SOIL –
The Fundamental Concepts
SOIL
- Geologic definition: Loose surface of the earth as distinguished from solid bedrock; support of plant life not required.
SOIL
- Traditional definition: Material which nourishes and supports growing plants; includes rocks, water, snow, air.
SOIL
Air 25%
Mineral Matter 45%
Water 25%
Organic Matter 5%
SOIL
- Component definition: Mixture of mineral matter, organic matter, water, and air.
- Example:
SOIL
- Soil Taxonomy definition: Collection of natural bodies of the earth’s surface, in places modified or even made by man or earthy materials, containing living matter and supporting or capable of supporting plants out of doors.
Its upper limit is air or shallow water and its lower limit is the depth to which soil weathering has been effective.
SOIL
- As a portion of the landscape: Collection of natural bodies occupying portions of the earth’s surface that support plants and that have properties due to the integrated effect of climate and living matter, acting upon parent material, as conditioned by relief, over periods of time.
Soil Forming Processes
- Translocations
- Transformations
- Additions
- Losses
- Mineral matter
- Organic matter
- Air
- Water
Major Components
Physical Properties
of Soil
- Soil texture
- Soil structure
- Soil color
- Bulk density
Three Fractions of Mineral Matter
- Sand
- Silt
- Clay
USDA Textural Triangle
Examples of Soil Structure
Aspects of Soil Structure
- The arrangement into aggregates of desirable shape and size
- The stability of the aggregate
- The configuration of the pores
Factors that Affect Aggregate Stability
- Kind of clay
- Chemical elements associated with the clay
- Nature of the products of decomposition or organic matter
- Nature of the microbial population
Factors that Affect
Soil Structure
- Kind of clay
- Amount of organic matter
- Freezing and thawing
- Wetting and drying
- Action of burrowing organisms
- Growth of root systems of plants
Important Note
- All of these have a loosening effect on the soil, but they have no effect on aggregate stability
Bulk Density
- Determined by dividing the weight of oven-dry soil in grams by its volume in cubic centimeters
- The variation in bulk density is due largely to the difference in total pore space
Effects of Bulk Density
- Engineering properties
- Water movement
- Rooting depth of plants
Soil Color
- Indicator of different soil types
- Indicator of certain physical and chemical characteristics
- Due to humus content and chemical nature of the iron compounds present in the soil
Major Forms of Iron and Effect on Soil Color
Form Chemical Formula Color
Ferrous oxide FeO Gray
Ferric oxide
(Hematite) Fe2O3 Red
Hydrated ferric oxide
(Limonite) 2Fe2O3 3H2O Yellow
