Soils Flashcards
Three Soil Classification Groups
- Cohesive Soils
- Granular Soils
- Organic Soils
Cohesive Soils
soil is compact, difficult to divide, and on desiccation, large cracks form (clay, silt)
Granular Soils
soil with granular structure in rounded aggregates of from 1 to 10 mm (sand, gravel)
- surface is rough
- easily separated
- difficult to handle rich regions
- sound in humus rich regions
Organic Soils
soil formed essentially of accumulated vegetation, not easily compacted
Soil Consistency Terminology
- Cemented
- Firm
- Friable
- Hard
- Loose
- Plastic
- Sticky
- Soft
Cemented
is not affected by moisture and is very hard
Firm
succumbs to moisture
Friable
crumbly soil that is capable of being reduced to small fragments of even small grains, when tilled friable soil will easily divide into small fragments (usually a loam)
Soil Texture
classified by USDA as sand, loamy sand, sandy loam, loam, silt, sandy, clay loam, clay loam, silty clay loam, sandy clay and clay
Aerobic
availability of free oxygen for organisms
Anaerobic
no available free oxygen, often occurs in wetlands because of the continual presence of water
Alluvial
soil formed by deposition on shores of lakes or large rivers, or in floodplains, alluvial soil is not homogenous, proportion of large grains depends on the speed and turbulence of the waters that deposited them, the obstacles encountered and the distance from the region of origin.
Angle of Repose
(Angle of friction), an engineering property of granular materials. It is the maximum angle of a stable slope determined by friction, cohesion and the shapes of the particles. The angle of repose is the angle a pile forms with the ground.
pH
an expression of the relative concentrations of hydrogen ions and hydroxyl ions in a soil sample. A scale range from 0-14. Terms acid and alkaline used.
Acid
pH less than 7. Most common in areas with high rainfall and are often high in organic matter.