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SOIL AND WATER CONSERVATION
AND
DRAINAGE OF WATER FOR FODDER
PRODUCTION
Dr. MANISH BOBADE
NAGPUR VETERINARY COLLEGE
NAGPUR
Soil Erosion
• It is the process of detachment of soil particles from the parent body and
transportation of the detached soil particles by wind and or water.
• The agents causing erosion are wind and water.
• The detaching agents are falling raindrops, channel flow and wind.
• The transporting agents are flowing water, rain splash and wind.
• Depending on the agents of erosion, it is called as water erosion or wind erosion
or wave erosion.
Soil conservation
• Soil conservation is using and managing land, based on the capabilities of the
land itself, involving the application of the best practices to result in greatest
profitable production without damaging the land.
• This is accomplished by.
– Land use based on its capability
– Conservation of soil and moisture to avoid damage to the soil
– Use of the best soils and crop management practices, correction of acidity,
alkalanity and drainage etc.
• Soil conservation is adopted to prevent the soil from soil erosion.
MEASURES TO CONSERVE SOIL DUE TO
WATER EROSION
Measures to prevent erosion are broadly classified as
A. Agronomic measures
B. Mechanical measures
C. Forestry measures and
D. Agrostological measures
A. AGRONOMIC MEASURES
Agronomic measures are mostly adopted in dry land areas where slope is gentle i.e.
less than 2% when one or more agronomic measures are combined, erosion can be
reduced even if the slope is more than 2%.
Following are the commonly adopted agronomic measures
1. Contour cultivation
2. Tillage
3. Mulching
4. Cropping systems
5. Strip cropping
6. Use of chemical and
7. Others
 Contour cultivation includes contour ploughing,
contour sowing and other intercultural operations.
 By ploughing and sowing across the slope, each
ridge of plough furrow and each row of the crop
act as an obstruction to run off and provide more
time for water to enter into the soil and reduce soil
loss.
1. Contour cultivation
 Conservation tillage is a tillage system that conserves soil, water and energy
resources through the reduction of tillage intensity and retention of crop
residue.
 Conservation tillage involves the planting, growing and harvesting of crops with
limited disturbance to the soil surface.
 Conservation tillage is disturbing the soil to minimum extent necessary and
leaving crop residues on the soil.
 Mostly adopted conservation tillage system is zero and minimum tillage, and
this can reduce the soil loss to an extent of 50% over conventional tillage.
 Improves soil water infiltration, thereby reducing erosion and water and nitrate
runoff.
zero-tillage sowing implement
2. Conservation Tillage
3.Mulching
 Mulching is the process or practice of covering the soil/ground to make more
favourable conditions for plant growth, development and efficient crop
production.
 Mulch technical term means 'covering of soil'.
 Mulching with plant materials reduces soils loss upto 43 times compared to
bare soil and 17 times compared to cropped soil without mulches.
 Mulches covers the soil surface and protects it from rain drop impact, thus
reducing the run off loss.
 Growing a crop with maximum vegetative cover reduces run off and soil loss.
 In multiple cropping systems, where the soil is covered with crops throughout
the year, the soil loss is minimum as the falling rain drops are interrupted by
the crop.
4. Cropping systems
5. Strip cropping
 Strip cropping is a system of crop
production in which long and narrow
strips of erosion resisting crops (close
growing crops) are alternated with strips
of erosion permitting crops (erect
growing crops) across the slope.
 Groundnut, moth bean, horse-gram, is
some of the erosion resistant crops and
erosion permitting crops are sorghum,
maize and millet.
6. Use of Chemicals
 Aggregate stability can be increased by spraying chemicals like Polyvinyl
Alcohol at 480 kg/ha, the rate however depending on the type of soil.
 Bitumin application also increases the water stable aggregates and
infiltration capacity of the soil.
 Application of organic matter, farmyard manure, crop residues and green
manure increases the aggregate stability and thereby reduces the runoff and
soil losses.
Application of manures and fertilizers provides early crop cover due to
quick growth and thereby reduces the soil loss.
7. Other agronomic practices
B. MECHANICAL MEASURES
Mechanical measures are supplemented with agronomical measures when the
latter, alone is not sufficient.
