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Soil Erosion andSoil Erosion and
DegradationDegradation
Nature Is Speaking –
Edward Norton is The Soil
SOIL: A RENEWABLE RESOURCESOIL: A RENEWABLE RESOURCE
TopsoilTopsoil – fertile top few inches that supports– fertile top few inches that supports
agriculture – slowly renewableagriculture – slowly renewable
LoamLoam – texture best suited for plant growth– texture best suited for plant growth
SOIL: A RENEWABLE RESOURCESOIL: A RENEWABLE RESOURCE
SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION
 Soil erosionSoil erosion – movement of soil components– movement of soil components
– especially surface litter and topsoil – from– especially surface litter and topsoil – from
one place to another by wind or waterone place to another by wind or water

Lowers soil fertilityLowers soil fertility

Can overload nearby waterbodies with sedimentCan overload nearby waterbodies with sediment
SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION
 Plant roots anchor soilsPlant roots anchor soils
 Destroyed through:Destroyed through:

FarmingFarming

LoggingLogging

ConstructionConstruction

OvergrazingOvergrazing

Off road vehiclesOff road vehicles
SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION
 Sheet erosionSheet erosion – surface water or wind peel off– surface water or wind peel off
thin layers of soil – not always noticeablethin layers of soil – not always noticeable
 Rill erosionRill erosion – fast-flowing little rivulets of– fast-flowing little rivulets of
surface water make small channelssurface water make small channels
 Gully erosionGully erosion – fast-flowing water join together– fast-flowing water join together
to cut wider and deeper ditches or gulliesto cut wider and deeper ditches or gullies
Global Outlook: Soil ErosionGlobal Outlook: Soil Erosion
 Soil is eroding faster than it is forming on moreSoil is eroding faster than it is forming on more
than one-third of the world’s croplandthan one-third of the world’s cropland
Case Study: Soil Erosion in the U.S. –Case Study: Soil Erosion in the U.S. –
Some Hopeful SignsSome Hopeful Signs
 Soil erosion > formation on most U.S. croplandSoil erosion > formation on most U.S. cropland

Since 1985 – cut by 40%Since 1985 – cut by 40%

1985 Food Security Act (Farm Act) – farmers1985 Food Security Act (Farm Act) – farmers
receive a subsidy for taking highly erodible landreceive a subsidy for taking highly erodible land
out of production and replanting it with soil savingout of production and replanting it with soil saving
plants for 10-15 yearsplants for 10-15 years
Desertification: Degrading DrylandsDesertification: Degrading Drylands
 DesertificationDesertification - process by which fertile- process by which fertile
land becomes desert, typically as a result ofland becomes desert, typically as a result of
drought, deforestation or inappropriate ag.drought, deforestation or inappropriate ag.
 1/3 of world’s land has lost some productivity1/3 of world’s land has lost some productivity
because of drought and human activities thatbecause of drought and human activities that
reduce or degrade topsoilreduce or degrade topsoil
Figure 13-12Figure 13-12
Fig. 13-11, p. 280
Very severeSevereModerate
Desertification around the world
Case Study: The Dust BowlCase Study: The Dust Bowl
 U.S. Plains – 1930s – most topsoil lost –U.S. Plains – 1930s – most topsoil lost –
poor soil practices and drought (1926 -1937)poor soil practices and drought (1926 -1937)

Plowing, left bare, overgrazingPlowing, left bare, overgrazing

Dust stormsDust storms

Farmers migrated – no jobs – Great DepressionFarmers migrated – no jobs – Great Depression
Case Study: The Dust BowlCase Study: The Dust Bowl
 1935 –1935 – Soil Erosion ActSoil Erosion Act – established– established SoilSoil
Conservation ServiceConservation Service (part of USDA- now(part of USDA- now
Natural Resources Conservation ServiceNatural Resources Conservation Service))

Local soil conservation districts set upLocal soil conservation districts set up
 1985 –1985 – Conservation Reserve ProgramConservation Reserve Program ––
part ofpart of Farm ActFarm Act – paid farmers to cover– paid farmers to cover
highly erodible landhighly erodible land
Salinization &Salinization &
WaterloggingWaterlogging
 RepeatedRepeated
irrigation canirrigation can
reduce cropreduce crop
yields byyields by
causingcausing
salinizationsalinization
(salt buildup) in(salt buildup) in
the soil andthe soil and
waterloggingwaterlogging
of crop plantsof crop plants
Figure 13-13Figure 13-13
Fig. 13-15, p. 281
CleanupPrevention
Soil Salinization
Solutions
Reduce irrigation
Switch to salt-
tolerant crops
(such as barley,
cotton,
sugarbeet)
Flush soil
(expensive and
wastes water)
Stop growing crops
for 2–5 years
Install underground
drainage systems
(expensive)
Salinization and Waterlogging ofSalinization and Waterlogging of
Soils: A Downside of IrrigationSoils: A Downside of Irrigation
 Example of highExample of high
evaporation,evaporation,
poor drainage,poor drainage,
and severeand severe
salinizationsalinization
 White alkalineWhite alkaline
salts havesalts have
displaced cropsdisplaced crops
Desertification

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Soil erosion and degradation lecture 2016-17

