問題一覧
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The detachment and subsequent transport of soil materials
soil erosion
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2 General types of erosion
Geologic or Natural erosion Accelerated Erosion
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this represents the erosion characteristics of the land in its natural environment. undisturbed by human activity
Geologic or Natural Erosion
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this is erosion induced by human activities that
Accelerated Erosion
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3 Processes involved during soil erosion by water
Soil Detachment by rainfall Transportation Deposition
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(detachment from the ground)
Soil Detachment by rainfall
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(via wind or water)
Transportation
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(sediemint setting)
Deposition
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This is a process by which raindrops splash soil sediments from the soil surface into the runoff
Soil detachment by rainfall
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from upslope to downhill direction,
transportation
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This refers to the process of sediment settling out under the action of gravity
Sediment deposition
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Types of erosion
water erosion wind erosion
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a type of erosion caused by rainwater, including melted snow running over exposed land surfaces.
Water erosion
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types of water erosion
Sheet Erosion Rill Erosion Gully erosion Stream bank erosion
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this is more or less less the removal of a thin layer of soil
Sheet Erosion
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This is a type of erosion when runat water generally concentrates on small channels
Rill Erosion
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develop deep incisions
Gully erosion
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this is an erasion occurring along the sides of river banks
Stream Bank Erosion
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Forms by Which Materials are Carried away
Extrusion Efflution Efflusion
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the rolling away by large particles
Extrusion
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the removal of very fine particles.
Efflution
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particles of intermediate size move off downwind into the bouncing action called saltation.
Efflusion
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is the movement by very fine particles
Suspension
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rolling movement of particles
Creep
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bouncing movement of particles
Saltation
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types of movement by wind action
suspension creep saltation
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Forms of Wind Erosion
Detrusion Abrasion
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soil projections by tine particles carned in suspension.
Detrusion
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moving particles are larger and bouncing along over the surface
abrasion
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Factors influencing the rate of erosion
1. Rainfall 2. Soil erodability 3. Vegetation or Plant cover 4. Relief (slope) 5. Human Activities
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this is the climatic element that mainly affects erosion in the humid tropics
Rainfall
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this refers to the vulnerability or proneness of the soil to erosion.
Soil erodability
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defined as the fineness or coarseness of soil particles.
Soil texture
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arrangement of primary particles into aggregates
Soil Structure
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is defined as the lowering of the soil's capacity to support human life.
Soil degradation
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is the portion of rainfall that makes its way toward stream channels, lakes, or oceans as surface or subsurface Flow.
Runoff
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FACTORS AFFECTING RUN-OFF
precipitation watershed factor topographic features VEGETATION AND MANAGEMENT PRACTICES
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was developed by the United States Natural Resources Conservation Service
(LCC) Land capability classification
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a method of assessing the extent to which limitations such as erosion
(LCC) Land capability classification
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Deep, productive soils easily worked
class 1
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Productive soils on gentle slopes; moderate depth
class 2
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Soils of moderate fertility on moderately steep slopes
CLASS 3
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Good soils on steep slopes, subject to severe erosion; very severe risk of damage but may be cultivated if handled with great care
class 4
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Land is too wet or stony for cultivation
class 5
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Shallow soils on steep slopes; use for grazing and forestry
class 6
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Steep, rough, eroded land with shallow soils; also includes droughty or swampy land
class 7
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Very rough land; not suitable even for woodland or grazing;
CLASS 8
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Classes I-IV
denote for suitable cultivation
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CLASS 5-8
denote for unsuitable for cultivation
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This method of estimating soil loss
The Universal Soil Loss Equation (USLE)
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USLE FACTORS
R FACTOR K FACTOR LS FACTOR C FACTOR P FACTOR
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is a mathematical model used to predict the long-term average annual rate of soil erosion.
The Universal Soil Loss Equation (USLE)