Some of the mechanical measures are
1. Contour bunding
2. Graded bunding
3. Bread base terrace
4. Bench terracing
5. Trenching
6. Vegetative barriers
7. Grassed waterways and
8. Gully control.
 It consists of building earthen embankments across the slope of the land, following
the contour as closely as possible.
 A series of such bunds divide the area into strips and act as barriers to the flow of
water, thus reducing the amount and velocity of the runoff.
 The contour bunds are formed at all lines of the greatest slope and this ensures
uniform water depth and distribution throughout its length.
 As the bunds are at regular intervals, they intercept the run off from attaining
erosive velocity and causing erosion. Contour bunds are adopted in areas with
rainfall of less than 1500 mm and the slope of upto 6%.
1. Contour Bunding
2. Graded Bunding
 When a grade is provided along the bund for safe disposal of runoff water over
the area between two consecutive bunds, they are called graded bund.
 Graded bunds are adopted in case of high or medium annual rainfall (>600 mm)
and relatively less permeable soil areas.
 Graded bunds are designed to dispose excess runoff safely from agricultural
field.
 This is recommended where the rain water is not readily absorbed either due to
high rainfall or low intake of the soil.
3. Broad Base Terrace
 A broad base terrace is the surface channel or
embankment type construction, which is formed
across the land slope.
 This is a combination of ridge and channel built
across the slope on a controlled grade and has a
wide base and low height of ridge.
 Suitable for deep black soils.
4. Bench Terracing
 Bench terraces are the platform like construction, which are constructed along
the contour of the sloping land.
 Bench terracing consists of principally transforming relatively steep land into a
series of level strips or platforms across the slope of the land.
 This type of terraces are generally constructed on the land slope ranging from
16 to 33%.
 Bench terraces play a significant role to make the hilly land suitable for
cultivation.
 It reduces the slope length and consequently erosion.
5. Trenching
 Contour trenches are ditches dug along a hillside in such a way that they
follow a contour and run perpendicular to the flow of water.
 The soil excavated from the ditch is used to form a berm on the downhill edge
of the ditch.
 Contour trenches are made in non - agricultural land for providing adequate
moisture conditions in order to raise tree and grass species.
 Size of the trench varies with slope, rainfall and depth of soil available.
 The trenches are half refilled diagonally with excavated material and remaining
half of the soil forms the spoil bank.
 Vegetative barriers are permanent strips of stiff, dense vegetation along
the general contour of slopes or across concentrated flow areas.
 These are closely spaced plantation, usually a few rows of grasses or
shrubs, grown along contours.
 Act as a barrier, to check the velocity of overland flow entrapment of silt
load behind them. Eg. Khus (Vettiveria zelanica)
6. Vegetative barriers
7. Grassed Waterways
 Grassed waterways are drainage channels developed either by shaping the
existing drainage ways or constructed separately to agricultural lands.
 Used to handle run off discharge from graded bunds, broad base terraces, bench
terraces etc.
 Suitable perennial grass, deep rooted and spreading type such as Panicum
repens, Brachiaria mutica, Cynodon plectostachyus, Cynodon dactylon and
Paspalum notatum may be established for the stability of the waterways.
8. Gully Control
Gullies are controlled by diverting run off by adoption of agronomical
measures and stabilizing the gully sides and bed by establishing vegetation
and reducing the gradient of the channel to maintain velocities below
erosive level by temporary and permanent structures.
C. FORESTRY MEASURES
• In forest lands, slopes are steep, uneven, soil is less stable, highly erodable
and precipitation is high.
• The vegetation and dried leaves on the floor intercept the rain and reduce
the impact of rain drops.
• Due to overgrazing and felling of trees, most of the hills and hillocks
became naked and barren.
• Re-establishment is essential to avoid erosion and to maintain ecological
balance.
• Afforestation by adopting contour trenching helps in reducing the soil
erosion and increases the infiltration rate.
D. AGROSTOLOGICAL MEASURES
• Grasses are used to prevent soil erosion by intercepting rainfall, binding the
soil particles and by improving soil structure.
• Grasses should be perennial, drought resistance, rhizomniferous, develop
good canopy, deep root system, prostrate in habit and useful for cottage
industries. Eg. Chloris gayana, Dicanthilum annulatum, Heteropogon
contortus etc.
