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- W2245898634 abstract "The Qualandary Crossing causeway dams the Salt River downstream from where it emerges from the broad 30-km long Yenyening Lakes system and immediately above its junction with the Avon River, 120 km from Perth. The crossing was constructed in the early 1900s and gradually increased in height, mostly to prevent the Avon River flooding back up the Salt River. The structure also retains saline water in the Qualandary Basin, the mostly deeper lakes at the lower end of the Yenyening Lakes, unless the drain-gates are opened. Stream and dryland salinity are now much greater issues than when the crossing first dammed the Salt River. There are both concerns that water held above the crossing might be affecting salinity and agricultural land upstream, and also awareness of the possibility that saline releases will affect the Avon River immediately downstream. As part of a review of the Salt River hydrology, the riverbed profile through the Yenyening Lakes and, especially across the Qualandary Basin, was drawn using GIS contouring of remotely sensed and surveyed levels. The elevation differences along this longitudinal profile are quite small but indicate the extent of water held by the Qualandary Crossing. Damming the Salt River at Qualandary Crossing retains water only within the Qualandary Basin and does not influence salt-affected land further upstream." @default.
- W2245898634 created "2016-06-24" @default.
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- W2245898634 date "2004-01-01" @default.
- W2245898634 modified "2023-09-26" @default.
- W2245898634 title "Is the Qualandary Crossing No Dam Good" @default.
- W2245898634 hasPublicationYear "2004" @default.
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