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Chapter 3 Soil Erosion and Its Controls

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Chapter 3 Soil Erosion and Its Controls 3.1 Introduction Soil erosion is the detachment and removal of soil particles from the soil mass by water or wind. 3.1 ... – PowerPoint PPT presentation

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Title: Chapter 3 Soil Erosion and Its Controls


1
Chapter 3 Soil Erosion and Its Controls

2
3.1 Introduction
  • Soil erosion is the detachment and removal of
    soil particles from the soil mass by water or
    wind.

3
3.1 Introduction
  • Geologic erosion is the erosion under natural or
    undisturbed condition. It is called normal
    erosion or natural erosion also.
  • Accelerated erosion is the increased rate of
    erosion over the geologic erosion brought about
    by humans activity.

4
3.1 Introduction
  • Soil erosion rate is the gross amount of soil
    moved by water and wind.
  • Soil loss is the soil moved off a particular
    slope or field.
  • Sediment yield is soil loss delivered to a point
    under evaluation.
  • Kirkby, M.J. and R.P.C. Morgan. Edited. Soil
    Erosion, John Wiley Sons.

5
3.1 Introduction
  • Classification of erosion by eroding agents
  • Water erosion
  • Wind erosion

6
3.1 Introduction
  • Classification of erosion by action
  • Rain drops
  • Shallow flows
  • Concentrated flows

7
3.1 Introduction
  • Classification of erosion by form
  • Sheet erosion
  • Rill erosion
  • Gully erosion
  • Channel erosion

8
3.1 Introduction
  • Classification of erosion by location
  • Inter-rill erosion
  • Rill erosion

9
General classification of erosion
Inter-rill erosion Rill erosion Gully
erosion Channel erosion
  • Water
  • Wind
  • Gravity
  • Freezing and thawing erosion

Mass movement
10
3.2 Factors affecting erosion
  • Climate R
  • Soil K
  • Topography LS
  • Biological B
  • Engineering E
  • Tillage T

11
3.3 Measurement of soil erosion
  • Microplots 1cm2
  • Unit plot 6ft?72.6ft 0.01 acre
  • Large plots
  • Small watersheds
  • lt1000 km2
  • lt200 km2
  • lt50km2
  • Hydrological stations

12
3.4 Prediction of soil loss
  • Scientific farm planning for soil and water
    conservation requires knowledge of the relations
    between those factors that cause loss of soil and
    water and those that help reduce such losses.
  • Controlled studies on field plots and small
    watershed have supplied much valuable information.

13
3.4 Prediction of soil loss
  • Greatest benefits from such research can be
    realized only when the finding are converted to
    sound practice.
  • Specific guidelines are needed fro selecting the
    control practices.
  • The soil loss prediction procedure provides such
    guidelines.

14
3.5 Soil Loss Tolerances
  • The maximum level of soil erosion that
    will permit a high level of crop productivity to
    be sustained economically and indefinitely

15
3.6 Models of soil erosion
  • 1940, Zigg, A.W., Degree and length of land slope
    as it effects soil loss I runoff
  • 1965, Wischmeier, W.W., Universal soil loss
    equation
  • 1978, USLE
  • 1980, CREAMSChemicals, Runoff, and Erosion from
    Agricultural Management Systems
  • 1996, WEPPWater Erosion Prediction Project
  • 1997, RUSLERevised Universal Soil Loss Equation
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