Preliminary groundwater and salinity investigation in the eastern wheatbelt. 1. Brennand's Catchment
Groundwaters were found to be 10 m below the floor of the ancestral playa lake in Brennand's catchment. They were extremely saline. A groundwater flow system was not established on much of the catchment. Flow was observed to be occurring from recharge areas near the playa lakes towards the midslopes of the catchment. Flow was apparently restricted from leaving Brennand's catchment because of obstruction to groundwaters created by dolerite dykes.
Groundwater recharge, Brennand's Catchment (WA), Western Australia, Groundwater, Catchment hydrology, Saline water
George, R J, and Frantom, P W. (1990), Preliminary groundwater and salinity investigation in the eastern wheatbelt. 1. Brennand's Catchment. Department of Primary Industries and Regional Development, Western Australia, Perth. Report 88.
Maps are not included as part of the complete document download. If this report contains a map, it will be available in the Individual Parts list below.