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Earth Science Unit 1.4: Weathering and Soils. The Rock Cycle. Weathering The breakdown of rock near the surface due to surface processes, such as:. Chemical Alteration Solution & leaching of water Biological action Hydration Mechanical Impact
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WeatheringThe breakdown of rock near the surface due to surface processes, such as: Chemical Alteration • Solution & leaching of water • Biological action • Hydration Mechanical • Impact • Wedging: Frost, Plant Roots, Salt Crystal Growth, Expansion of Hydrated Minerals
Mass-WastingMovement of Large Amounts of Material Downhill under Gravity • Creep • Mudflows • Slump • Rockfalls • Avalanches
What Determines Soil Type • Climate • Vegetation • Drainage • Time • Parent Material • Residual - Transported • Least Important Factor for Mature Soils
Soil Formation Processes Leaching from Surface • K, Mg, Na • Ca • Si • Al, Fe Accumulation beneath Surface • Al, Fe in Humid Climates • Ca in Arid Climates
Soil Horizons and Profiles Soil Horizons • Layers in Soil • Not Deposited, but Zones of Chemical Action Soil Profile • Suite of Layers at a Given Locality
Principal Soil Horizons • O - Organic (Humus) Often Absent • A – Leaching (Clay Removed) • E - Bleached Zone - Only in Certain Soils • B – Accumulation • Absent in Young Soils • Distinct in Old Soils • Al, Fe, Clay (Moist) • Si, Ca (Arid) • C - Parent Material (bedrock)
This may be the most difficult classification problem in science because of the many factors involved. Varied Bases for Classification Parent Material Special Constituent Materials Maturity Structure Climate & Vegetation Multiple Objectives Scientific Genesis & Evolution Agricultural Fertility Most Effective Use Engineering Slope Stability Expansion and Shrinkage Stability of Excavations Soil Classification
"The 7th Approximation" • U.S. Soil Conservation Service • 12 Soil Orders