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Soil Erosion and
Conservation
“Erosion”
• a natural leveling process that wears down
high places; fills in low places
• agents: running water, ice, wind, gravity,
waves
“accelerated erosion”
• Process by which soil particles are
removed, transported and deposited;
rate of removal of soil greater than rate
of formation
• 500 yrs / inch topsoil
– Caused by removal of vegetation
• agents: wind, water
• Deposition or sedimentation is flip side
of erosion.
• the soil that is removed has to go somewhere:
wetlands, lakes, streams, atmosphere
Worldwide
75 billion metric tons soil lost / year
(predominantly cropland)
80% cropland: moderate - severe erosion
10% cropland: slight - moderate erosion
highest rates in Asia, Africa, South America
Short History of Agriculture
Post WWII:
– Increase in chemical/mechanical intensive
production practices
• Decrease in number of farms
• Increase in size of farms
– Production of commodities/export crops
• Top 5 commodities (2003)
– Cattle, dairy, corn, soybeans, broilers
– Cheap food policy
• Over-production, cost-price squeeze,
consolidation of farms
Farm Crisis
Since 1980’s
• Falling prices
• Spiraling overproduction
• Bankruptcies, foreclosures
1. Water erosion
a. rainsplash erosion
• Raindrops accelerate as fall until they
reach speed at which friction balances
gravity
– for large raindrops: 30 km / hr
– transfer kinetic energy to soil:
• detach soil
• destroy structure
• transport soil (as much as 0.7 m vertically and 2
m horizontally)
• Only in intense rain events; soil stays local
b. sheet erosion
Water flows smoothly in a thin film over
surface; detached soil moves with the
water
c. rill erosion
• Sheet flow concentrates water into
channels
d. gully erosion
• Water cuts deeper into soil, rills
coalesce into deep troughs
• cannot (easily) be removed by tillage
• most dramatic, but most soil loss is due
to sheet and rill erosion
Universal Soil Loss Equation
(USLE)
A = RKLSCP
R : rainfall erosivity (intensity, quantity)
K : soil erodibility (erosion rate per unit of R; in Soil
Survey)
L : slope length
S : slope gradient
C : cover and management (ratio of soil loss compared
to fallow)
P : erosion-control practices
2. Wind erosion
• Arid and semi-arid climates
• Dry soil; loss of structure; wind can
remove soil particles
• Damage is on-site and off-site
• Smallest detach into suspension
(<0.1 mm)
• medium move by saltation
(0.1 - 0.5 mm)
• large move by rolling and sliding (creep)
> 0.5 mm
Wind Erosion Model (WEQ)
E = ƒ( ICKLV)
I : soil erodibility (slope angle, soil moisture,
structural stability)
C : climate factor (wind speed , soil temp.,
ppt.)
K : roughness factor
L : width of field factor
V : vegetative cover
35 mph wind
loess
Soil Conservation Measures
US gov’t response to Great Dust Bowl:
1. SES---SCS---NRCS
2. 3000 Soil and Water Conservation
Districts
3. Shelterbelt Program
218 million trees
Prevention practices:
1. Windbreaks
Plant trees on windward side of crops
30 mph --> 13 mph
Senegal
2. Contour plowing
Cultivate with the contour of the slope
(rather than parallel to it); lessens water
runoff
3. Strip cropping
Plant strips of alternating crops.
(Contour strip cropping)
4. Terracing
on sloping land ; to check water flow
Inca
Bolivia
5. Reclamation of gullies
build dams (manure and straw, concrete,
stones, sticks) to collect silt; plant gully
6. Cover crops or surface mulch
(in orchards or vineyards)
protects ground surface between rows or
during non-growing season
6. Conservation tillage
eliminates or restricts tilling
• In traditional tilling,
surface soil is
inverted,
• plant residue buried
• bare soil exposed
In conservation tillage:
· leave plant residue on at least 30% of
surface
No-till:
no plowing, seeds are
planted in narrow
slits or directly
drilled into holes
17.5% US cropland in
2000
increases need for
herbicide
Conservation methods in construction:
• schedule during low rain
• work one area at a time
• cover soil immediately (vegetation,
straw,etc)
• control runoff to prevent gullies
• trap sediment
Open-top culvert on logging road
lead runoff water off of road
Sedimentation pond
Catch sediment
bioengineering
Riprap channel
guide runoff, prevent gullies, reduce soil
loss
6.soil erosion By Allah Dad Khan

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6.soil erosion By Allah Dad Khan

