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Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
What is Soil Erosion
The word "erosion" is derived from the Latin "erosio",
meaning to "to gnaw away". In general terms soil
erosion implies the physical removal of topsoil by
various agents, including rain, water flowing over and
through the soil profile, wind, ice or gravitational
pull.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Erosion and Weathering
Erosion is distinguished from weathering, which is
the process of chemical or physical breakdown of the
minerals in the rocks, although the two processes may
be concurrent.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
On site and Off site
The consequences of soil erosion can be seen both on-
site and off-site.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
On site
On-site effects are the loss of soil, the breakdown of
the soil structure and a decline in organic matter.
Erosion also reduces available soil moisture, resulting
in more draught-prone conditions.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Off Site
Off-site problems result from sedimentation
downstream or downwind which reduces the capacity
of rivers and drainage ditches, increases the risk of
flooding, blocks irrigation canals and shortens the
design life of reservoirs. Eroded sediment is also a
pollutant, the chemicals absorbed by it can increase
the levels of nitrogen and phosphorus in water bodies
and result in eutrophication.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Types of Soil Erosion
Wind erosion: Wind erosion is the removal soil
particles by the force and kinetic energy of the wind.
These soil particles are transported and deposited
when the wind energy drops.
Water erosion: Water erosion is caused by the
kinetic energy of rain falling on the soil surface and by
the mechanical force of runoff.
Gravity erosion: Mass movement of soil occurs on
steep slopes under the influence of gravity. The
process involves the transfer of slope-forming
materials from higher to lower grounds due to self
weight. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Causes of Soil Erosion
Climatic Factors
Land use – by man
Soil itself
Hydrology
Landform and topography
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Climatic Factors
The two most important climatic factors having a
direct effect on erosion are precipitation and wind
velocity. Other climatic factors have an indirect effect
on soil erosion, such as water balance,
evapotranspiration, temperature and relative
humidity. Indirect factors affect the erosivity of
rainfall by altering the soil moisture regime and the
proportion of rainfall that may become surface runoff.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Land Use
Humans play a major role in soil erosion through
their use and abuse of natural resources, for example
deforestation, grazing, arable land use, faulty farming
systems, high crop intensity, housing construction,
mining etc.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Soil Itself
The susceptibility of a soil to erosion is influenced by
its physical, hydrological, chemical and mineralogical
properties as well as its soil profile characteristics.
Important soil physical and hydrological properties
that affect the resistance of a soil to erosion include
texture, structure, water retention and transmission
properties.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Hydrology
Infiltration, surface detention, overland flow velocity,
and subsurface water flow are important soil erosion
components of the hydrological cycle. The different
types of flow and their velocities may be turbulent or
laminar, steady or unsteady, uniform or non-uniform
and influence the extent of erosion
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Topography
Slope gradient, slope length and shape of slope are
the important variables of landform that affect
erosion processes for all types of soil erosion, e.g.,
splash, sheet, rill, and gully erosion.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Soil Conservation
Soil is effectively a non-renewable resource because
erosion occurs at rates that outpace soil formation.
Artificial soil formation is impractical, so we have
little choice but to conserve the soil we have to ensure
a continued supply of agricultural products.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Techniques
Modern techniques include
- contour plowing
- terracing
- crop rotation
- shelter belt
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Other Techniques
Afforestation
Using organic fertilisers
Using stubble and mulch
Practicing Intercropping – alternative strips of taller
and shorter plants can lift the wind over the land
surface and cut down the amount of soil blown away.
Cut down on overgrazing
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
And Other Techniques
Reduced tillage
No – tillage
Water harvesting
But, what is tillage?
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Tillage
Tillage is the agricultural preparation of the soil by ploughing,
ripping, or turning it. Tillage can also mean the land that is
tilled. There are two types of tillage: primary and secondary
tillage.
Primary tillage loosens the soil and mixes in fertilizer and/or
plant material, resulting in soil with a rough texture.
Secondary tillage produces finer soil and sometimes shapes the
rows. It can be done by a using various combinations of
equipment: plough, harrow, dibble, hoe, shovel, rotary tillers,
subsoiler, ridge or bed forming tillers and roller.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
Water Harvesting
Water Harvesting is capturing and storing rainfall to
irrigate plants or to supply people and animals. It is
one of the oldest known gardening methods, dating
back to the beginnings of agriculture.
Water harvesting will help you save money on
monthly water bills and reduce your dependence on
municipally-supplied water. A well-designed system
will also decrease your landscape maintenance needs.
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.
