This document discusses soil and water conservation measures for fodder production. It describes soil erosion caused by water and wind, and measures to conserve soil like agronomic practices (contour cultivation, conservation tillage, mulching, cropping systems), mechanical measures (contour bunding, graded bunding, terracing), forestry measures, and agrostological measures (using grasses). It also discusses surface and subsurface drainage methods for agricultural lands.
Soil water conservation methods in agricultureVaishali Sharma
This presentation includes introduction as well as all the methods in agriculture either engineering or agronomic measures used in conservation of soil and water against erosion or other deteriorative factors.
Soil water movement
Soil water movement
Soil water movement
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Soil water conservation methods in agricultureVaishali Sharma
This presentation includes introduction as well as all the methods in agriculture either engineering or agronomic measures used in conservation of soil and water against erosion or other deteriorative factors.
Soil water movement
Soil water movement
Soil water movement
Soil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movement
Soil moisture characteristic curve is the relationship between the water content and the soil water potential, ψ.
It describes the functional relationship between soil water content and its energy status in terms of its matric potential under equilibrium conditions.
This curve is characteristic for different types of soil.
It is also called the Water retention curve
This presentation includes description about water erosion, types of water erosion i.e. Raindrop erosion, Sheet erosion, Rill erosion, Gully erosion, Stream bank erosion, Sea-shore erosion Landslide/ slip erosion and Tunnel erosion.
Universal soil loss equation, soil loss estimation, factors of USLE, its use and limitation, soil loss measurement by multi slot divisor and coshocton wheel sampler
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
Introduction
enlist of problematic soil
Salt affected soil
Characteristic of salt affected soil
Comparison between salt affected soil
Reclamation of Saline soils
Reclamation of sodic soils
Reclamation of saline-sodic soils
Acidic soils
Reclamation of acidic soil
Acid Sulphate soils and its management
Calcareous soil
IN this presentation cover Erosivity and erodibilty
Different methods to calculate soil loss.
Er. Gurpreet Singh
M.tech from PAU, Ludhiana
Assistant Prof.
Khalsa college.
Soil moisture characteristic curve is the relationship between the water content and the soil water potential, ψ.
It describes the functional relationship between soil water content and its energy status in terms of its matric potential under equilibrium conditions.
This curve is characteristic for different types of soil.
It is also called the Water retention curve
This presentation includes description about water erosion, types of water erosion i.e. Raindrop erosion, Sheet erosion, Rill erosion, Gully erosion, Stream bank erosion, Sea-shore erosion Landslide/ slip erosion and Tunnel erosion.
Universal soil loss equation, soil loss estimation, factors of USLE, its use and limitation, soil loss measurement by multi slot divisor and coshocton wheel sampler
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
Introduction
enlist of problematic soil
Salt affected soil
Characteristic of salt affected soil
Comparison between salt affected soil
Reclamation of Saline soils
Reclamation of sodic soils
Reclamation of saline-sodic soils
Acidic soils
Reclamation of acidic soil
Acid Sulphate soils and its management
Calcareous soil
IN this presentation cover Erosivity and erodibilty
Different methods to calculate soil loss.
Er. Gurpreet Singh
M.tech from PAU, Ludhiana
Assistant Prof.
Khalsa college.
Watershed Management for Sustainable Development of Rainfed areasAntaraPramanik
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Over 120 million ha land area has been declared degraded (Maji et al., 2007) in India.
The annual soil loss rate in India is nearly 16.4 t/ha (Mandal and Sharda, 2013).
The loss of sediments caused by soil erosion not only deteriorates the quality of surface water, nearby water bodies, and wetlands but also reduces the productivity of agricultural land (Issaka and Ashraf, 2017).
Watershed technology is suitable to protect and enhance soil fertility, which is deteriorating at an alarming rate with agricultural intensification. A vast range of activities of every day life depends upon adequate supplies of water. For e.g. Agriculture and Industry, power production, inland transportation, sanitation and public health services and so on.
Therefore to provide all these activities construction of watershed and manage is essential.
Fast deterioration of natural resources is one of the key issues, threatening sustainable development of rainfed agriculture as most rainfed regions are facing multifaceted problems of land degradation, water shortage, acute poverty, and escalating population pressure.
Poor watershed management is a major cause of land and water degradation, rural poverty in India.
The management of watershed provides a means to achieve sustainable land and water management.
Improved and appropriate soil and water management practices are most important for sustainable and improved livelihoods in the rainfed areas because other technological interventions such as improved varieties, fertilizers, etc. are generally not so effective where soil is degraded and water is severely limited.
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The mechanical measures of soil conservation include various engineering techniques and structures which are adopted to supplement the biological methods when the latter alone are not sufficiently effective. These are also called as engineering measures.
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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.