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SEDIMENTATION
• Sedimentation is the tendency for particles in
suspension to settle out of the fluid in which they
are entrained and come to rest against a barrier.
This is due to their motion through the fluid in
response to the forces acting on them: these forces
can be due to gravity, centrifugal acceleration, or
electromagnetism.
SEDIMENTATION
• In geology, sedimentation is often used as
the opposite of erosion. In that sense, it
includes the termination of transport by
siltation or true bed load transport. Settling is
the falling of suspended particles through the
liquid, where as sedimentation is the
termination of the settling process.
Contd…
• Sedimentation may pertain to objects of various
sizes, ranging from large rocks in flowing water
to suspensions of dust and pollen particles to
cellular suspensions to solutions of single
molecules such as proteins and peptides. Even
small molecules supply a sufficiently strong
force to produce significant sedimentation.
SEDIMENTATION PROCESSES
• Sedimentation is the process of allowing particles
in suspension in water to settle out of the
suspension under the effect of gravity. The
particles that settle out from the suspension
become sediment, and in water treatment is known
as sludge. When a thick layer of sediment
continues to settle, this is known as consolidation.
When consolidation of sediment, or sludge, is
assisted by mechanical means then this is known
as thickening.
Different aspects in sedimentation process
The sedimentation process comprises the
following aspects:
• Erosion
• Transportation
• Deposition
• Compaction & Cementation
EROSION
• The term erosion refers to the process of
weathering, corrosion or abrasion of a material to
form smaller particles.
• The smaller units thus formed are relocated by
water, wind, ice, animals or humans.
• The top soil, organic material and other valuable
natural resources are removed by the process of
erosion.
TRANSPORTATION
• The sediment particles move under the action of
the force of gravity and/ or the movement of fluid
in which the sediment is entrained by a variety of
sediment transport process, such as rolling, sliding,
jumping and suspension.
• The sediment transport is due to the movement in
the fluid occurs in water bodies such as rivers,
lakes, oceans and sea, due to currents and tides and
in glaciers under the influence of wind.
DEPOSITION
• The sediment particles carried by wind, water or
ice are laid down near the banks or the shores.
• The sediments carried by flowing water, for
instance, a stream are deposited when the velocity
of the flowing water decreases.
• The large sediment particles are deposited near the
shore, whereas the smaller sediment particles settle
away from the shore.
COMPACTION & CEMENTATION
• The deeply buried sediments are under pressure
because of the weight of overlying layers, which
causes the grains to pack tightly. This is
Compaction.
• Cementation involves the sticking of the sediment
particles together with the help of cementing
minerals such as calcium carbonate, silicon
dioxide, iron oxides and clay minerals. This is
similar to the cement binding the sand grains in a
brick layer’s mortar.
GLOBAL SEDIMENTATION PROBLEMS
• Damage of agricultural land because the harmful
materials in sediments reduce the fertility and
productivity of soils.
• Sediments deposited in fertile plains hamper
surface drainage.
• Its deposition in stream channels lowers the flood
carrying capacity therefore, causing more frequent
overflows.
GLOBAL SEDIMENTATION PROBLEMS
• Sediment deposition affects the quality of water
and its suitability for human consumption.
• Loss of important or sensitive aquatic habitat.
• Decrease in fishery resources.
• Loss of recreation attributes such as boating,
fishing, swimming etc.,
• Corals have been observed to be intolerant to
sediments as it affects the physical and biological
processes, which hampers their existence.
GLOBAL SEDIMENTATION PROBLEMS
 Sediments threaten a nation’s economy.
Sedimentation of reservoirs have the following
impacts,
Loss of Hydroelectric power generation
Loss of Irrigation production
Loss of Flood control benefits
Increasing in dredging costs of hydroelectric
reservoirs
Loss of revenues from tourism and recreational
activities.
Corrective measures of
Erosion & Sedimentation
• Effective erosion & sedimentation control measures
can be accomplished only when the soil surface is
protected from the erosive forces of wind, rain &
runoff.
• Some of the techniques for best management
practices of erosion control are:
1. Mulching: In this method, organic material is
applied to soil surface to conserve soil moisture,
prevent surface compaction and erosion of top
soil, control of weeds, etc.,
SILT FENCES
• Silt fences are constructed usually at the
construction site. They act like dams to trap the
sediment and allow water to leave the site.
BERMS
• Berms are narrow, earthen ridges built across
roads to allow water to leave the site.
GEOTEXTILE ROLL
• They are known as filter fabrics. These are highly
permeable, synthetic textile material used to prevent
erosion of soil. It acts like a filter, allows water to
move from the soil while the soil is retained.
BRUSH MATTRESS
• It is also referred as brush mat. It is a revegetation
technique that provide protection to stream banks or
slopes from soil erosion.
GABIONS
• These are structures filled with bricks, boulders and
stones, used for stabilization and retention of soil.
They are of three types namely gabion basket,
gabion mattress and sack gabion.
TREE REVETMENT
• In this method, trees are anchored along the banks of
a stream. The erosion of soil, sand and silt decrease,
which get deposited along the bank.
SODDING
• Layers of soil containing grass and plant roots
are placed as a thick mat over an area of exposed
soil as an effective erosion control measure.

