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SOIL PROFILE
SOIL EROSION
SOIL CONSERVATION
CONTROL ON FLOODS
SOIL PROFILE
SOIL PROFILE
• Soil profile is the sequence and nature of
the horizons super imposed one above the
other & exposed in a pit section dug
through the soil mantle .
The O horizon
The A horizon
The B horizon
The C horizon
The R horizon
The O horizon
• These are organic horizons mainly composed of fresh or
partly decomposed organic matter .
This horizon is divided into two sub layers
O1 (Aoo) region
It is the uppermost layer which consists of freshly-fallen
dead leaves , flowers & fruits , dead remains of animals
etc .
O2 (Ao) region
This is just below the O1 region in which decomposition has
began . Thus organic matter is found under different stages of
decomposition & micro organisms like bacterium , fungi ,
actinomycetes are formed
The A horizon
• These are the mineral horizons . These are rich in
organic matter & soluble salts , clay ,aluminum etc.
A1 region
• This is dark & rich in organic matter . The
amorphous , finely divided organic matter become
mixed with mineral matter which is known as
Humus which is dark brown or black colored
A2 region
• This is light in color which the mineral particle of
large size as sand are more with little amount of
organic matter . This is also known as eluvial zone
THE B HORIZON
• The B horizon is dark colored due to the presence of silica rich
clay organic compounds , hydrated oxides of aluminum & iron
etc.
THE C HORIZON
• These are the mineral horizon below the B horizon but
excluding true bed rock and without any characteristics of A & B
horizons . It consists of incompletely weathered large mass of
rocks.
THE R HORIZON
• This is the parent unweathered bedrock upon which there is a
collected water
SOIL EROSION
What is soil erosion
Types of soil erosion
Agents of soil erosion
Factors influencing soil erosion
Effects of soil erosion
SOIL EROSION
What is soil erosion ?
• Soil erosion is a natural process & remove
soil from one location to another. It
becomes a problem when human activity
causes it to occur much faster than under
natural conditions .
TYPES OF SOIL EROSION
• Normal or geologic erosion
It occurs under normal natural conditions
by itself without the interference of man .
It is a very slow process.
• Accelerated soil erosion
This is the most serious types of loss
generally caused by an interference of any
agencies like man & animals. It is a rapid
process
BY VARIOUS AGENTS
AGENTS OF SOIL EROSION
Based on the various agents that bring about soil erosion , there are following
types of soil erosion in nature .
• WATER EROSION
• WIND EROSION
• EROSION DUE TO OVER HUNTING , OVER GRAZING
& DEFORESTATION
WATER EROSION
• It is caused by the action of rain water , which
removes the soil by falling as rain drops as well
as by its surface slope action
• Types soil erosion caused by water
 Splash erosion
 Sheet erosion
 Rill erosion
 Gully erosion
 Stream bank erosion
WATER EROSION
• This type of soil erosion occurs when the
falling drops splash on the soil .
SPLASH EROSION
SHEET EROSION
• The soil removed in small but uniform amounts
from all over and therefore , does not leave a
mark behind.
WATER EROSION
• Rill erosion
The run off water moves rapidly & cuts small
stream like structure
• Gully erosion
Several rills converge towards the steep slopes
& join to form board channels of water called
gullies .
• Stream bank erosion
The rivers during floods splash their water
against the banks & cuts through them
WIND EROSION
• Soil erosion by wind is common in dry regions
where soil is chiefly sandy & vegetation is very
poor or even absent
• Wind erosion also triggered by the destruction
of natural vegetation cover of land
• Erosion due to winds is very common &
includes
Saltation
Suspension
Surface creeping
WIND EROSION
• Suspension
The wind lift finer particles high up.
• Surface creeping
The coarser & heavier particles roll along the
surface
• Saltation
In arid regions , where rainbow is low , drainage
is poor & high temperature prevail , water
evaporates quickly leaving behind the salts
EFFECTS OF SOIL EROSION
 Loss of soil
 Harmful effects of soil erosion on organic
matter and soil structure
Decline of soil capacity
Deposition of sand and gravel on agriculture
land
Flooding of streams
EFFECTS OF SOIL EROSION
• 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 the formation of gullies
& ravines , valuable agriculture lands are
lost .