  • 1. Soil Erosion andSoil Erosion and DegradationDegradation
  • 2. Nature Is Speaking – Edward Norton is The Soil
  • 3. SOIL: A RENEWABLE RESOURCESOIL: A RENEWABLE RESOURCE TopsoilTopsoil – fertile top few inches that supports– fertile top few inches that supports agriculture – slowly renewableagriculture – slowly renewable
  • 4. LoamLoam – texture best suited for plant growth– texture best suited for plant growth SOIL: A RENEWABLE RESOURCESOIL: A RENEWABLE RESOURCE
  • 5. SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION  Soil erosionSoil erosion – movement of soil components– movement of soil components – especially surface litter and topsoil – from– especially surface litter and topsoil – from one place to another by wind or waterone place to another by wind or water  Lowers soil fertilityLowers soil fertility  Can overload nearby waterbodies with sedimentCan overload nearby waterbodies with sediment
  • 6. SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION  Plant roots anchor soilsPlant roots anchor soils  Destroyed through:Destroyed through:  FarmingFarming  LoggingLogging  ConstructionConstruction  OvergrazingOvergrazing  Off road vehiclesOff road vehicles
  • 7. SOIL EROSION AND DEGRADATIONSOIL EROSION AND DEGRADATION  Sheet erosionSheet erosion – surface water or wind peel off– surface water or wind peel off thin layers of soil – not always noticeablethin layers of soil – not always noticeable  Rill erosionRill erosion – fast-flowing little rivulets of– fast-flowing little rivulets of surface water make small channelssurface water make small channels  Gully erosionGully erosion – fast-flowing water join together– fast-flowing water join together to cut wider and deeper ditches or gulliesto cut wider and deeper ditches or gullies
  • 8. Global Outlook: Soil ErosionGlobal Outlook: Soil Erosion  Soil is eroding faster than it is forming on moreSoil is eroding faster than it is forming on more than one-third of the world’s croplandthan one-third of the world’s cropland
  • 9. Case Study: Soil Erosion in the U.S. –Case Study: Soil Erosion in the U.S. – Some Hopeful SignsSome Hopeful Signs  Soil erosion > formation on most U.S. croplandSoil erosion > formation on most U.S. cropland  Since 1985 – cut by 40%Since 1985 – cut by 40%  1985 Food Security Act (Farm Act) – farmers1985 Food Security Act (Farm Act) – farmers receive a subsidy for taking highly erodible landreceive a subsidy for taking highly erodible land out of production and replanting it with soil savingout of production and replanting it with soil saving plants for 10-15 yearsplants for 10-15 years
  • 10. Desertification: Degrading DrylandsDesertification: Degrading Drylands  DesertificationDesertification - process by which fertile- process by which fertile land becomes desert, typically as a result ofland becomes desert, typically as a result of drought, deforestation or inappropriate ag.drought, deforestation or inappropriate ag.  1/3 of world’s land has lost some productivity1/3 of world’s land has lost some productivity because of drought and human activities thatbecause of drought and human activities that reduce or degrade topsoilreduce or degrade topsoil Figure 13-12Figure 13-12
  • 11. Fig. 13-11, p. 280 Very severeSevereModerate Desertification around the world
  • 12. Case Study: The Dust BowlCase Study: The Dust Bowl  U.S. Plains – 1930s – most topsoil lost –U.S. Plains – 1930s – most topsoil lost – poor soil practices and drought (1926 -1937)poor soil practices and drought (1926 -1937)  Plowing, left bare, overgrazingPlowing, left bare, overgrazing  Dust stormsDust storms  Farmers migrated – no jobs – Great DepressionFarmers migrated – no jobs – Great Depression
  • 13. Case Study: The Dust BowlCase Study: The Dust Bowl  1935 –1935 – Soil Erosion ActSoil Erosion Act – established– established SoilSoil Conservation ServiceConservation Service (part of USDA- now(part of USDA- now Natural Resources Conservation ServiceNatural Resources Conservation Service))  Local soil conservation districts set upLocal soil conservation districts set up  1985 –1985 – Conservation Reserve ProgramConservation Reserve Program –– part ofpart of Farm ActFarm Act – paid farmers to cover– paid farmers to cover highly erodible landhighly erodible land
  • 14. Salinization &Salinization & WaterloggingWaterlogging  RepeatedRepeated irrigation canirrigation can reduce cropreduce crop yields byyields by causingcausing salinizationsalinization (salt buildup) in(salt buildup) in the soil andthe soil and waterloggingwaterlogging of crop plantsof crop plants Figure 13-13Figure 13-13
  • 15. Fig. 13-15, p. 281 CleanupPrevention Soil Salinization Solutions Reduce irrigation Switch to salt- tolerant crops (such as barley, cotton, sugarbeet) Flush soil (expensive and wastes water) Stop growing crops for 2–5 years Install underground drainage systems (expensive)
  • 16. Salinization and Waterlogging ofSalinization and Waterlogging of Soils: A Downside of IrrigationSoils: A Downside of Irrigation  Example of highExample of high evaporation,evaporation, poor drainage,poor drainage, and severeand severe salinizationsalinization  White alkalineWhite alkaline salts havesalts have displaced cropsdisplaced crops

Editor's Notes

  1. Figure 13.11 Natural capital degradation: desertification of arid and semiarid lands is caused by a combination of prolonged drought and human activities that expose soil to erosion. QUESTION: What three things would you do to reduce desertification? (Data from UN Environment Programme and Harold E. Drengue)
  2. Figure 13.15 Solutions: methods for preventing and cleaning up soil salinization. QUESTION: Which two of these solutions do you think are the most important?