• Grass legumes association is ideal for soil conservation.
• Legumes build up soil fertility by fixing atmospheric nitrogen.
• Grasses are used to stabilize the surface of waterways, contour bunds,
bench terraces etc.
• Further, grasses improve, the soil structure, porosity, infiltration and also
add organic matter to the soil.
METHODS OF DRAINAGE
Surface drainage
• Simplest and commonly adopted method is India. Drainage is achieved by
digging open drains at suitable intervals and depth. Irrigation channels also
serve as drainage channel.
• Surface drainage may be needed to prevent or modify saline-alkali condition in
a soil by leaching.
• If the land is not naturally well drained, artificial drainage must be established
at the same time, the irrigation system is installed.
• Different methods of surface drainage are adopted, depending on the
topography of the land, soil characteristics and crops that are proposed to be
grown.
1. Surface drainage and 2. Subsurface drainage
1. Random field ditch method
– Standing water may be present in the field at several places distributed randomly. These depressions
or micro ponds are connected by means of shallow channels or ditches and these are led into an outlet.
2. Land smoothing
– The elevated areas are cut off and excess soil is spread over lower areas, so that the surface is even
with uniform slope. Excess surface run off is collected and conveyed into the field ditches provided at
the lower end of the field.
3. Bedding
– Small furrows are formed at known intervals parallel to the slope for draining out water and known as
dead furrows. The land between these furrows is known as beds. Small ridge or bund is made at the
centre of the bed with gradual slope to drain water into the dead furrows.
4. Parallel field ditch system
– Almost similar to bedding system except for deep drains and uneven interval between drains.
5. Broad bed and furrow method
– The field is laid out into 1.05 m beds and 45 cm wide furrows across the slope. About 0.5% slope is
provided for the furrows for free drainage.
– Crops are sown on the beds and furrows help in drainage of water when there is excess rain.
Subsurface drainage
• When surface drainage is not possible due to subsoil conditions, water table
and topography, subsurface drainage is resorted to remove ground water, or
to lower water table.
• Unlike open drainage, land is not wasted and there is no interference to
farming operations by subsurface drainage.
• However, this requires less maintenance and high investments.
Lecture 6 soil & water conservation

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Lecture 6 soil & water conservation

  • 1. SOIL AND WATER CONSERVATION AND DRAINAGE OF WATER FOR FODDER PRODUCTION Dr. MANISH BOBADE NAGPUR VETERINARY COLLEGE NAGPUR
  • 2. Soil Erosion • It is the process of detachment of soil particles from the parent body and transportation of the detached soil particles by wind and or water. • The agents causing erosion are wind and water. • The detaching agents are falling raindrops, channel flow and wind. • The transporting agents are flowing water, rain splash and wind. • Depending on the agents of erosion, it is called as water erosion or wind erosion or wave erosion.
  • 3.
  • 4. Soil conservation • Soil conservation is using and managing land, based on the capabilities of the land itself, involving the application of the best practices to result in greatest profitable production without damaging the land. • This is accomplished by. – Land use based on its capability – Conservation of soil and moisture to avoid damage to the soil – Use of the best soils and crop management practices, correction of acidity, alkalanity and drainage etc. • Soil conservation is adopted to prevent the soil from soil erosion.
  • 5.
  • 6.
  • 7. MEASURES TO CONSERVE SOIL DUE TO WATER EROSION Measures to prevent erosion are broadly classified as A. Agronomic measures B. Mechanical measures C. Forestry measures and D. Agrostological measures
  • 8. A. AGRONOMIC MEASURES Agronomic measures are mostly adopted in dry land areas where slope is gentle i.e. less than 2% when one or more agronomic measures are combined, erosion can be reduced even if the slope is more than 2%. Following are the commonly adopted agronomic measures 1. Contour cultivation 2. Tillage 3. Mulching 4. Cropping systems 5. Strip cropping 6. Use of chemical and 7. Others
  • 9.  Contour cultivation includes contour ploughing, contour sowing and other intercultural operations.  By ploughing and sowing across the slope, each ridge of plough furrow and each row of the crop act as an obstruction to run off and provide more time for water to enter into the soil and reduce soil loss. 1. Contour cultivation
  • 10.  Conservation tillage is a tillage system that conserves soil, water and energy resources through the reduction of tillage intensity and retention of crop residue.  Conservation tillage involves the planting, growing and harvesting of crops with limited disturbance to the soil surface.  Conservation tillage is disturbing the soil to minimum extent necessary and leaving crop residues on the soil.  Mostly adopted conservation tillage system is zero and minimum tillage, and this can reduce the soil loss to an extent of 50% over conventional tillage.  Improves soil water infiltration, thereby reducing erosion and water and nitrate runoff. zero-tillage sowing implement 2. Conservation Tillage
  • 11. 3.Mulching  Mulching is the process or practice of covering the soil/ground to make more favourable conditions for plant growth, development and efficient crop production.  Mulch technical term means 'covering of soil'.  Mulching with plant materials reduces soils loss upto 43 times compared to bare soil and 17 times compared to cropped soil without mulches.  Mulches covers the soil surface and protects it from rain drop impact, thus reducing the run off loss.
