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Class 13b: Soils (pedology)
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What is soil? Not just dirt
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Soil components Parent material: Temperature and moisture
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Soil formation Bedrock breaks apart into regolith
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Classifying soils: color Color tells you about chemistry
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Classifying soils: texture Size, organization of particles
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Classifying soils: texture
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Classifying soils: structure Arrangement of soil particles
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Classifying soils: structure Porosity: Permeability:
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Soil moisture
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Soil-water balance Warmer temperatures: higher ET Higher precipitation: higher percolation
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Soil profiles
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Soil classification More complicated than climate
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Entisols Relativey new: most recent soils
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Oxisols Old soils; minerals except oxides leached out
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Aridisols Found in arid environments
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Mollisols Most productive soil
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Alfisols Significant aluminum (Al) and iron (Fe)
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Spodosols Most acidic soil; minerals leached to lower horizon
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Soil degradation Forms in 500 years, but can disappear in one
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Soil degradation
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Salinization: salty soil
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