State of the Environment

2001

Inland Waters Theme Report

Australia State of the Environment Report 2001 (Theme Report)
Prepared by: Jonas Ball, Sinclair Knight Merz Pty Limited, Authors
Published by CSIRO on behalf of the Department of the Environment and Heritage, 2001
ISBN 0 643 06750 7

Water quality and sources of pollution

This section reports on the following environmentals, which are defined in Fairweather and Napier (1998):

Environmental Indicator
IW 2.1 Human criteria exceedances
IW 2.3 Wastewater treatment
IW 3.1 Guideline trigger levels reached
IW 3.2 Algal blooms
IW 3.3 | a | b | c | Nutrient loads
IW 3.5 | a | b | c | Pesticide exposure
IW 3.6 | a | b | c | d | Pollution point sources
IW 3.7 Minesite remediation
IW 3.8 Bloom contingency plans
IW 3.9 Polluter pays principle
IW 3.11 Waterwatch participation
IW 3.13 Instream salinity trends

Australia has limited inland surface water and groundwater resources suitable for human uses, so the protection of the quality of these waters is important. Equally important is protecting water quality to ensure that the health of Australia's inland aquatic ecosystems and endemic flora and fauna is protected. The major water quality threats to human uses of water and the health of aquatic ecosystems are: increasing instream salinity and land salinisation; siltation, nutrient enrichment and algal blooms; increasing water acidity; and pollutants such as metals and pesticides.

Salinity of surface waters

The increasing salinity of soils and inland waters is a major threat to the health of terrestrial and aquatic ecosystems and water resources in many catchments. The impacts on inland waters from increasing land and instream salinity include:

The major cause of land and water salinisation in Australia is dryland salinity, and the area of land affected is predicted to triple in size over the next fifty years. Secondary salinisation can be caused by over-irrigation; however, its effects are often localised and can be more easily managed.

It should be noted that certain Australian waters have relatively high levels of salt as a result of natural influences. For example, the western zone of the Murray and many parts of south-west Western Australia are underlain by sediments of marine origin, which yield regionally saline groundwaters. Groundwater inflow into rivers, streams and wetlands in these areas provides most of the baseflow so many of these inland waters are naturally brackish or saline.