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Gully and Streambank Erosion
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Gully and Streambank Erosion


Most gullies and streams running through farmland show some signs of erosion. The most devastating erosion occurs during periods of peak flow following heavy rains, especially if soils in the upper catchment are saturated. In larger streams, bank erosion is largely a catchment issue and may require the involvement of other farmers and land managers to find collective ways of tackling excessive runoff.


Erosion of small tributaries and drainage lines contributes to the bulk of sediment in larger streams and can often be tackled effectively by individual farmers. Any action in the small waterways high in the catchment will help reduce flooding and erosion downstream, and help improve water quality.

Gully and streambank erosion are often triggered by particular land and water management practices. Activities such as the extensive clearing of land, uncontrolled stock grazing along watercourses, and the straightening of channels disturb the equilibrium that exists between the flow regime and channel structure, leading to instability.


There are three types of soil erosion processes that may contribute to gully and streambank erosion:
1. Subaerial erosion — this occurs when the bank is exposed to the weather and is subject to rainsplash, stock trampling etc.
2. Scour — the direct removal of bank material by flowing water.
3. Slumping — a mass movement that occurs when bank material slips or falls into the stream often as a result of waterlogging of the bank.


Identifying which of these are contributing to an erosion problem and understanding the process itself, can guide revegetation to control the problem. Before tackling a problem at a particular point, it is important to look at the condition of the watercourse up and down stream and if possible, observe the stream during a storm.


In many cases the revegetation of unstable banks can provide relatively cheap long-term stability. Trees on the bank can reduce waterlogging and the risk of slumping, and the roots may also bind unstable soils. Grass and shrubs on the top of the bank and up the slope can protect the bank from direct scouring by flowing water. Although revegetation is a positive option for the environment, in some cases it is not enough to address streambank stability problems. In these instances it may be appropriate to use complementary engineering solutions.

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