Isotopic and geochemical evidence of recharge sources and water quality in the Quaternary aquifer beneath Jinchang city, NW China
Authors:
- Jinzhu MaJMJinzhu Ma
- Tianming HuangTianming Huang
- 1 July 2010
- journal article
- Published by Elsevier in Applied Geochemistry
- Vol. 25 (7) , 996-1007
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Limits to recharge of groundwater from Tibetan plateau to the Gobi desert, implications for water management in the mountain frontJournal of Hydrology, 2009
- Conceptual model of recharge to southeastern Badain Jaran Desert groundwater and lakes from environmental tracersApplied Geochemistry, 2008
- Groundwater recharge history and hydrogeochemical evolution in the Minqin Basin, North West ChinaApplied Geochemistry, 2006
- The characteristics of ground-water resources and their changes under the impacts of human activity in the arid Northwest China—a case study of the Shiyang River BasinJournal of Arid Environments, 2005
- Groundwater recharge in a sedimentary basin in semi-arid MexicoHydrogeology Journal, 2004
- Hydrogeochemical processes in shallow quaternary aquifers from the northern part of the Datong Basin, ChinaApplied Geochemistry, 2004
- Changes in Lena River streamflow hydrology: Human impacts versus natural variationsWater Resources Research, 2003
- Paleoclimatic interpretation of the past 30 ka from isotopic studies of the deep confined aquifer of the North China plainApplied Geochemistry, 2003
- Groundwater evolution in the Continental Intercalaire aquifer of southern Algeria and Tunisia: trace element and isotopic indicatorsApplied Geochemistry, 2003
- Water salinization in arid regions—observations from the Negev desert, IsraelJournal of Hydrology, 1997