Origin of dissolved salts in a large, semi-arid groundwater system: MurrayBasin, Australia

Hypotheses to explain the source of the 10(11) tons of salt in groundwaters of the Murray Basin, southeastern Australia, are evaluated; these are (a) mixing with original sea water, (b) dissolution of salt deposits, (c) weath ering of aquifer minerals and (d) acquisition of solutes via rainfall. The total salinity and chemistry of many groundwater samples are similar to sea -water composition. However, their stable isotopic compositions (delta O-18 = -6.5 parts per thousand; delta H-2 = -35) are typical of mean winter rain fall, indicating that all the original sea water has been flushed out of th e aquifer. Br/Cl mass ratios are approximately the same as sea water (3.57 x 10(-3)) indicating that NaCl evaporites (which have Br/Cl<10(-4)) are not a significant contributor to Cl in the groundwater. Similarly, very low ab undances of Cl in aquifer minerals preclude rock weathering as a significan t source of Cl. About 1.5 million tons of new salt is deposited in the Murr ay-Darling Basin each year by rainfall. The groundwater chemistry has evolv ed by a combination of atmospheric fallout of marine and continentally deri ved solutes and removal of water by evapo-transpiration over tens of thousa nds of years of relative aridity. Carbonate dissolution/precipitation, cati on exchange and reconstitution of secondary clay minerals in the aquifers r esults in a groundwater chemistry that retains a 'sea-water-like' character .