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Soil Formation
Soil is formed when parent material is weathered, transported and deposited
Parent material - original rocks that were broken down to form the basis of the soil
Weathering - mechanical breakdown of rock
Factors in Soil Formation
Type of parent material - rocks are broken down by wind and rain; soil tends to retain basic chemistry of these rock
Climate - average temperature and moisture change rate of weathering and leaching(nutrients in water), wind redistribution as well
Topography - slope of the land may affect erosion
Biological factors - plants, animals, microorganisms
Time - soil formation is continuous, there’s no end
Soil profile (soil horizons)
Overtime, soil layers build up and from common layers
These are known as soil horizons, or soil profile
Organic matter
Surface horizon (rock and humus (organic material)
Subsoil
Substrata (most parent material)
Bedrock
Soil Erosion
Overtime, soil erodes due to several factors
Water
Wind
Gravity
Human factors
Leads to water contamination
Human Factors - Agriculture and Soil Erosion
First problem: Deforestation - The lack of roots holding down soil
They are often replaced with plants that worsen erosion, ex. soybean and wheat
Second problem: Overgrazing - Pastureland can lead to cattle overeating and the top layer of soil can erode with wind and rain
Third problem: Pesticides and fertilizers - These can change chemistry of soil and kill microorganisms in the soil
Fourth problem: Tillage practices: Turning and breaking up soil keeps top layer from accumulating organic material and roots
Erosion of Soil into Water
Sheet Erosion - surface layer is removed by water
Solution: Maintain plant cover
Rill Erosion - small channels of water flow
Solution: Strip cropping or contour plowing
Gully Erosion - Wider cuts from expanded rill erosion
Solution: Divert water away from rills and gullies
Erosion’s Effect on Watersheds
USDA Study on Watersheds
Study on thousands of watersheds
Public and private lands
Farm fields all over US
Sheet and Rill Erosion