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Published byArleen Palmer Modified over 8 years ago
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Soil Basics AP Environmental Science
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SOIL ≠ DIRT
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What is soil? a complex mixture of organic and inorganic components full of living organisms whose actions help keep it fertile (can be considered its own ecosystem)
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Composition of Good Quality Soil
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Soil Formation 1.weathering – processes that break down rocks, turning large particles into smaller particles a. physical weathering- rain and wind b. chemical weathering- water or other substances interact with parent material c. biological weathering- rock broken apart by living organisms 2. erosion – movement of soil from one area to another 3.deposition and decomposition of organic matter
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Five Factors Impacting Soil Formation 1. Climate: temperature and rain (ie: soil forms quicker in warm environments) 2. Organisms: Activity of earthworms, plants, etc. mix soil and add organic matter 3. Topographical relief: The effects of hills and valleys (ie: steep slopes have more runoff and erosion and less leaching and accumulation of organics) 4. Parent material: Type of rock influences soil properties 5. Time: Forming soil takes time; all the factors above change over time
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Soil Horizons O horizon: organic or litter layer A horizon: inorganic mineral components and humus (topsoil) E horizon: loses some minerals and organic material through leaching B horizon: collects and accumulates minerals from above C horizon: weathered parent material R horizon: unaltered parent material
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Soil Texture ParticleDiameter Sand0.05 – 2 mm Silt0.002 – 0.05 mm Clayless than 0.002 mm Loam: relatively even mixture of three particle sizes
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Soil Triangle
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Soil Texture by Fractionation
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