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• W2045384345 abstract "A study of water and salt balances within a first-order catchment in the Western Australian wheatbelt has shown that the salt load in the main surface drainage comes largely from groundwater discharging upstream from the basement highs and dykes that extend across the surface drainage and conductive channels within the regolith. Although salt fall from rainfall is about 2.0 g m−2 year−1 (Cl−), the stream load ranges from 180 to 850 g m−2 year−1 with an out/input ratio of 100–425. Salt storage in the catchment varies from 900–4000 g m−2 in the top 3 m, to 27 000–71 000 g m−2 in the 3–15 m depth range and 5000–21 000 g m−2 below 15 m. Groundwater discharge calculated using Br and Cl as tracers for the groundwater component fluctuates between 20 and 40% of streamflow. Stream salinity during the last 3 years was below the long-term average. This is attributed to a reduction in groundwater discharge caused by low rainfall during this period. The downward displacement and leaching of salt stored in the regolith indicates that if groundwater levels continue to rise, the quantity and salinity of groundwater discharge will continue to increase causing further rises in stream salinity." @default.
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• W2045384345 date "1993-05-01" @default.
• W2045384345 modified "2023-09-23" @default.
• W2045384345 title "Salinity trends in the wheatbelt of Western Australia: results of water and salt balance studies from Cuballing catchment" @default.
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• W2045384345 doi "https://doi.org/10.1016/0022-1694(93)90219-y" @default.
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