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one form of soil degradation.
 The agents of soil erosion are water and
wind, each contributing a significant
amount of soil loss each year.
The loss of soil from farmland may
be reflected in reduced crop
production potential, lower surface
water quality and damaged drainage
networks.
 Excessive (or accelerated) erosion causes both
"on-site" and "off-site" problems.
include decreases in agricultural
productivity and (on natural landscapes)
ecological collapse, both because of loss
of the nutrient-rich upper soil layers.
include sedimentation of waterways and
as well as sediment-related damage to
roads and houses.
Soil and water being splashed by the
impact of a single raindrop.
 Splash Erosion- the impact of a
falling raindrop creates a small
crater in the soil, ejecting soil
particles.
 Sheet erosion - the transport of
loosened soil particles by
overland flow.
 Rill erosion refers to the development
of small, ephemeral
concentrated flow paths which
function as both sediment
source and sediment delivery
systems for erosion on
hillslopes.
 Gully erosion occurs when runoff
water accumulates and rapidly
flows in narrow channels
during or immediately after
heavy rains or melting snow,
removing soil to a considerable
depth.
 is derived from the erosion and entrainment of
material by the moving ice of a glacier.
 Occurs with continued water flow along a
linear feature.
 occurring due to the flow of the stream, and
the boulders and stones (and much of the soil)
that are lying on the edges are glacial till that
was left behind as ice age glaciers flowed over
the terrain.
 wearing away of the banks of a stream or
river. This is distinguished from changes on
the bed of the watercourse, which is referred
to as scour.
 At extremely high flows, kolks, or vortices are
formed by large volumes of rapidly rushing
water.
 a major geomorphological force, especially in
arid and semi-arid regions. It is also a major
source of land degradation, evaporation,
desertification, harmful airborne dust, and
crop damage—especially after being increased
far above natural rates by human activities
such as deforestation, urbanization, and
agriculture.
 Deflation, where the wind picks up and
carries away loose particles; and
 Abrasion, where surfaces are worn down as
they are struck by airborne particles carried by
wind.
 Surface Creep, where larger, heavier particles slide
or roll along the ground;
 Saltation, where particles are lifted a short height
into the air, and bounce and saltate across the surface
of the soil; and
 Suspension, where very small and light particles are
lifted into the air by the wind, and are often carried
for long distances.
 The amount and intensity of precipitation is
the main climatic factor governing soil erosion
by water.
 The composition, moisture, and compaction of
soil are all major factors in determining the
erosivity of rainfall.
 Vegetation acts as an interface between the
atmosphere and the soil.
 Tilled farmland such as this is very susceptible
to erosion from rainfall, due to the destruction
of vegetative cover and the loosening of the
soil during plowing.
 In this clear cut, almost all of the vegetation
has been stripped from surface of steep slopes,
in an area with very heavy rains.
 first by denuding the land of vegetative cover,
altering drainage patterns,
 compacting the soil during construction; and
 next by covering the land in an impermeable layer of
asphalt or concrete that increases the amount of
surface runoff and increases surface wind speeds.
 Much of the sediment carried in runoff from urban
areas (especially roads) is highly contaminated with
fuel, oil, and other chemicals.
 The warmer atmospheric temperatures
observed over the past decades are expected to
lead to a more vigorous hydrological cycle,
including more extreme rainfall events.
 (the row of trees)planted next to an
agricultural field, acting as a shield against
strong winds. This reduces the effects of wind
erosion, and provides many other benefits.
 The most effective known method for erosion
prevention is to increase vegetative cover on
the land, which helps prevent both wind and
water erosion.
 an extremely effective means of erosion
control, which has been practiced for
thousands of years by people all over the
world.
such as mixed-cropping (instead of
monocropping) and crop rotation have also
been shown to significantly reduce erosion
rates.
PENTECOSTES, Aga C.
BSED 2F-1

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2.soil.d pentecostes, aga c.

  • 1.
  • 2. one form of soil degradation.  The agents of soil erosion are water and wind, each contributing a significant amount of soil loss each year.
