Hydrochemical processes in the Lower Murrumbidgee Area, NSW : the influence of weathering reactions, evaporation, and salt dissolution on groundwater quality
The Lower Murrumbidgee area is a major agricultural region located on the Eastern margin of the sedimentary Murray Basin. A large low-salinity groundwater body extends from the Eastern margin in the semi-confined Calivil and Renmark Formation aquifers, and is overlain by higher salinity water in the surficial Shepparton Formation. Deep groundwater extraction has increased to ~300 GL in last decade, leading to substantial pressure declines, and the resulting increased vertical hydraulic gradient...[Show more]
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