Intro to Soil Science Flashcards
General knowledge of intro to soil science
Definition of Soil
“The layer(s) of generally loose mineral and/or organic material that are affected by physical, chemical, and/or biological processes at or near the planetarysurface and usually hold liquids, gases, and biota and support plants.”
Function of Soils (six ecological roles)
- medium for plant growth
- recycling system for nutrients and organic waste
- modifier of the atmosphere
- habitat for soil organisms
- engineering medium
- system for water supply and purification
Soil components
45% mineral, 25% air, 25% water and 5% organic matter
Soil & climate change
4 per 1000
carbon sequestration in soils for food security and climate
Soil importance in global and local health
globally; soil science can help predict where arsenic contamination of groundwater is
locally; soil influence on food, water filtration, and chemical/pathogen exposure
The five soil forming factors:
- Parent material
•The starting material from which a soil develops - Climate
•Temperature and moisture - Biota
•Kinds of plants, worms, rodents, insects, fungi, microbes
4.Topography
•Slope steepness, position, orientation - Time
•Younger soils tend to be less developed than older soils
How does soil formation lead to horizons?
The effects of climate, biota, topography, and time on the parent material bring about the vertical differentiation we see in soils.
What is Soil profile and what is it composed of?
A vertical excavation exposes a 2D cross-section called the soil profile.
The soil profile is composed of layers called horizons.
•Variable thickness
•Parallel to the land surface.
What is a soil pedon?
Pedon= A representative volume (3D)
Incorporates the natural vertical & lateral variabilityof a specific soil
How do horizons form?
Translocation and accumulation of material in a soil.
Soil Horizon notations:
- The O, A, E, and B horizons = solum
- The A, E, B, and C horizons are = regolith.
- R horizon (Bedrock): Hard rock. