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- W1963630614 abstract "A simple groundwater recharge-depletion model is presented for the Magela Creek catchment. Recharge is through infiltration of rain water while depletion is through evapotranspiration and aquifer discharge. The model was applied to the phreatic aquifer near Magela Creek, downstream from the Ranger uranium mine site, and was able to match the seasonal variation of the water table, about its mean head, over 4 years within a maximum error of 30% (corresponding to about 1 m). The model computations indicate that the dominant depletion process is evapotranspiration rather than aquifer discharge. The model can be used to define the far-field groundwater boundary conditions in models for groundwater seepage from the mine water impoundments." @default.
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- W1963630614 date "1993-08-01" @default.
- W1963630614 modified "2023-10-16" @default.
- W1963630614 title "A simple groundwater recharge-depletion model for the tropical Magela Creek catchment" @default.
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- W1963630614 doi "https://doi.org/10.1016/0304-3800(93)90014-j" @default.
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