EFFECTS OF SOIL EROSION
• Harmful effects of soil erosion on organic
matter & soil structure
Erosion of upper layer of soil
decreases the content of organic matter &
as soil nutrients . As a result the soil
structure gets impoverished .
EFFECTS OF SOIL EROSION
• Decline in soil capacity
When soil is removed bodily from
field , both potential and available plant food
along with mineral material is carried away . As
erosion progresses , the compact soil of low
infiltration capacity is approached . The ability of
land to supply moisture for plant growth is
reduced and the beneficial activity of micro-
organisms lessened . Due to these bad effects ,
the yield are lowered .
EFFECTS OF SOIL EROSION
• Deposition of sand & gravel on agriculture
lands
The wind-borne sand
encroaches the arable lands and makes
them unfertile . Crops are damaged due to
sand storms .
EFFECTS OF SOIL EROSION
Flooding of streams
Soil erosion in catchment areas
of streams due to deforestation & other
destructive activities leads to silting of
streams & reservoirs . This reduces the
capacity of these water bodies to carry
large volume of waters , as they occur
during the rainy season . This way streams
are more prone to flooding .
SOIL CONSERVATION
Soil conservation means
protection , improvement
& sustained renewal of
the soil at any place .
SOIL CONSERVATION
PRINCIPLES OF SOIL CONSERVATION
• Protection of soil from impact of rain drops
• To prevent water from concentrating & moving
down the slope
• To slow down the water movement when it
flows around the slope
• To encourage more water to enter the soil
• To increase the size of soil particle
• Reduction in wind velocity near the ground by
growing vegetation cover , ridging the land .
SOIL CONSERVATION
• METHODS OF SOIL CONSERVATION
BIOLOGICAL METHODS
( Agronomic practices , Dry farming ,
Agrostological methods )
MECHANICAL METHODS
(Countour bunding , contour terracing , water
harvesting etc. )
OTHER METHODS
(Gully control , stream bank protection ,
afforestation )
AGRONOMIC PRACTICES
Natural protection is provided to the soil by
growing vegetation in a manner that reduces
soil loss .
• Contour farming
It involves preparation of the field with
alternative furrows and ridges
Terrace cropping
• The soil is cut and laid to make steps . On the
margins between two steps the slope is vertical
STRIP CROPPING
This practices consists of growing erosion-permitting crops (jowar,
bajra , maize ) in alternate strips with erosion checking close
growing crops ( grasses , pulses )
CROP ROTATION
This refers to growing of two or more different crops in sequence
in a field for maintaining the soil fertility .
MECHANICAL METHODS
• Basin listing
It involves the construction of small basin
along the contours to retain water which
also reduces its velocity
• Contour terracing
This involves digging a channel along the
slope to intercept and divert the run off
water
OTHER METHODS
• Gully control
To check the widening of gullies by constructing
bunds , dams , drains or diversions through which
excess run off water is channeled
• Stream bank protection
For preventing the cutting and caving of river
banks , drains and constructed and concrete or
pitching is done
FLOOD
• A flood is a natural event that can have
reaching effects on people and
environment
• Put simply , a flood is too much water in
the wrong place
• Flood is caused by many factors . Heavy
rain fall , highly accelerated rainfall , severe
wind over rainfall
EFFECTS OF FLOODS
• It damages the property and endangers
the lives of humans and other species
• Rapid water runoff causes soil erosion
• The spawning grounds for fish and other
habitats can become polluted or
completely destroyed
METHODS OF CONTROL
• DAMS
Construction of dams and their associated
reservoirs are designed completely or
partially to aid in flood protection and
control
METHODS OF CONTROL
• River defenses
In many countries rivers are prone to
floods and are often carefully managed.
Defenses such as levees , bunds , and
reservoirs are used to prevent rivers from
their banks . When these defenses fail
emergency measures such as sandbags or
portable inflatable tubes are used .