  • 12.  Growing a crop with maximum vegetative cover reduces run off and soil loss.  In multiple cropping systems, where the soil is covered with crops throughout the year, the soil loss is minimum as the falling rain drops are interrupted by the crop. 4. Cropping systems
  • 13. 5. Strip cropping  Strip cropping is a system of crop production in which long and narrow strips of erosion resisting crops (close growing crops) are alternated with strips of erosion permitting crops (erect growing crops) across the slope.  Groundnut, moth bean, horse-gram, is some of the erosion resistant crops and erosion permitting crops are sorghum, maize and millet.
  • 14. 6. Use of Chemicals  Aggregate stability can be increased by spraying chemicals like Polyvinyl Alcohol at 480 kg/ha, the rate however depending on the type of soil.  Bitumin application also increases the water stable aggregates and infiltration capacity of the soil.  Application of organic matter, farmyard manure, crop residues and green manure increases the aggregate stability and thereby reduces the runoff and soil losses. Application of manures and fertilizers provides early crop cover due to quick growth and thereby reduces the soil loss. 7. Other agronomic practices
  • 15. B. MECHANICAL MEASURES Mechanical measures are supplemented with agronomical measures when the latter, alone is not sufficient. Some of the mechanical measures are 1. Contour bunding 2. Graded bunding 3. Bread base terrace 4. Bench terracing 5. Trenching 6. Vegetative barriers 7. Grassed waterways and 8. Gully control.
  • 16.  It consists of building earthen embankments across the slope of the land, following the contour as closely as possible.  A series of such bunds divide the area into strips and act as barriers to the flow of water, thus reducing the amount and velocity of the runoff.  The contour bunds are formed at all lines of the greatest slope and this ensures uniform water depth and distribution throughout its length.  As the bunds are at regular intervals, they intercept the run off from attaining erosive velocity and causing erosion. Contour bunds are adopted in areas with rainfall of less than 1500 mm and the slope of upto 6%. 1. Contour Bunding
  • 17. 2. Graded Bunding  When a grade is provided along the bund for safe disposal of runoff water over the area between two consecutive bunds, they are called graded bund.  Graded bunds are adopted in case of high or medium annual rainfall (>600 mm) and relatively less permeable soil areas.  Graded bunds are designed to dispose excess runoff safely from agricultural field.  This is recommended where the rain water is not readily absorbed either due to high rainfall or low intake of the soil.
  • 18. 3. Broad Base Terrace  A broad base terrace is the surface channel or embankment type construction, which is formed across the land slope.  This is a combination of ridge and channel built across the slope on a controlled grade and has a wide base and low height of ridge.  Suitable for deep black soils.
  • 19. 4. Bench Terracing  Bench terraces are the platform like construction, which are constructed along the contour of the sloping land.  Bench terracing consists of principally transforming relatively steep land into a series of level strips or platforms across the slope of the land.  This type of terraces are generally constructed on the land slope ranging from 16 to 33%.  Bench terraces play a significant role to make the hilly land suitable for cultivation.  It reduces the slope length and consequently erosion.
  • 20. 5. Trenching  Contour trenches are ditches dug along a hillside in such a way that they follow a contour and run perpendicular to the flow of water.  The soil excavated from the ditch is used to form a berm on the downhill edge of the ditch.  Contour trenches are made in non - agricultural land for providing adequate moisture conditions in order to raise tree and grass species.  Size of the trench varies with slope, rainfall and depth of soil available.  The trenches are half refilled diagonally with excavated material and remaining half of the soil forms the spoil bank.
