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Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

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Surface Erosion and Surface Erosion and Control Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM
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Page 1: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Surface Erosion and ControlSurface Erosion and Control

Ali Fares, PhD

Watershed Hydrology, NREM662

UHM-CTAHR-NREM

Page 2: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Ia is all losses before runoff begins it includes:– water retained in surface

depressions,– Water interception by

vegetation– Evaporation and

infiltration.

Ia was found to follow: Ia = 0.2*S

S)(P

S)(PQ

2

*8.0

*2.0

Page 3: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Potential Maximum RetentionPotential Maximum Retention

S is related to the soil cover conditions of the watershed through the CN.

CN has a range of 0 to 100

10CN

1000S

Page 4: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.
Page 5: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Soil ErosionSoil Erosion

Page 6: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

What’s soil erosion?What’s soil erosion?

Erosion is the process of detachment and transport of soil particles by erosive agents (Ellison, 1944)

Erosion is a natural geologic process

WATER EROSION WIND EROSION TILLAGE TRANSLOCATION

Page 7: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

SOIL EROSION IS GLOBAL SOIL EROSION IS GLOBAL PROBLEMPROBLEM

1/3 WORLD’S ARABLE LAND LOST SINCE 1950 MOST IN ASIA, AFRICA, S. AMERICA

13-18 t/a/yr 30% OF US FARMLAND ABANDONED

EROSIONSALINIZATIONWATER-LOGGING

90% OF US CROPLAND LOSING SOIL FASTER THAN IT IS REPLACED>1 t/a/yr

PIMENTEL ET AL., 1995

Page 8: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

SIGNIFICANT SOIL LOSS IN THE USA

WATER3.5 X 109 T/yr

WIND1.5 X 109 T/yr

Page 9: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.
Page 10: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

WIND EROSIONWIND EROSION

WIND

CREEP

SUSPENSION

SALTATION

SALTATION DETACHES PARTICLES SMALLER PARTICLES SUSPENDED LARGER PARTICLES CREEP SANDY AND SILTY SOILS MOST SUSCEPTIBLE SOIL ACCUMULATION IN DITCHES AND FENCE ROWS

Page 11: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

WIND EROSION CAN BE SIGNIFICANT

Near Mitchell, SD

Page 12: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Dust bowl Dust bowl 1931-1939 there was a

drought called the “dust bowl”. It caused huge dust storms to erupt that destructed billions of acres of farm land.

Page 13: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

stormsstorms

In the first year of the drought there were 14 storms reported and the second year there were 38 storms. It was getting worse.

Page 14: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Ruined landRuined landTons of damage

was done to every ones land and it costs billions of dollars to repair the damages.

Page 15: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

Black SundayBlack SundayApril 14th,1934

black Sunday was the worst blizzard of the dustbowl which caused the most extensive damage.

Page 16: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.
Page 17: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

REDUCING WIND EROSIONREDUCING WIND EROSION

MAINTAIN SURFACE COVERCROP RESIDUECOVER CROPS

INCREASE STUBBLE HEIGHT INSTALL WINDBREAKS

EFFECTIVE 15x HEIGHT IRRIGATE STRIP CROPS PERPENDICULAR TO

PREVAILING WIND

Page 18: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

The Shelterbelt ProgramThe Shelterbelt Program

Page 19: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

WATER EROSION WATER EROSION PROCESSPROCESS

BEGINS WITH RAINDROPS STRIKING BARE SOIL DISLODGING PARTICLES

INTENSE RAINS SEAL SURFACE WHEN RAINFALL EXCEEDS

INFILTRATION WATER IS STORED IN SMALL DEPRESSIONS

ONCE DEPRESSIONS ARE FILLED, RUNOFF BEGINS

Page 20: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.
Page 21: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.
Page 22: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

WATER EROSIONWATER EROSION PROCESSPROCESSInitially water flows in a discontinuous

sheetEventually it concentrates into small

channels or rills. The runoff now has energy to break off particles and cut deeper

The amount of erosion caused by sheet and rill erosion increases with slope and distance

Rills may eventually form gullies

Page 23: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

THE SOIL WATER EROSION THE SOIL WATER EROSION PROCESSPROCESS

Page 24: Surface Erosion and Control Ali Fares, PhD Watershed Hydrology, NREM662 UHM-CTAHR-NREM.

EFFECTS ON ENVIRONMENTAL EFFECTS ON ENVIRONMENTAL QUALITY AND PRODUCTIVITYQUALITY AND PRODUCTIVITY

LOSS OF OM, CLAY, AND NUTRIENTS REDUCES PRODUCTIVITY

DAMAGE TO PLANTS

FORMATION OF RILLS AND GULLIES AFFECTS MANAGEMENT

SEDIMENTATION IN WATERWAYS, DIVERSIONS, TERRACES, DITCHES

DELIVERY OF NUTRIENTS TO SURFACE WATER


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