Soil Study Notes
Harvesting Impact on Soil
- Mechanical Harvesting Effects:
- Bulk Density (B.D.) measurements from various harvesting methods:
- No mechanical harvest:
- Number of fields: 24, B.D.: 1.49 g/cc
- 1 mechanical harvest:
- Number of fields: 14, B.D.: 1.50 g/cc
- 2 mechanical harvests:
- Number of fields: 17, B.D.: 1.52 g/cc
- 3+ mechanical harvests:
- Number of fields: 34, B.D.: 1.60 g/cc
- Yield suppression noted with increasing B.D., affecting root penetration.
Soil Moisture
- Importance of Water in Soil:
- Vital for plant and microorganism life.
- Different soils have varying water retention capacities affecting:
- Plant health (too little results in wilting, too much results in oxygen deprivation).
- Key roles of water include:
- Promoting plant growth and nutrient availability
- Influencing soil erosion and structure (creates horizons).
Water Cycle Overview
- Hydrology studies the water cycle:
- Snow accumulation, precipitation, percolation, transpiration etc.
- Water moves through various stages: snowmelt, evaporation, groundwater discharge, etc.
Forces Holding Water in Soil
- Water retention driven by:
- Adhesion: Attraction between water molecules and soil particles
- Cohesion: Attraction among water molecules.
Soil Moisture Constants
- Field Capacity: Water retained after saturation, available for plant use.
- Moisture Equivalent: Water retention against centrifugal force.
- Permanent Wilting Percentage: Water remaining when plants wilt (1-15% range).
- Hygroscopic Coefficient: Bound water not accessible to plants.
Biological and Physical Classification of Soil Water
- Free Water: Excess water not held at field capacity, removed via drainage.
- Capillary Water: Held in soil pores between field capacity and hygroscopic coefficients, essential for plant use.
- Hygroscopic Water: Thin film around particles, not available to plants.
Water's Role in Plant Growth
- Plants require significant water content (approx. 80% of green weight).
- Osmosis: Water absorption through roots driven by concentration gradients.
- Mineral nutrients are carried along with water uptake.
- Crop Water Requirement:
- Water loss through evaporation and transpiration noted as evapotranspiration.
- Example: Water utilized for producing 1 kg of dry matter varies across crops (e.g., wheat: 452.7 kg water per kg dry matter).
Physical and Biological Properties of Soil Water
- K-Types of Water:
- Free/Drainage: excess water, easy leaching.
- Capillary: available for plants, essential nutrient transporter.
- Hygroscopic: held tightly, not available.
- Biologically Active:
- Water availability tightly linked to soil structure and health impacting nutrient cycling.
Cation Exchange Capacity (CEC)
- CEC reflects soil's ability to hold nutrients (cations) exchangeable at surfaces.
- Influenced by clay type, organic content, and pH levels.
- Key to maintaining fertility across soil types.
- Techniques for determining include various soil samples and estimates based on soil chemistry.
Soil Acidity and Fertility Management
- Acidity defined by free H+ concentration, critical for nutrient availability.
- Liming: process to raise pH and enhance nutrient uptake by altering exchange capacities.
- Soils present a range of pH preferences for optimal crop growth, affecting nutrient dynamics, particularly phosphorus.
Organic Matter in Soil
- Organic Matter Composition:
- Includes living organisms, decaying material, and humus.
- Functions of Organic Matter:
- Improves soil structure and aeration.
- Enhances water retention.
- Serves as a reservoir for nutrients.
- Supports the microbes that contribute to organic cycling and health of the ecosystem.
- Impacts on the soil carbon/nitrogen balance.
- Stability and Protection: Factors influencing decomposition rates and retention of OM.
Soil Fertility and Productivity
- Fertility vs. Productivity:
- Fertility: Nutrient provision capacity to sustain plant growth.
- Productivity: Actual output levels achieved in crop yields.
- Fundamental for agricultural practices to sustain soils for long-term cropping success.