The END
Author: Faiq Allaud-din, M.Phill Scholar, Dept. of
Botany, Kust.

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Erosion of soils

  • 1. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 2. What is Soil Erosion The word "erosion" is derived from the Latin "erosio", meaning to "to gnaw away". In general terms soil erosion implies the physical removal of topsoil by various agents, including rain, water flowing over and through the soil profile, wind, ice or gravitational pull. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 3. Erosion and Weathering Erosion is distinguished from weathering, which is the process of chemical or physical breakdown of the minerals in the rocks, although the two processes may be concurrent. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 4. On site and Off site The consequences of soil erosion can be seen both on- site and off-site. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 5. On site On-site effects are the loss of soil, the breakdown of the soil structure and a decline in organic matter. Erosion also reduces available soil moisture, resulting in more draught-prone conditions. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 6. Off Site Off-site problems result from sedimentation downstream or downwind which reduces the capacity of rivers and drainage ditches, increases the risk of flooding, blocks irrigation canals and shortens the design life of reservoirs. Eroded sediment is also a pollutant, the chemicals absorbed by it can increase the levels of nitrogen and phosphorus in water bodies and result in eutrophication. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 7. Types of Soil Erosion Wind erosion: Wind erosion is the removal soil particles by the force and kinetic energy of the wind. These soil particles are transported and deposited when the wind energy drops. Water erosion: Water erosion is caused by the kinetic energy of rain falling on the soil surface and by the mechanical force of runoff. Gravity erosion: Mass movement of soil occurs on steep slopes under the influence of gravity. The process involves the transfer of slope-forming materials from higher to lower grounds due to self weight. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 8. Causes of Soil Erosion Climatic Factors Land use – by man Soil itself Hydrology Landform and topography Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 9. Climatic Factors The two most important climatic factors having a direct effect on erosion are precipitation and wind velocity. Other climatic factors have an indirect effect on soil erosion, such as water balance, evapotranspiration, temperature and relative humidity. Indirect factors affect the erosivity of rainfall by altering the soil moisture regime and the proportion of rainfall that may become surface runoff. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 10. Land Use Humans play a major role in soil erosion through their use and abuse of natural resources, for example deforestation, grazing, arable land use, faulty farming systems, high crop intensity, housing construction, mining etc. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 11. Soil Itself The susceptibility of a soil to erosion is influenced by its physical, hydrological, chemical and mineralogical properties as well as its soil profile characteristics. Important soil physical and hydrological properties that affect the resistance of a soil to erosion include texture, structure, water retention and transmission properties. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 12. Hydrology Infiltration, surface detention, overland flow velocity, and subsurface water flow are important soil erosion components of the hydrological cycle. The different types of flow and their velocities may be turbulent or laminar, steady or unsteady, uniform or non-uniform and influence the extent of erosion Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 13. Topography Slope gradient, slope length and shape of slope are the important variables of landform that affect erosion processes for all types of soil erosion, e.g., splash, sheet, rill, and gully erosion. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 14. Soil Conservation Soil is effectively a non-renewable resource because erosion occurs at rates that outpace soil formation. Artificial soil formation is impractical, so we have little choice but to conserve the soil we have to ensure a continued supply of agricultural products. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 15. Techniques Modern techniques include - contour plowing - terracing - crop rotation - shelter belt Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 16. Other Techniques Afforestation Using organic fertilisers Using stubble and mulch Practicing Intercropping – alternative strips of taller and shorter plants can lift the wind over the land surface and cut down the amount of soil blown away. Cut down on overgrazing Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 17. And Other Techniques Reduced tillage No – tillage Water harvesting But, what is tillage? Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 18. Tillage Tillage is the agricultural preparation of the soil by ploughing, ripping, or turning it. Tillage can also mean the land that is tilled. There are two types of tillage: primary and secondary tillage. Primary tillage loosens the soil and mixes in fertilizer and/or plant material, resulting in soil with a rough texture. Secondary tillage produces finer soil and sometimes shapes the rows. It can be done by a using various combinations of equipment: plough, harrow, dibble, hoe, shovel, rotary tillers, subsoiler, ridge or bed forming tillers and roller. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 19. Water Harvesting Water Harvesting is capturing and storing rainfall to irrigate plants or to supply people and animals. It is one of the oldest known gardening methods, dating back to the beginnings of agriculture. Water harvesting will help you save money on monthly water bills and reduce your dependence on municipally-supplied water. A well-designed system will also decrease your landscape maintenance needs. Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.
  • 20. The END Author: Faiq Allaud-din, M.Phill Scholar, Dept. of Botany, Kust.