METHODS OF CONTROL
• Coastal defenses
Coastal flooding has been addressed in
Europe and the Americans with coastal
defenses such as sea walls , beach
nourishment and barrier islands
SOIL  PROFILE  SOIL EROSION SOIL CONSERVATION  CONTROL ON FLOODS
SOIL  PROFILE  SOIL EROSION SOIL CONSERVATION  CONTROL ON FLOODS

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SOIL PROFILE SOIL EROSION SOIL CONSERVATION CONTROL ON FLOODS

  • 1. SOIL PROFILE SOIL EROSION SOIL CONSERVATION CONTROL ON FLOODS
  • 3. SOIL PROFILE • Soil profile is the sequence and nature of the horizons super imposed one above the other & exposed in a pit section dug through the soil mantle . The O horizon The A horizon The B horizon The C horizon The R horizon
  • 4. The O horizon • These are organic horizons mainly composed of fresh or partly decomposed organic matter . This horizon is divided into two sub layers O1 (Aoo) region It is the uppermost layer which consists of freshly-fallen dead leaves , flowers & fruits , dead remains of animals etc . O2 (Ao) region This is just below the O1 region in which decomposition has began . Thus organic matter is found under different stages of decomposition & micro organisms like bacterium , fungi , actinomycetes are formed
  • 5. The A horizon • These are the mineral horizons . These are rich in organic matter & soluble salts , clay ,aluminum etc. A1 region • This is dark & rich in organic matter . The amorphous , finely divided organic matter become mixed with mineral matter which is known as Humus which is dark brown or black colored A2 region • This is light in color which the mineral particle of large size as sand are more with little amount of organic matter . This is also known as eluvial zone
  • 6. THE B HORIZON • The B horizon is dark colored due to the presence of silica rich clay organic compounds , hydrated oxides of aluminum & iron etc. THE C HORIZON • These are the mineral horizon below the B horizon but excluding true bed rock and without any characteristics of A & B horizons . It consists of incompletely weathered large mass of rocks. THE R HORIZON • This is the parent unweathered bedrock upon which there is a collected water
  • 7.
  • 8. SOIL EROSION What is soil erosion Types of soil erosion Agents of soil erosion Factors influencing soil erosion Effects of soil erosion
  • 9. SOIL EROSION What is soil erosion ? • Soil erosion is a natural process & remove soil from one location to another. It becomes a problem when human activity causes it to occur much faster than under natural conditions .
  • 10.
  • 11. TYPES OF SOIL EROSION • Normal or geologic erosion It occurs under normal natural conditions by itself without the interference of man . It is a very slow process. • Accelerated soil erosion This is the most serious types of loss generally caused by an interference of any agencies like man & animals. It is a rapid process
  • 12.
  • 14. AGENTS OF SOIL EROSION Based on the various agents that bring about soil erosion , there are following types of soil erosion in nature . • WATER EROSION • WIND EROSION • EROSION DUE TO OVER HUNTING , OVER GRAZING & DEFORESTATION
  • 15. WATER EROSION • It is caused by the action of rain water , which removes the soil by falling as rain drops as well as by its surface slope action • Types soil erosion caused by water  Splash erosion  Sheet erosion  Rill erosion  Gully erosion  Stream bank erosion
  • 16.
  • 17.
  • 18. WATER EROSION • This type of soil erosion occurs when the falling drops splash on the soil . SPLASH EROSION SHEET EROSION • The soil removed in small but uniform amounts from all over and therefore , does not leave a mark behind.
  • 19.
  • 20. WATER EROSION • Rill erosion The run off water moves rapidly & cuts small stream like structure • Gully erosion Several rills converge towards the steep slopes & join to form board channels of water called gullies . • Stream bank erosion The rivers during floods splash their water against the banks & cuts through them
  • 21.
  • 22.
  • 23. WIND EROSION • Soil erosion by wind is common in dry regions where soil is chiefly sandy & vegetation is very poor or even absent • Wind erosion also triggered by the destruction of natural vegetation cover of land • Erosion due to winds is very common & includes Saltation Suspension Surface creeping
  • 24.
  • 25. WIND EROSION • Suspension The wind lift finer particles high up. • Surface creeping The coarser & heavier particles roll along the surface • Saltation In arid regions , where rainbow is low , drainage is poor & high temperature prevail , water evaporates quickly leaving behind the salts
  • 26. EFFECTS OF SOIL EROSION  Loss of soil  Harmful effects of soil erosion on organic matter and soil structure Decline of soil capacity Deposition of sand and gravel on agriculture land Flooding of streams
  • 27. EFFECTS OF SOIL EROSION • 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 the formation of gullies & ravines , valuable agriculture lands are lost .
