2f. Soil Erosion and Conservation
Geologic Erosion
process that transforms soil into sediment
takes place naturally without the influence of human activities
geologic erosion is greatest in semiarid regions
rain is not enough to be damaging
not enough to support plant life that would have protected the soil
Accelerated Erosion
occurs when people disturb the soil or the natural vegetation by:
overgrazing lovestock
cutting forests
plowing hillsides
tearing up land for construction projects
can be 10 to 1000 times as destructive as geologic erosion
erosion rates
US: avg on cropland is 12 Mg/ha (5.4 tons/ac)
7 Mg/ha (3.1 tons/ac) by water
5 Mg/ha (2.2 tons/ac) by wind
cultivated soils in africa and asia can be 10 times that
Effect of raindrops
bigger raindrops are more erosive
faster, more energy at point of impact
splash
moves soil in all directions
if on a slope, more soil splashes downhill
net movement of soil downslope
raindrops are more important than running water
if soil is covered and protected, its less likely to move
sheet erosion
splashed soil is moved uniformly
columns of soil remain where pebbles protected soil from raindrop impacts
rill erosion
running water gathers into small channels due to irregularities on the soil surface
those channels incise into the soil surface
can be smoothed by tillage, but damage is already done
location of rills is random
interrill erosion
sheet erosion that takes place between rills
gully erosion
rill erosion that cannot be smoothed by tillage equipment
ephemeral gullies
similar concept to “ephemeral stream”
follows the slope
similar to rill erosion
can be smoothed by tillage
different from rill erosion
not random, always occurs in same location
if not managed, can cause permanent damage
conservation practices
contour cropping
pool water
contour strip-cropping
both slow flow of runoff
terraces
shorten length of slope
grassed waterways
slow runoff
conservation tillage - no till