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• W293765341 abstract "The hydroperiod, filling frequency, local shallow groundwater movement and surface water and shallow groundwater chemistry of six small ( 211 days and filling frequency from 1 to 3 cycles over the study period, reflecting rainfall and sub-catchment variability. The playas are net discharge points for groundwater. However, small local vertical head variations suggest that groundwater does not discharge at the same rate across the playa surfaces and that playas may have short-lived recharge phases. Chemically, the playas are typical of salt lakes in Australia. Surface waters showed an ionic dominance consistent with seawater with minor variations attributed to transitional phases in the geochemical evolution of the waters. Shallow ground waters showed a common and consistent pattern of ionic dominance: Na+ > Mg2+ > K+ > Ca2+: Cl- > SO42- > HCO3- > CO32-. A geochemical pathway of brine evolution is proposed." @default.
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• W293765341 date "2007-01-01" @default.
• W293765341 modified "2023-09-26" @default.
• W293765341 title "The hydrology and hydrochemistry of six small playas in the Yarra Yarra drainage system of Western Australia" @default.
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