Soils+and+Soil+Testing
Soils and Soil Testing
Phases of Soils
Solid: Clay, silt, sand, organic matter
Liquid: Soil water, dissolved minerals
Gas: Soil air (N2, O2, CO2)
Particle Sizes and Characteristics
Sand: Adds porosity
Silt: Adds body to the soil
Clay: Adds chemical & physical properties
Soil Texture Comparison
Characteristics
Sand
Ability to Compact: Low
Air Space: High
Soil Fertility: Low
Water-Holding Capacity: Low
Workability: High
Silt
Ability to Compact: Moderate
Air Space: Moderate-High
Soil Fertility: Moderate-High
Water-Holding Capacity: Moderate-High
Workability: Moderate-High
Clay
Ability to Compact: High
Air Space: Low
Soil Fertility: Moderate-High
Water-Holding Capacity: High
Workability: Low
Soil Formation
Horizons:
O horizon: Loose & partly decayed organic matter
A horizon: Mineral matter mixed with humus
E horizon: Zone of eluviation
B horizon: Accumulation of clay transported from above
C horizon: Partially altered parent material
Parent Material: Unweathered material
Soil Texture vs. Soil Structure
Soil Texture: Composition based on particle size (% sand, silt, clay)
Soil Structure: Arrangement of soil particles, pores, and aggregates
Soil Testing and Fertility
Sample ID and Parameters:
Soil pH, Lime Requirement Index
Macronutrients: Phosphorus, Potassium, Magnesium, Calcium
Micronutrients: Zinc, Copper, Manganese, Boron, Iron
Estimated Cation Exchange Capacity (CEC) and Base Saturation
Importance of Soil pH
pH affects nutrient availability and soil health
pH Adjustments: Use of limestone to neutralize acidity
Summary
Soil consists of mineral (sand, silt, clay) and organic matter
Components aggregate to create soil structure
Soil testing provides essential information on mineral nutrients for plant health