  • 21.  Vegetative barriers are permanent strips of stiff, dense vegetation along the general contour of slopes or across concentrated flow areas.  These are closely spaced plantation, usually a few rows of grasses or shrubs, grown along contours.  Act as a barrier, to check the velocity of overland flow entrapment of silt load behind them. Eg. Khus (Vettiveria zelanica) 6. Vegetative barriers
  • 22. 7. Grassed Waterways  Grassed waterways are drainage channels developed either by shaping the existing drainage ways or constructed separately to agricultural lands.  Used to handle run off discharge from graded bunds, broad base terraces, bench terraces etc.  Suitable perennial grass, deep rooted and spreading type such as Panicum repens, Brachiaria mutica, Cynodon plectostachyus, Cynodon dactylon and Paspalum notatum may be established for the stability of the waterways.
  • 23. 8. Gully Control Gullies are controlled by diverting run off by adoption of agronomical measures and stabilizing the gully sides and bed by establishing vegetation and reducing the gradient of the channel to maintain velocities below erosive level by temporary and permanent structures.
  • 24. C. FORESTRY MEASURES • In forest lands, slopes are steep, uneven, soil is less stable, highly erodable and precipitation is high. • The vegetation and dried leaves on the floor intercept the rain and reduce the impact of rain drops. • Due to overgrazing and felling of trees, most of the hills and hillocks became naked and barren. • Re-establishment is essential to avoid erosion and to maintain ecological balance. • Afforestation by adopting contour trenching helps in reducing the soil erosion and increases the infiltration rate.
  • 25. D. AGROSTOLOGICAL MEASURES • Grasses are used to prevent soil erosion by intercepting rainfall, binding the soil particles and by improving soil structure. • Grasses should be perennial, drought resistance, rhizomniferous, develop good canopy, deep root system, prostrate in habit and useful for cottage industries. Eg. Chloris gayana, Dicanthilum annulatum, Heteropogon contortus etc. • Grass legumes association is ideal for soil conservation. • Legumes build up soil fertility by fixing atmospheric nitrogen. • Grasses are used to stabilize the surface of waterways, contour bunds, bench terraces etc. • Further, grasses improve, the soil structure, porosity, infiltration and also add organic matter to the soil.
  • 26. METHODS OF DRAINAGE Surface drainage • Simplest and commonly adopted method is India. Drainage is achieved by digging open drains at suitable intervals and depth. Irrigation channels also serve as drainage channel. • Surface drainage may be needed to prevent or modify saline-alkali condition in a soil by leaching. • If the land is not naturally well drained, artificial drainage must be established at the same time, the irrigation system is installed. • Different methods of surface drainage are adopted, depending on the topography of the land, soil characteristics and crops that are proposed to be grown. 1. Surface drainage and 2. Subsurface drainage
  • 27. 1. Random field ditch method – Standing water may be present in the field at several places distributed randomly. These depressions or micro ponds are connected by means of shallow channels or ditches and these are led into an outlet. 2. Land smoothing – The elevated areas are cut off and excess soil is spread over lower areas, so that the surface is even with uniform slope. Excess surface run off is collected and conveyed into the field ditches provided at the lower end of the field. 3. Bedding – Small furrows are formed at known intervals parallel to the slope for draining out water and known as dead furrows. The land between these furrows is known as beds. Small ridge or bund is made at the centre of the bed with gradual slope to drain water into the dead furrows. 4. Parallel field ditch system – Almost similar to bedding system except for deep drains and uneven interval between drains. 5. Broad bed and furrow method – The field is laid out into 1.05 m beds and 45 cm wide furrows across the slope. About 0.5% slope is provided for the furrows for free drainage. – Crops are sown on the beds and furrows help in drainage of water when there is excess rain.
  • 28. Subsurface drainage • When surface drainage is not possible due to subsoil conditions, water table and topography, subsurface drainage is resorted to remove ground water, or to lower water table. • Unlike open drainage, land is not wasted and there is no interference to farming operations by subsurface drainage. • However, this requires less maintenance and high investments.