Erosion control

Last updated 25 Jun 2018 

The soil crust is made up of lichens, leaf litter and soil invertebrates that together protect the soil surface and increase its ability to absorb water. Erosion occurs when the soil crust and its cover of vegetation is damaged.

Damage from feral pigs on Yourka Reserve, Qld. Photo Paul Foreman.
Damage from feral pigs on Yourka Reserve, Qld. Photo Paul Foreman.
The poor placement or design of tracks, dams and infrastructure and the compaction of the soil, often caused by the action of hard-hooved animals, and vehicles are major causes of erosion. Once drainage lines change, water run off can impact new areas and also cause erosion issues.

We use a number of techniques to control erosion. They range from simple silt traps to major earthworks.

Simple silt traps can be created by filling erosion gullies with tree branches to slow the flow of water over the ground and catch waterborne soil particles and seeds. Leaves eventually drop off the branches also helping to trap seeds, soil and organic matter and over time the area begins to stabilise as the soil is held together and new plants establish.

Similarly simply cutting some bands into areas of compacted soil can help reduce water run off and allow sediment and water to pool, encouraging new plants to establish. 

Volunteers inspect an erosion gully at Nardoo Hills in Victoria. Photo Craig Allen.
Volunteers inspect an erosion gully at Nardoo Hills in Victoria. Photo Craig Allen.
Major earthworks are sometimes needed to remove levy banks or dams that disrupt the natural flow of water, or to repair serious erosion gullies. The Gungoandra Creek rock weir and fish way on Scottsdale Reserve is a great example.

How the land responds

The seeds of plants caught in silt traps quickly germinate and help to further slow the movement of water and stabilise the soil.

Restoring the natural flow of water across the land surface helps to return water to creeks, rivers and natural aquifers and nourishes the soil and the native habitats.

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