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Soil Erosion by Water. AST 324 Carl E. Anderson. Chapter 6: Soil Erosion by Water: Learning Objectives. Understand the factors effecting the erosive force of flowing water Understand the factors effecting the forces resisting soil erosion
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Soil Erosion by Water AST 324 Carl E. Anderson
Chapter 6: Soil Erosion by Water: Learning Objectives • Understand the factors effecting the erosive force of flowing water • Understand the factors effecting the forces resisting soil erosion • Understand the basic procedures available for controlling soil erosion
Soil Erosion • The gradual wearing away of the land surface by running water, wind, ice, or other geological agents. • Erosion is a natural process which can’t be stopped completely. • Some natural ecosystems depend on a natural rate of erosion.
Accelerated ErosionCAUSED BY • Overgrazing range and pasture • Cultivation • Construction • Heavy traffic on bare slopes • Maximum when bare soil is exposed during periods of maximum rainfall.
SOIL EROSION PROCESSES • DETACHMENT • TRANSPORT
Forces Tending to Cause Soil Particle Detachment • Raindrop impact • Forces of flowing water • Abrasive action of other moving particles • Weathering • Animal and human actions • Burrowing • Tillage • Excavation
Soil Properties Tending to Resist Detachment • Adhesion • Cohesion • Binding forces of plant root systems • Protective coverings such as plant material
Forces Tending to Transport Soil Particles • Raindrop splash • Forces of flowing water • Wind movement • Gravity
Soil Properties Tending to Resist Transport • Inertia • High density • Large particle size
EFFECTS OF RAINDROPS ON SOIL EROSION • Break up soil aggregates into small particles • Compact the soil surface and thus increase surface runoff • Splash small soil particles down the slope • Increase the turbulence of overland flow and thus increase the transport capacity of the flow.
Erosion Control Methods • Reduce Forces of Fluid • Reduce Flow Velocity • Increase Forces Holding Soil • Increase Adhesion • Increase Plant Root Structure • Separate Soil From Flow • Pavement • Mulch • Residue
TYPES OF SOIL EROSION BY WATER • SHEET OR INTERRILL • RILL • GULLY • STREAMBANK
Soil Loss Tolerance The maximum level of soil erosion that will permit a high level of crop productivity to be maintained both economically and indefinitely.
SOIL EROSION UNITS • MASS PER UNIT AREA PER UNIT TIME • TONS PER ACRE PER YEAR • METRIC TONS PER HECTARE PER YEAR
NATURAL EROSION RATE • 1 TO 5 TONS / ACRE / YEAR • Erosion Rates in this Range are Sustainable Indefinitely. • 1 ton / ac / year = 163 years / inch soil loss
MAJOR FACTORS AFFECTING SOIL EROSION • Climate R • Soil K • Topography LS • Vegetation C • Conservation Practices P