  • 3. The loss of soil from farmland may be reflected in reduced crop production potential, lower surface water quality and damaged drainage networks.
  • 4.  Excessive (or accelerated) erosion causes both "on-site" and "off-site" problems.
  • 5. include decreases in agricultural productivity and (on natural landscapes) ecological collapse, both because of loss of the nutrient-rich upper soil layers.
  • 6. include sedimentation of waterways and as well as sediment-related damage to roads and houses.
  • 7.
  • 8. Soil and water being splashed by the impact of a single raindrop.
  • 9.  Splash Erosion- the impact of a falling raindrop creates a small crater in the soil, ejecting soil particles.  Sheet erosion - the transport of loosened soil particles by overland flow.
  • 10.  Rill erosion refers to the development of small, ephemeral concentrated flow paths which function as both sediment source and sediment delivery systems for erosion on hillslopes.
  • 11.  Gully erosion occurs when runoff water accumulates and rapidly flows in narrow channels during or immediately after heavy rains or melting snow, removing soil to a considerable depth.
  • 12.
  • 13.  is derived from the erosion and entrainment of material by the moving ice of a glacier.
  • 14.
  • 15.  Occurs with continued water flow along a linear feature.
  • 16.  occurring due to the flow of the stream, and the boulders and stones (and much of the soil) that are lying on the edges are glacial till that was left behind as ice age glaciers flowed over the terrain.
  • 17.
  • 18.  wearing away of the banks of a stream or river. This is distinguished from changes on the bed of the watercourse, which is referred to as scour.
  • 19.
  • 20.  At extremely high flows, kolks, or vortices are formed by large volumes of rapidly rushing water.
  • 21.
  • 22.  a major geomorphological force, especially in arid and semi-arid regions. It is also a major source of land degradation, evaporation, desertification, harmful airborne dust, and crop damage—especially after being increased far above natural rates by human activities such as deforestation, urbanization, and agriculture.
  • 23.
  • 24.  Deflation, where the wind picks up and carries away loose particles; and  Abrasion, where surfaces are worn down as they are struck by airborne particles carried by wind.
  • 25.
  • 26.  Surface Creep, where larger, heavier particles slide or roll along the ground;  Saltation, where particles are lifted a short height into the air, and bounce and saltate across the surface of the soil; and  Suspension, where very small and light particles are lifted into the air by the wind, and are often carried for long distances.
  • 27.
  • 28.
  • 29.  The amount and intensity of precipitation is the main climatic factor governing soil erosion by water.
  • 30.  The composition, moisture, and compaction of soil are all major factors in determining the erosivity of rainfall.
  • 31.  Vegetation acts as an interface between the atmosphere and the soil.
  • 32.
  • 33.  Tilled farmland such as this is very susceptible to erosion from rainfall, due to the destruction of vegetative cover and the loosening of the soil during plowing.
  • 34.
  • 35.  In this clear cut, almost all of the vegetation has been stripped from surface of steep slopes, in an area with very heavy rains.
  • 36.
  • 37.  first by denuding the land of vegetative cover, altering drainage patterns,  compacting the soil during construction; and  next by covering the land in an impermeable layer of asphalt or concrete that increases the amount of surface runoff and increases surface wind speeds.  Much of the sediment carried in runoff from urban areas (especially roads) is highly contaminated with fuel, oil, and other chemicals.
  • 38.  The warmer atmospheric temperatures observed over the past decades are expected to lead to a more vigorous hydrological cycle, including more extreme rainfall events.
  • 39.
  • 40.  (the row of trees)planted next to an agricultural field, acting as a shield against strong winds. This reduces the effects of wind erosion, and provides many other benefits.
  • 41.
  • 42.  The most effective known method for erosion prevention is to increase vegetative cover on the land, which helps prevent both wind and water erosion.
  • 43.
  • 44.  an extremely effective means of erosion control, which has been practiced for thousands of years by people all over the world.
  • 45.
  • 46. such as mixed-cropping (instead of monocropping) and crop rotation have also been shown to significantly reduce erosion rates. PENTECOSTES, Aga C. BSED 2F-1