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Physical Environment
8. Soil
Soil erosion
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Created by
Maddie Clayton
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Cards (13)
Soil
formation
and soil
erosion
are in
dynamic
equilibrium
Soil formation:
Rocks
->
regolith
->
Soil
Organic matter
->
humus
->
Soil
Soil
=
regolith
+
humus
+
air
+
water
+
biota
Vegetation
Vegetation increases
interception
which reduces the
kinetic energy
of the
raindrops
, reducing
rainsplash.
Vegetation
root binds
the soil, keeping it
together
and reducing
erosion.
It acts as a
windbreak
that reduces
wind blow
It adds
dead organic matter
to the soil, increasing soil
formation
Vegetation means
leaf litter
which reduces
rainsplash
and adds
humus
to the soil
High infiltration rates
High infiltration rates
decreases
surface run-off
because water does not
build up
on the surface
Soil organic matter
Soil organic matter
takes in
water
which decreases
surface run-off.
It also
holds
soil together.
Environmental impacts:
Loss of
nutrients
-
washed
or
blown
away means decreased
fertility
and decreased
crop growth
Desertification
- Global climate change means
low rainfall
, soil
erodes
to the point where it can't hold
water
- no
plants
can grow
Air pollution
-
atmospheric particulates
cause
diming
, decreasing
photosynthesis
and causing
respiratory issues
Turbidity
increases -
murky
+
dark
water decreases
photosynthesis
and increases
water treatment
required.
Sediment
builds up =
flooding
Flooding
- rivers
overflow
and
banks
are
eroded
Landslides
-
subsidence
and
collapsing
of soil
Human impacts on soil erosion:
vegetation removal
-
deforestation
Overgrazing
- too many/much
livestock
Ploughing
- breaks up
peds
Reducing soil biota
- via
pesticides
Soil compaction
-
livestock
and
machinery
Cultivating steep slopes
Human impacts on soil erosion
Vegetation removal:
e.g
deforestation
for
building
materials,
farmland
or
mineral mines
Decreased interception
soil
exposed to increased
rainsplash.
decreased
infiltration
=
increased runoff.
decreased
wind barriers
=
increased wind blow
Decreased
root binding
the soil =
increased erosion
Decreased
leaf litter
=
decreased soil formation
Human impacts on soil erosion
Overgrazing:
e.g too many/much
livestock
eating
at a rate that doesn't allow
vegetation
to
recover
This leads to decreased
vegetation
decreased
interception
=
increased rainsplash
decreased
root binding
=
increased erosion
decreased
windbreaks
=
increased wind blow
decreased
leaf litter
=
decreased soil formation
Human impacts on soil erosion
Ploughing:
Breaking up peds
Soil is
less dense
so it is easily
carried away
by
wind blow
and
surface run-off
Human impacts on soil erosion
Reducing soil biota:
Pesticides
kill
biota
Decreased
decomposition
= decreased
soil formation
Decreased
earthworms
= decreased
aeration
of soil = decreased
infiltration
=
increased surface run-off
Human impacts on soil erosion
Soil compaction:
Due to
heavy machinery
and
livestock
around a
waterhole
Decreased
gaps
in the soil = decreased
infiltration
=
increased surface run-off
Human impacts on soil erosion
Cultivation steep slopes:
Gravity
increases
surface run-off
Increased
ploughing
/
compaction
/
overgrazing
/ or
decreased vegetation
=
increased wind blow