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November 2003

Local resident struggling through mud deposited near Lang Lang Jetty (western Port Bay, Victoria). Photo: Peter Wallbrink
Murky Secrets Revealed

Draining the Koo Wee Rup Swamp seemed like a good idea at the time. They cut down the trees and made drains across the swamp to reclaim fertile land for market gardens to supply nearby Melbourne.

But that was in the 1890s and today, soil erosion from those drains and more recently-formed erosion gullies seems the likely cause of changes in Western Port Bay. Mud, for example, now occupies large areas that were previously inhabited by ecologically important seagrass meadows – areas that have suffered serious decline over the last 30 years.

‘Time, winds, tides – and the resulting sediment transport wait for no-one’, says Dr Peter Wallbrink, CSIRO Land and Water. ‘Over the last century, and particularly in the last 25 years, a significant amount of mud from the drainage channels has been distributed, in a clockwise fashion, around French island within the bay.’

‘But before we can begin to set priorities for rehabilitation, we need to understand sediment movement processes – where is the sediment coming from within the catchment, where is it accumulating and how is it moving within the waters of the bay?’

In search of the answers, a team of nine scientists from CSIRO Land and Water undertook a three-year study in conjunction with Melbourne Water Corporation and the Victorian Environment Protection Authority (EPA). And they deployed a whole swag of scientific techniques (see ‘The Science behind the Western Port Bay Sediment Study’ page 2).

These techniques, together with landscape based mathematical models and the researchers’ own knowledge of sediment and nutrient transport processes, allowed the team to describe the sources, accumulation and redistribution of sediment in the bay.

‘Armed with this knowledge, we were able to suggest priorities for action plans – both short and long term – for each of the major sediment sources: Bunyip and Lang Lang rivers, north-eastern shorelines, drainage channels and gullies’, says Dr Wallbrink. ‘If acted upon, these will reduce the sediment and nutrients entering Western Port Bay.’

‘In the short term, stabilisation of the river and gully banks would be an effective option.’

‘In the long term, we recommended re-establishment of shoreline mangroves if appropriate, reconnection of channels to floodplains and re-establishment of riparian vegetation along the streams and river corridors.’

Now it is up to the residents of Western Port Bay, and the catchment and water authorities involved, to decide how to balance the use of the Western Port catchment for agriculture against its impact on the bay.

More on the science of the Western Port Bay Sediment Study.

Reports on this study are available on the CSIRO Land and Water website.
CSIRO contact:

Dr Peter Wallbrink
Ph: +61-2-6246 5823