Water Erosion

Water Erosion

Erosion is the detachment of earth material from the surface. Once detached, agents like water or wind transport the material to a new location where it is deposited. The most ubiquitous form of erosion is that done by water. 

Figure WM.10 Rain drop impact causing splash erosion (Image courtesy NRCS)

Rain splash erosion is caused by the impact of water striking the surface. Rain splash erosion generally takes place in two steps. As precipitation is absorbed by the surface it fills the pore spaces, loosening soil particles and driving them apart. The impact of subsequent rain drops hitting the surface splash the particle away from the point of impact. The effect is to give the surface a dimpled-like appearance.

 

Figure WM.11 Severe sheet erosion on a field (Image courtesy NRCS)

Surface runoff forms when the rainfall intensity of a storm exceeds the infiltration capacity of the soil. Sheet erosion is caused by the unconfined flow of water running across the surface. The effects of sheet erosion are often hard to distinguish because such thin layers of soil are being removed. It isn't until several years later that significant degradation is perceived. 

 

 

Figure WN.12 NRCS personnel inspecting rill erosion on a field (Image courtesy NRCS)

Rill erosion is caused by water concentrating into innumerable, closely-spaced small channels. Left unchecked, rills can cut vertically and horizontally and when joined, for gullies.


 

Figure WN.13 Severe gully erosion on a field in Iowa (Image courtesy NRCS)

Gullies are steep-sided trenches formed by the coalescence of many rills. Once started they are difficult to stop. 

 


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Mass Movement Types
 

تصاویری از دنیایی فرسایش و عوامل مربوط به آن

 

 creep

A hill side in northern New Zealand showing creeping erosion. Large sections of soil are slowly creeping downhill, leaving deep cracks behind. Notice the difference in soil management between the farm on left, who uses fertiliser and the one on the right side of the fence, who doesn't.

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clips

A hill side near the one on left, showing land clipping where sheep and cattle tread. Clips are small drops of soil, leaving bare soil behind

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slip or land slide

A slip or land slide on a hill side in northern New Zealand. The bare soil left behind is very vulnerable to erosion from raindrop impact and should be fertilised and re-sown, followed by fertiliser maintenance. Seeding alfalfa, which is a leguminous deep-rooting ground cover, resistant to drought, could hasten the soil's recovery.

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creep with tunnelling

A form of creep caused by tunnelling and subsequent collapse of the underground tunnel. Such erosion forms creeping gullies that are very hard to contain. Planting trees uphill preventively and inside the gully helps to contain it and to minimise erosion by water. Retirement would not necessarily be a remedy

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retired and fenced hillside

The erodible hillside has been retired from grazing and fenced off. Natural vegetation is allowed to re-establish, pioneered by the leguminous and prickly gorse. Gorse is considered a pest because it infests poor farmland and is hard to eradicate. But for hillslopes like these, it brings natural nitrogen fertiliser, while preparing the soil for the native bush (on left

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space-planted trees

A hillside preventively planted in poplar trees, widely spaced in order to let light through. Trees anchor the soil, cycle deep nutrients and provide decomposing litter to feed the soil. Fallen branches and stems slow down sheet wash. Leaf litter covers the soil against raindrop damage. Stems and branches can be used in gullies to stem the flow of water

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spaced tree planting on hill side

A hill side is preventively planted in widely spaced poplar trees. These trees bring many advantages and may make a decisive difference in the sustainability of this grassland. The trees are not intended to be harvested, but need occasional maintenance

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dense gully planting

To overcome gully erosion and land slides, the gullies have been planted with poplar trees in dense formation. Poplar trees can be planted as tall posts, reaching over cattle and sheep, so the area does not need to be fenced off.

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pugging

Particularly where grazing animals camp, the ground becomes compacted and waterlogged, a process called pugging. Pugs with standing water in them, are the result. The soil is bared, and exposed to raindrop impact damage

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tramping

Where animals tramp on their accustomed patterns of movement, the soil becomes compacted and pugged. Particularly on dairy farms where the cows walk to and from the milking shed twice daily, this can be a problem. Paving sensitive pathways, helps to protect the soil from eroding

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riparian fence

The riparian fence in this picture was not placed to protect a river bank but to protect a stand of mangrove trees in northern New Zealand. As can be seen, these plants disappeared where cattle grazed.

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topdressing

A four-wheel drive truck topdressing pasture in New Zealand. This farm is accessible by four-wheel drive vehicle, but even then, a suitable day must be picked, with little wind and the soil dry enough. Steeper farms are topdressed by plane

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ploughing downhill, not along contours

A cropland near Bombay, New Zealand, is not being ploughed along height contours, inviting disaster. Farmers often plough this way to prevent waterlogging; water trapped between furrows. The methods used also leave far too much soil bare

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massive erosion on cropland

Not far from the place on left, this cropland was severely damaged by rain. It was courting disaster by not contour-ploughing, and allowing such a long water course (field length down-hill). Estimated loss: 10% of the top soil in one rain storm! Notice how rilling starts already high up the field

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strip cropping and contour ploughing

Fields take on bizarre patterns when ploughed along height contours. But it reduces erosion considerably. The picture shows how the land is cropped in strips, each with its own crop and seasonal timing

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terraced padi culture

In the humid tropics, padi culture has proved its sustainability. The terraces contour the land, forming perfectly horizontal cropland, which harvests its own water. Padis make their own nitrogen fertiliser with the help of Azolla ferns

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erosion rilling on a road side

An example of erosion rilling in loose topsoil on a highway bank. Note how the young grass roots were insufficient to stop it, neither was the cover of hay that preceded sowing. See the chapter on roading and roadside management

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gully control by car tyres

This farmer attempts to control erosion with the help of thousands of old car tyres; in the gully to prevent gully scouring and also on the sandy slopes. Rather than introducing an element of pollution, it would be much better to fight erosion by natural means. Besides, trees would have achieved much more. But the point here is that these hills should never have been grazed in the first place, and retirement is now the best remedy

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sand saltating over beach

In heavy wind, the sand is seen saltating away from the photographer, as a fast moving sheet, weaving ripples as it goes. The darker sand, which contains heavier particles and magnetite, stays put underneath, as the light-coloured sand moves over it

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smoke & dust over north Africa

This satellite image captured smoke and dust blowing from northern Africa over the Mediterranean Sea. The white plumes are smoke, the brown plumes on left are dust. Burning is still a common practice, particularly in arid areas. It is done to prepare soil for planting, but precious nutrients and soil organic matter are lost.

(Image courtesy NASA)

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