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Agronomic Soil Conservation measures -
Use of Vegetation:
Crops and vegetables which cover the ground surface
well and have extensive root system reduce soil
erosion. Plant canopy protect the soil from the
adverse effect of rainfall. The grasses and legumes
produce dense sod which helps in reducing soil
erosion. The vegetation provides organic matter to
the soil. As a result, the fertility of soil
increases and the physical condition of soil is
improved. Following cropping systems help in
controlling soil erosion -
Crop rotation:
Crop rotation is planned sequence of cropping.
Rotation of crop is an important method for checking
erosion and maintaining productivity of soil. A good
rotation should include densely planted small grain
crops, spreading legume crop etc. which may check
soil erosion.
Strip Cropping:
It consists of growing erosion permitting crop (e.g.
Jowar, Bajra, Maize etc.) in alternate strips with
erosion checking close growing crops (e.g. grasses,
pulses etc.). Strip cropping employs several good
farming practices including crop rotation, contour
cultivation, proper tillage, stubbles mulching,
cover cropping etc. It is very effective and
practical means for controlling soil erosion,
specially for gently slopping land. It may be of
different types as follows:
-
Contour strip Cropping: Contour strip
cropping is the growing of erosion permitting and
erosion resisting crops alternately in strips
across the slope and on the contour line. This
practice is useful because it checks the fast flow
of run-off water increases the infiltration of
water in the soil and prevents soil erosion.
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Field Strip Cropping: Strips of crop are
parallel to the general slope of the land.
-
Wind Strip Cropping: Strips of crop are
across the direction of wind regardless of
contour.
-
Buffer Strip Cropping: In this, the
severally eroded portion of land is permanently
kept under grass and contour strip cropping is
practices in the rest of the area.
There is a special type of contour strip cropping in
which care is taken to check soil erosion.
Cultivation of dense plant and grasses:
Sod forming crop such as lucern (medicago sativa L),
Egyptian Cloveror. Berseem (Trifolium alexandrinum),
ground nut (Arachis hypogea L), Sannhemp (Crotolaria
juncea), grass etc. cover the surface of the land
and their roots bind the soil particles to form soil
aggregates, thus preventing soil erosion.
Cultivation of proper crops:
Cultivation of row crop in sloppy lands permits soil
erosion. In this filed, the crops particularly
cereals, fodder crop etc. should be broadcasted and
the plants remain haphazardly in field. As a result,
the movement of water gets obstacle and more water
is absorbed in the soil, thus reducing soil
erosion.Mixed and intercropping (Cowpea-Vigna
catjang, with cotton – Gossipum Sp, maize – Zea mays
with soyabean – Glycine max etc.) practice checks
the soil erosion and avoids the risks of the crop
failure.
The land should not be kept without crop:
There is very scope of soil erosion if there are no
crops on the land. The soil erosion decreases in
different way of cropped land.
Afforestation:
Afforestation means growing of forests where there
were no forests before owing to lack of seed trees
or due to adverse factors such as unstable soil,
aridity or swampiness. Along with afforestation,
reforestation should be undertaken which means
replanting of forests at places where they have been
destroyed by uncontrolled forest fires, excessive
felling and lopping. Afforestation is the best means
to check the soil erosion. Lutz and Chandler (1946)
cited the following points in support of
vegetational check erosion as follows:
-
Infiltration of water is favoured due to high
porosity of soil under vegetation. Percolation of
water helps in preventing the soil moisture which
accelerates further growth of the vegetation.
-
Surface accumulation of organic matter increases
the water holding capacity of the underground
soil.
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Root system of vegetation holds the soil
mechanically and provides stability of the
underground soil.
-
It gives the protection against wind. The forest
vegetation shields the soil from direct effect of
drought, snow and rain.
Mulching: Mulches
of different kinds such a leaves, straws, paper,
stubbles, etc. minimize evaporation and increase the
absorption of moisture and protect the surface of
the land against the beating action of rain drops.
Later on they decay to form humus which improves the
physical condition of soil. Natural mulching also
helps in the infiltration of water and the reduction
of evaporation.
Organic manure:
Organic manures improve the soil structure. The
crumb and granular structure increases the
infiltration and permeability in the soil and
conserve the soil water. Consequently soil erosion
decreases.
Control of grazing:
Grazing increases the soil erosion. But the grazing
cannot be completely stopped in all areas. So the
restricted and rotational grazing may be helpful in
checking soil erosion to some extent. The area open
to grazing for sometimes should be closed for the
following year to facilitate regeneration of forests
and to maintain thick ground vegetation.
Good tillage:
Tillage is the mechanical manipulation of soil by
different kinds of implements. Tillage makes the
soil loose and friable which helps in retention of
water. The special method of tillage practices
should be followed for the conservation purposes.
Tillage may consist of several types of soil
manipulation such as ploughing, harrowing,
cultivation etc.
Mechanical Soil Conservation measures -
Mechanical measures include various engineering
techniques and structure. This practices aim at some
objective as follows:
-
To divide a long slope of land into a series of
shorter ones in order to reduce the velocity of
run off water.
-
To retain the water in the land for long period so
as to allow maximum water to be absorbed and held
in the soil and less water flows down the slope of
the land at non-erosive velocity.
-
To protect the soil against erosion by water.
The important mechanical soil conservation measures
are as follows:
Contour bunding:
Contour bunding consists of building earthen
embankment at intervals across the slope and along
the contour line of the field. A series of such bund
divide the area into strips and act as barrier to
the flow of water. As a result, the amount and
velocity of run-off are reduced, resulting reducing
the soil erosion. Contour bunding is made on land
where the slope is not very steep and the soil is
fairly permeable. Contour bunds are also called
level terraces, absorbtion type terraces or ridge
type teracces. Contour bunding works are carried out
over wide areas in many parts of India, notably in
Andhra Pradesh, Gujarat, Karnataka, Maharashtra and
Tamil Nadu.
Terracing:
A
terrace is an embankment of ridge of earth
constructed across the slope to control run off and
to minimize soil erosion. A terrace reduces the
length of the hill side slope, thereby reducing
sheet and rill erosion and prevents formation of
gullies. There are different types of terraces as
follows:
Bench terracing:
It consists of transforming relatively steeps land
into a series of level or nearly level strips or
steeps running across the slope. The soil materials
that are excavated from the upper part of the
terrace is used in filling the lower part and a
small bund is also raised along the outer edge of
the terrace to check the downward flow of rainwater
and also soil erosion.
Channel terrace:
It consists of making of wide but shallow channels
across the slope of the land either exactly on
contour line or with a slight grade (0.1 to 0.2 per
cent). In this process, the excavated soil is placed
along the lower edge of the channel in the form of
low ridge.
Narrow based terrace:
It consists of making a number of narrow based
ridges or bunds at a distance of 1m to 2m across the
slope of the land at suitable intervals in high
rainfall areas.
Broad based ridge terrace:
It consists of making wide but low bunds on the
contour lines by excavating soils from both sides of
terrace. This is practiced in areas where the
rainfall is relatively low.
Contour trenching:
It consist of making a series of deep pit (i.e. 2ft.
wide and 1ft. deep) or trenches across the slope at
convenient distance. The soil excavated from the
trenches is deposited on the lower edge of the
trenches where forest trees are planted. |