SOILEROSION
SOILEROSION
SOILEROSION
SOIL EROSION:
● Splash erosion
● Sheet erosion
● Rill erosion
● Gully erosion
● Stream bank erosion
● Seashore erosion
SPLASH EROSION:
The vegetative cover protects the soil from the beating and dispersing action of
the raindrops by forming a canopy over the soil surface. Vegetation also acts as a
mechanical obstruction to flowing water, thus reducing its erosive potential. The
plant roots help in building a better structure. They said in opening the soil and
thereby accelerating water absorption and reducing surface run-off.
3. Tillage:
The infiltration and permeability of the soil is improved by the practice of proper
tillage and thereby reducing the chances of erosion. But excess tilling exposes the
soil to erosion, especially by wind.
4. Nature of the soil:
Erodability of the soil is influenced by the nature of the soil, particularly
its texture, structure, organic matter, amounts and kinds of salts present,
presence of hard pan in the soil and presence of high water table.
5. Soil Moisture:
The presence of high water table checks the infiltration and permeability,
thus allowing more flow of water on the surface, and greater erosion. At
the same time, long continuous rainless periods cause loosening of soil
and thus expose the soil to erosion by wind
CAUSES
1. Deforestation:
Removal of vegetation cover has caused widespread erosion in Western
CAUSES
Ghats, Uttar Pradesh and in Himachal Pradesh.
4. Overgrazing:
A surplus of livestock population in our country is a big strain on grasses and
fodder. The tread of cattle hardens the soil and prevents new shoots from
emerging. Overgrazing by goats is a serious problem in certain stretches of
the Aravalis and in Punjab and Himachal hills. The goats not only pull off
leaves and branches, but they also uproot grass, as opposed to sheep, which
only nibble the top shoots.
EFFECTS OF SOIL EROSION
EFFECTS OF SOIL EROSION:
1. Loss of Soil:
The top-soil is lost by erosion which is the most fertile section, having evolved
over centuries of soil-forming processes. Due to formation of gullies and
ravines, valuable agricultural lands are lost.
2. Gullies or Ravines:
Because of gully erosion, nearly 10 mHa area is affected. These gulleys are
known by different names—khars in Gujarat, Maharashtra and Karnataka;
ravines in Madhya Pradesh, Uttar Pradesh and Rajasthan along Yamuna and
Chambal; kotar lands in Gujarat and chos (the rainy season torrents) and
landslides in Hoshiarpur in the Shivaliks.
. Coastal Erosion:
An extreme example of soil erosion is to be seen in sand movement from the
coast in the Saurashtra region of Gujarat, where the once flourishing ports are
now covered with advancing sand-dunes.
Measures to control
MEASURES TO CONTROL soil erosion
SOIL EROSION
Strip Cropping:
This practice consists of growing erosion-permitting crops (jowar, bajra,
maize) in alternate strips with erosion checking close- growing crops (grasses,
pulses). The erosion checking strips check and hold the flowing water and soil.
Crop Rotation:
This refers to growing of two or more different crops in sequence in a field for
maintaining the soil fertility. Continuous growing of clean-cultivated crops
(e.g., tobacco) causes more erosion. A good rotation should include densely
planted small grains, spreading legume which may check soil erosion.
Strip cropping
Stubble Mulching:
This means leaving crop residue or vegetative litter on the land as a surface
protection against erosion and for conserving moisture by favouring
infiltration and reducing evaporation.
Terracing:
L.sowjanya
Roll: 35
F1