水污染物, 化学性(Water Pollutants, Chemical)

DOI 10.1016/j.scitotenv.2017.12.031

PMID 29890573

发布时间 2018-06-21

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