  • 1.
  • 3. “Erosion” • a natural leveling process that wears down high places; fills in low places • agents: running water, ice, wind, gravity, waves
  • 4. “accelerated erosion” • Process by which soil particles are removed, transported and deposited; rate of removal of soil greater than rate of formation • 500 yrs / inch topsoil – Caused by removal of vegetation • agents: wind, water
  • 5. • Deposition or sedimentation is flip side of erosion. • the soil that is removed has to go somewhere: wetlands, lakes, streams, atmosphere
  • 6.
  • 7. Worldwide 75 billion metric tons soil lost / year (predominantly cropland) 80% cropland: moderate - severe erosion 10% cropland: slight - moderate erosion highest rates in Asia, Africa, South America
  • 8. Short History of Agriculture Post WWII: – Increase in chemical/mechanical intensive production practices • Decrease in number of farms • Increase in size of farms – Production of commodities/export crops • Top 5 commodities (2003) – Cattle, dairy, corn, soybeans, broilers – Cheap food policy • Over-production, cost-price squeeze, consolidation of farms
  • 9. Farm Crisis Since 1980’s • Falling prices • Spiraling overproduction • Bankruptcies, foreclosures
  • 10.
  • 11. 1. Water erosion a. rainsplash erosion • Raindrops accelerate as fall until they reach speed at which friction balances gravity – for large raindrops: 30 km / hr – transfer kinetic energy to soil: • detach soil • destroy structure • transport soil (as much as 0.7 m vertically and 2 m horizontally) • Only in intense rain events; soil stays local
  • 12.
  • 13. b. sheet erosion Water flows smoothly in a thin film over surface; detached soil moves with the water
  • 14.
  • 15.
  • 16.
  • 17. c. rill erosion • Sheet flow concentrates water into channels
  • 18.
  • 19.
  • 20.
  • 21.
  • 22. d. gully erosion • Water cuts deeper into soil, rills coalesce into deep troughs • cannot (easily) be removed by tillage • most dramatic, but most soil loss is due to sheet and rill erosion
  • 23.
  • 24.
  • 25.
  • 26.
  • 27.
  • 28.
  • 29. Universal Soil Loss Equation (USLE) A = RKLSCP R : rainfall erosivity (intensity, quantity) K : soil erodibility (erosion rate per unit of R; in Soil Survey) L : slope length S : slope gradient C : cover and management (ratio of soil loss compared to fallow) P : erosion-control practices
  • 30. 2. Wind erosion • Arid and semi-arid climates • Dry soil; loss of structure; wind can remove soil particles • Damage is on-site and off-site
  • 31. • Smallest detach into suspension (<0.1 mm) • medium move by saltation (0.1 - 0.5 mm) • large move by rolling and sliding (creep) > 0.5 mm
  • 32.
  • 33. Wind Erosion Model (WEQ) E = ƒ( ICKLV) I : soil erodibility (slope angle, soil moisture, structural stability) C : climate factor (wind speed , soil temp., ppt.) K : roughness factor L : width of field factor V : vegetative cover
  • 34.
  • 35.
  • 36.
  • 37.
  • 38.
  • 40. loess
  • 41. Soil Conservation Measures US gov’t response to Great Dust Bowl: 1. SES---SCS---NRCS 2. 3000 Soil and Water Conservation Districts 3. Shelterbelt Program 218 million trees
  • 42. Prevention practices: 1. Windbreaks Plant trees on windward side of crops 30 mph --> 13 mph
  • 43.
  • 44.
  • 45.
  • 47. 2. Contour plowing Cultivate with the contour of the slope (rather than parallel to it); lessens water runoff 3. Strip cropping Plant strips of alternating crops. (Contour strip cropping)
  • 48.
  • 49.
  • 50. 4. Terracing on sloping land ; to check water flow
  • 51.
  • 52. Inca
  • 53.
  • 55. 5. Reclamation of gullies build dams (manure and straw, concrete, stones, sticks) to collect silt; plant gully
  • 56.
  • 57.
  • 58. 6. Cover crops or surface mulch (in orchards or vineyards) protects ground surface between rows or during non-growing season
  • 59. 6. Conservation tillage eliminates or restricts tilling
  • 60. • In traditional tilling, surface soil is inverted, • plant residue buried • bare soil exposed
  • 61. In conservation tillage: · leave plant residue on at least 30% of surface
  • 62. No-till: no plowing, seeds are planted in narrow slits or directly drilled into holes 17.5% US cropland in 2000 increases need for herbicide
  • 63. Conservation methods in construction: • schedule during low rain • work one area at a time • cover soil immediately (vegetation, straw,etc) • control runoff to prevent gullies • trap sediment
  • 64. Open-top culvert on logging road lead runoff water off of road
  • 68. Riprap channel guide runoff, prevent gullies, reduce soil loss

Editor's Notes

  1. Show Future of Food clip here about chemicals and food More info on Future of Food Commodity: Value added