types of soil erosion
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types of soil erosion


Stream bank erosion can also be accelerated by factors such as: Read more about what causes bank erosion (PDF, 161KB) and what causes stream bed erosion (PDF, 645KB). Rain splash erosion happens when raindrops move the soil. It is estimated that formation of one centimetre of soil requires several years. Therefore, we can talk of two types of soil erosion viz., water erosion and wind erosion.

Water Erosion: Type # 6. Grassed waterways are usually used on farms. Gullies often starts along bullock cart tracks or burrows of animals (Fig.

It takes place when run-off water laden with soil flowing along the slopes forming small finger-like channels. Water Erosion: Type # 5.

On cleared areas, plant locally adapted, deep-rooted, fast-growing trees. This is called glacial erosion (Fig.

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Sheet movement of running water causes sheet erosion, which has eroded layers from hill slopes.

When water penetrates through a soil crack or a hole where a root has decayed, the soil disperses and is carried away with the flow to leave a small tunnel.

7.2). Soil is being swept away much faster than it can be replenished and is quickly becoming one of the most important environmental issues of the day. For example, a waterfall may form, with runoff picking up energy as it plunges over the gully head.

Water erosion consisting of rilling, gullying sheet-wash and rain peeling process is mainly confined to the mountains, hills and upper slopes of the piedmont zone.

Sheet erosion occurs when runoff travels over ground and moves particles that are dislodged by splash erosion. ; this is known as soil erosion. More intense rain, more erosion. Water Erosion: During heavy rains, water removes a lot of soil. Recent floods have made stream bank erosion a widespread problem across Queensland.

Rivulets form larger channels and gradually erode the soil. It results in the accumulation of excessive coarse material on the surface within a short time after the beginning of rainfall.

Hence, the water forms small rivulets which, in turn, erode a deeper layer of the soil. Wind erosion is hard to measure but some signs are bare soil, drifts, exposed plant roots and dust clouds.

Regions with very heavy and frequent rainfall face a large amount of soil loss. Soil erosion is the process where wind, water and human beings detach soil particles and deposit them somewhere else. Equilibrium occurs in nature between the climate (chiefly rainfall and temperature) of a place and the vegetation cover which protects the layer of soil. Even though the land is practically level, much of the organic matter and fertility bearing elements of the soil may be floated away. It is better to prevent landslides than pay for expensive, time-consuming rehabilitation which may only be partially effective. The soil surface layer is made dense and compact.

As the volume of concentrated run-off increase and attains more velocity on slopes, it enlarges the rill into gullies.

The beating and churning action of raindrops make the soil into an impervious layer of surface mud. Soil is formed by the process of ‘weathering’ of rocks, that is, disintegration and decomposition of rocks and mineral at or near the earth’s surface ... Before moving into types of foundation, let's learn what is foundation or footing. In cultivation or pastures, advanced rill erosion can develop into gully erosion.

Even modest wind velocities can keep individual particles of humus, clay and silt in suspension. Raindrops hit bare soil with enough force to break the soil aggregates. Running water is one of the main cause of soil erosion. Stream Bank Erosion: Streams and rivers change their course by cutting one bank and depositing silt loads on the others.

Construction sites and sloping fields often show signs of rill erosion. Rill and sheet erosion on a cultivated paddock, Example of mass movement—landslip on a steep slope near Coolangatta, Queensland, Dust storm, western Queensland, in October 2007. This depends on the rate and amount of run-off water and erodability of soils.

Wind erosion is accentuated when the soil is dry, weakly aggregated, devoid of vegetation cover along with over grazing and the winds are strong.

Hill slopes are prone to sheet erosion and rill erosion. Field shelter belts made from trees and tall grasses provide some extra protection against wind erosion by reducing the wind velocity. Falling raindrops splash soil. Grass, shrubs and trees retard the transportation of soil. However, sandy soils are vulnerable to wind erosion because they cannot store very much moisture and have low fertility.

This article throws light upon the eight main types of water erosion. Therefore, we can talk of two types of soil erosion viz., water erosion and wind erosion. Most of the structure consist of two parts, one above the ground wh... A number of systems of classification have been evolved for categorizing various types of soil. The major cause of stream bank erosion is the destruction of vegetation on river banks (generally by clearing, overgrazing, cultivation, vehicle traffic up and down banks or fire) and the removal of sand and gravel from the stream bed. state election. Soil erosion is a kind of soil degradation that occurs naturally on all land.

Report a Violation, Paragraphs on Soil Erosion: Meaning, Causes and Forms, Soil Erosion: 4 Major Causes of Soil Erosion, Soil Erosion: Notes on the Human Factors Responsible for Soil Erosion.

A single raindrop may splash wet soil as much as two feet high five feet away.

Tree roots act as a binder of the top layer of the soil. All Rights Reserved. This can... Rill Erosion. Wind erosion: Wind erosion is the removal soil particles by the force and kinetic energy of the wind.These soil particles are transported and deposited when the wind energy drops.

Controlling tillage erosion has only one real solution, using no-till systems that eliminate tillage completely.


Move topsoil from the depositional areas back to hill crests to reduce clay knobs and rocks. The amount of hill slope erosion largely depends on how the land is used. Some of Queensland’s best agricultural land is on floodplains because of the high fertility soils and availability of water for irrigation. Large amounts of top soil are carried away due to precipitation, wind, flowing rivers, glaciers etc.

Water erosion is the most prevalent kind of erosion.

It may be controlled by the following conservation methods: By this erosion, soil is removed uniformly in thin layer from the entire surface area.

Tunnel erosion is the removal of subsoil.

It is different from the erosion of the bed of a watercourse, that is referred to as scouring.

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One of the most important things that we can do to ensure the health of our crops and nearby ecosystems is to reduce soil erosion. This site is protected by reCAPTCHA and the Google At an advanced stage, gullies result in ravines which are sometimes 50 to 10 feet deep.

The puddle erosion may be controlled by growing cover crops and grasses; and by the use of organic matter and stubble mulch. The slope of the land is a potent factor in determining the velocity of water and the consequent soil erosion. In gentle topographical areas covered by vegetation weathered soil and clay particles will resist erosion. The movement and relocation of topsoil by water is water erosion. It is most likely to occur when strong winds blow over light-textured soils that have been heavily grazed during drought periods. Some soil erosion causes are mentioned below. Wind erosion removes topsoil and redistributes it elsewhere. Rain splash only occurs if the rain falls with high intensity.

Soil is moved from the top of the field down a slope, exposing the subsoil while burying top soil.

This type of erosion is highly visible and affects soil productivity, restricts land use, and can damage roads, fences and buildings.

Sheet Erosion.

The movement and relocation of topsoil by water is water erosion. When raindrops, loosen the soil and splash it into the air, nearly all of the particles that are dislodged seem to be 2 mm or less in diameter.

Soils vulnerable to tunnel erosion have dispersible subsoils with naturally high levels of sodium.

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