Soil formation, Conservation, and Protection Flashcards
Unconsolidated regolith modified over time by water, air, and organic material.
Soil
a mixture of minerals, air, water, and organic matter in the correct proportion
Fertile soil.
The study of soil as a habitat for living organisms
Edaphology
Study of social as geologic entity, meaning, its formation, classification, chemistry, and morphology
Pedology
Break down of rocks from the result of a mechanical action. Temperature changes, abrasion, or frost can cause rocks to break dowm.
Physical weatherimg
breakdown of rocks through a change of their chemical makeup. this can happen when the minerals than rocks react with water, air, or other chemicals.
Chemical weathering
Breakdown of rocks by living things. Burrowing animals help water and air get into rock, and plant roots can grow Into cracks in the rocks, making it split.
Biological weathering
6 factors that affect soil formation:
• Parent Material
• Time
• Climate
• Organisms
• Topography
• Weathering
determined by the size of them mineral particles within the soil
Soil texture
Largest soil particle which consist of fragments larger than 2.0 mm in diameter
Gravel
0.05 and 2.0 mm
Sand particles
range from 0.002 to 0.05 millimeter.
Silt particles
Smallest particle, less than 0.002 millimeter in diameter
Clay particles
Ideal soil for agriculture. provides good aeration and drainage properties of large particles with nutrient - retention and water - holding ability.
Loam
They use a standard system for classifying soils according to the amount of clay, silt, and sand.
USDA Textural Classification Chart