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Sedimentation

  • 1. SEDIMENTATION • Sedimentation is the tendency for particles in suspension to settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the forces acting on them: these forces can be due to gravity, centrifugal acceleration, or electromagnetism.
  • 2. SEDIMENTATION • In geology, sedimentation is often used as the opposite of erosion. In that sense, it includes the termination of transport by siltation or true bed load transport. Settling is the falling of suspended particles through the liquid, where as sedimentation is the termination of the settling process.
  • 3. Contd… • Sedimentation may pertain to objects of various sizes, ranging from large rocks in flowing water to suspensions of dust and pollen particles to cellular suspensions to solutions of single molecules such as proteins and peptides. Even small molecules supply a sufficiently strong force to produce significant sedimentation.
  • 4. SEDIMENTATION PROCESSES • Sedimentation is the process of allowing particles in suspension in water to settle out of the suspension under the effect of gravity. The particles that settle out from the suspension become sediment, and in water treatment is known as sludge. When a thick layer of sediment continues to settle, this is known as consolidation. When consolidation of sediment, or sludge, is assisted by mechanical means then this is known as thickening.
  • 5.
  • 6. Different aspects in sedimentation process The sedimentation process comprises the following aspects: • Erosion • Transportation • Deposition • Compaction & Cementation
  • 7. EROSION • The term erosion refers to the process of weathering, corrosion or abrasion of a material to form smaller particles. • The smaller units thus formed are relocated by water, wind, ice, animals or humans. • The top soil, organic material and other valuable natural resources are removed by the process of erosion.
  • 8. TRANSPORTATION • The sediment particles move under the action of the force of gravity and/ or the movement of fluid in which the sediment is entrained by a variety of sediment transport process, such as rolling, sliding, jumping and suspension. • The sediment transport is due to the movement in the fluid occurs in water bodies such as rivers, lakes, oceans and sea, due to currents and tides and in glaciers under the influence of wind.
  • 9. DEPOSITION • The sediment particles carried by wind, water or ice are laid down near the banks or the shores. • The sediments carried by flowing water, for instance, a stream are deposited when the velocity of the flowing water decreases. • The large sediment particles are deposited near the shore, whereas the smaller sediment particles settle away from the shore.
  • 10.
  • 11. COMPACTION & CEMENTATION • The deeply buried sediments are under pressure because of the weight of overlying layers, which causes the grains to pack tightly. This is Compaction. • Cementation involves the sticking of the sediment particles together with the help of cementing minerals such as calcium carbonate, silicon dioxide, iron oxides and clay minerals. This is similar to the cement binding the sand grains in a brick layer’s mortar.
  • 12.
  • 13. GLOBAL SEDIMENTATION PROBLEMS • Damage of agricultural land because the harmful materials in sediments reduce the fertility and productivity of soils. • Sediments deposited in fertile plains hamper surface drainage. • Its deposition in stream channels lowers the flood carrying capacity therefore, causing more frequent overflows.
  • 14. GLOBAL SEDIMENTATION PROBLEMS • Sediment deposition affects the quality of water and its suitability for human consumption. • Loss of important or sensitive aquatic habitat. • Decrease in fishery resources. • Loss of recreation attributes such as boating, fishing, swimming etc., • Corals have been observed to be intolerant to sediments as it affects the physical and biological processes, which hampers their existence.
  • 15. GLOBAL SEDIMENTATION PROBLEMS  Sediments threaten a nation’s economy. Sedimentation of reservoirs have the following impacts, Loss of Hydroelectric power generation Loss of Irrigation production Loss of Flood control benefits Increasing in dredging costs of hydroelectric reservoirs Loss of revenues from tourism and recreational activities.
  • 16. Corrective measures of Erosion & Sedimentation • Effective erosion & sedimentation control measures can be accomplished only when the soil surface is protected from the erosive forces of wind, rain & runoff. • Some of the techniques for best management practices of erosion control are: 1. Mulching: In this method, organic material is applied to soil surface to conserve soil moisture, prevent surface compaction and erosion of top soil, control of weeds, etc.,
  • 17. SILT FENCES • Silt fences are constructed usually at the construction site. They act like dams to trap the sediment and allow water to leave the site.
  • 18. BERMS • Berms are narrow, earthen ridges built across roads to allow water to leave the site.
  • 19. GEOTEXTILE ROLL • They are known as filter fabrics. These are highly permeable, synthetic textile material used to prevent erosion of soil. It acts like a filter, allows water to move from the soil while the soil is retained.
  • 20. BRUSH MATTRESS • It is also referred as brush mat. It is a revegetation technique that provide protection to stream banks or slopes from soil erosion.
  • 21. GABIONS • These are structures filled with bricks, boulders and stones, used for stabilization and retention of soil. They are of three types namely gabion basket, gabion mattress and sack gabion.
  • 22. TREE REVETMENT • In this method, trees are anchored along the banks of a stream. The erosion of soil, sand and silt decrease, which get deposited along the bank.
  • 23. SODDING • Layers of soil containing grass and plant roots are placed as a thick mat over an area of exposed soil as an effective erosion control measure.