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
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
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
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
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)
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