Lecture 7: Soil System Notes
Definitions of Soil
- Soil is a dynamic, three-dimensional natural body on the Earth's surface where plants grow.
- It consists of minerals, organic material, living organisms, water, and air.
- Soil properties develop due to the integrated effects of climate, topography, and living organisms acting upon parent material.
Function of Soil
- Plant Growth Medium: Soil provides physical support and supplies water and nutrients to plants.
- Habitat for Organisms: It hosts a diverse community of organisms, including bacteria, fungi, invertebrates, and vertebrates, essential for decomposition and nutrient cycling.
- Environmental Interactions: Soil interacts with climate, atmosphere, and the broader environment.
- Buffering System: Soil can resist changes in its properties and overcome drastic changes, acting as a buffer for pH and ionic composition.
- Influence on Vegetation: Soil influences the types of crops and weeds that can grow.
Soil Components
- Four major phases:
- Solid
- Liquid
- Gases
- Living components
Soil Phase (Solid)
- Composed of mineral particles (from rocks) and organic matter.
- Makes up 50% or more of the soil volume.
- Organic matter typically comprises 0.5 to 6% of soil volume.
Liquid Phase (Soil Solution)
- Primarily water, occupying 10-50% of soil volume.
- Contains dissolved minerals and organic substances.
- Supplies water and nutrients to plants.
Gases Phase
- Primarily air, occupying 10-50% of soil volume.
- Fills pore space not occupied by water.
- Adequate air (oxygen) is essential for aerobic microorganisms and plant roots.
Colloidal Components
- Very small particles, mainly clay and organic matter.
- High surface area and negative charge.
- Critical for the soil's ability to hold and exchange positively charged ions (cations), influencing nutrient availability.
Living Components
- Diverse community of organisms such as bacteria, fungi, invertebrates, and vertebrates.
- Play crucial roles in soil health and function.
Texture
- Soil texture is defined by the relative proportion of mineral particle sizes: sand, silt, and clay.
- These particles are sorted into size classes.
- The specific combination of sand, silt, and clay percentages determines the soil texture class, which can be visualized using a standard soil texture triangle.
- Texture can be broadly categorized as:
- Coarse (sandy)
- Fine (clay)
- Medium (loam): a mixture of sand, silt, and clay.
Soil Characteristics
- Soil properties differ significantly from one soil to another.
- Texture
- Structure
- Aggregate stability
- Porosity
- Water holding capacity
- Aeration
- Nutrient holding capacity
- Cation exchange capacity (CEC), largely influenced by colloidal clay and organic matter, is a crucial characteristic affecting the soil's ability to retain and exchange cations, which are often essential nutrients.
- Organic matter significantly enhances CEC.
- Soil also responds to climate, topography, and natural vegetation.
- Soil biota activity is influenced by moisture, aeration, temperature, and organic matter.
- As a buffered system, soil resists changes in pH and ionic composition.
Soil and Weeds
- Soil conditions play a significant role in determining the success and composition of weed populations.
- Factors such as moisture, aeration, fertility level, and pH influence weed growth.
- Some weeds can serve as indicators of specific soil conditions, such as saline or acidic soil.
- Weeds can adapt and thrive in soil conditions that might be unsuitable for crops.
- Certain invasive weeds have the capacity to alter soil properties.
- Weed control practices have a major impact on the soil system.
- Tillage: A common method that physically disturbs the soil, affecting soil structure, erosion, and the distribution of weed seeds within the soil profile.
- No-Tillage Systems: Minimize soil disturbance, altering weed populations and species composition compared to tilled systems, often relying more on herbicides.
- Surface soil conditions, which are affected by weed control methods, can influence weed seed germination.