Tuckean Swamp is a 6,000 hectare low-lying floodplain located on the Richmond River, which has been extensively drained since the 1880’s. By 1971, the existing drainage works were completed with the installation of the Bagotville Barrage, a large one-way flow control structures that excludes tidal exchange and prevents backwater flooding from the estuary. These drainage works altered the hydrology of the Tuckean Swamp floodplain, lowering the water table and exposing highly acidic soils to oxygen.

The ongoing drainage of the floodplain sees the regular discharge of highly acidic waters (pH < 3) with extremely high concentrations of iron and aluminium. Due to the very low-lying elevation of Tuckean Swamp, prolonged inundation following wet weather results in the generation of low dissolved oxygen ‘blackwater’ runoff. As a result, the impacts to the Richmond River estuary and wetland ecology itself has been significant.

Engineers at the Water Research Laboratory worked with landholde...

Tuckean Swamp drainage options study
The ongoing drainage of the floodplain sees the regular discharge of highly acidic waters (pH < 3) with extremely high concentrations of iron and aluminium.

For further information please contact:

Alice Harrison | Principal  Engineer | a.harrison@wrl.unsw.edu.au