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Volumn 380, Issue 1-2, 2010, Pages 203-221

Physical hydrogeology and environmental isotopes to constrain the age, origins, and stability of a low-salinity groundwater lens formed by periodic river recharge: Murray Basin, Australia

Author keywords

Baseflow; Environmental isotopes; Groundwater; Recharge; Surface water

Indexed keywords

AQUITARDS; BASEFLOWS; CHANNEL SANDS; ENVIRONMENTAL ISOTOPES; FLOOD PLAINS; FLOWTHROUGH; GROUND WATER RECHARGE; HIGH FLOW; HYDRAULIC GRADIENTS; HYDRAULIC HEADS; HYDROGEOLOGICAL; LAND CLEARING; MIXING ZONES; MURRAY BASIN , AUSTRALIA; MURRAY RIVER; REGIONAL GROUNDWATER; RIVER LEVELS; RIVERINE ECOSYSTEMS; SALINE GROUNDWATER; SCALE TRANSITION; SHALLOW CHANNELS; TIME-SCALES; TOTAL DISSOLVED SOLIDS; VICTORIA , AUSTRALIA; WATER TABLES;

EID: 71849086053     PISSN: 00221694     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jhydrol.2009.11.001     Document Type: Article
Times cited : (58)

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