  • 28. EFFECTS OF SOIL EROSION • Harmful effects of soil erosion on organic matter & soil structure Erosion of upper layer of soil decreases the content of organic matter & as soil nutrients . As a result the soil structure gets impoverished .
  • 29. EFFECTS OF SOIL EROSION • Decline in soil capacity When soil is removed bodily from field , both potential and available plant food along with mineral material is carried away . As erosion progresses , the compact soil of low infiltration capacity is approached . The ability of land to supply moisture for plant growth is reduced and the beneficial activity of micro- organisms lessened . Due to these bad effects , the yield are lowered .
  • 30. EFFECTS OF SOIL EROSION • Deposition of sand & gravel on agriculture lands The wind-borne sand encroaches the arable lands and makes them unfertile . Crops are damaged due to sand storms .
  • 31. EFFECTS OF SOIL EROSION Flooding of streams Soil erosion in catchment areas of streams due to deforestation & other destructive activities leads to silting of streams & reservoirs . This reduces the capacity of these water bodies to carry large volume of waters , as they occur during the rainy season . This way streams are more prone to flooding .
  • 32. SOIL CONSERVATION Soil conservation means protection , improvement & sustained renewal of the soil at any place .
  • 33. SOIL CONSERVATION PRINCIPLES OF SOIL CONSERVATION • Protection of soil from impact of rain drops • To prevent water from concentrating & moving down the slope • To slow down the water movement when it flows around the slope • To encourage more water to enter the soil • To increase the size of soil particle • Reduction in wind velocity near the ground by growing vegetation cover , ridging the land .
  • 34. SOIL CONSERVATION • METHODS OF SOIL CONSERVATION BIOLOGICAL METHODS ( Agronomic practices , Dry farming , Agrostological methods ) MECHANICAL METHODS (Countour bunding , contour terracing , water harvesting etc. ) OTHER METHODS (Gully control , stream bank protection , afforestation )
  • 35. AGRONOMIC PRACTICES Natural protection is provided to the soil by growing vegetation in a manner that reduces soil loss . • Contour farming It involves preparation of the field with alternative furrows and ridges Terrace cropping • The soil is cut and laid to make steps . On the margins between two steps the slope is vertical
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  • 37. STRIP CROPPING This practices consists of growing erosion-permitting crops (jowar, bajra , maize ) in alternate strips with erosion checking close growing crops ( grasses , pulses ) CROP ROTATION This refers to growing of two or more different crops in sequence in a field for maintaining the soil fertility .
  • 38. MECHANICAL METHODS • Basin listing It involves the construction of small basin along the contours to retain water which also reduces its velocity • Contour terracing This involves digging a channel along the slope to intercept and divert the run off water
  • 39. OTHER METHODS • Gully control To check the widening of gullies by constructing bunds , dams , drains or diversions through which excess run off water is channeled • Stream bank protection For preventing the cutting and caving of river banks , drains and constructed and concrete or pitching is done
  • 40. FLOOD • A flood is a natural event that can have reaching effects on people and environment • Put simply , a flood is too much water in the wrong place • Flood is caused by many factors . Heavy rain fall , highly accelerated rainfall , severe wind over rainfall
  • 41. EFFECTS OF FLOODS • It damages the property and endangers the lives of humans and other species • Rapid water runoff causes soil erosion • The spawning grounds for fish and other habitats can become polluted or completely destroyed
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  • 44. METHODS OF CONTROL • DAMS Construction of dams and their associated reservoirs are designed completely or partially to aid in flood protection and control
  • 45. METHODS OF CONTROL • River defenses In many countries rivers are prone to floods and are often carefully managed. Defenses such as levees , bunds , and reservoirs are used to prevent rivers from their banks . When these defenses fail emergency measures such as sandbags or portable inflatable tubes are used .
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  • 47. METHODS OF CONTROL • Coastal defenses Coastal flooding has been addressed in Europe and the Americans with coastal defenses such as sea walls , beach nourishment and barrier islands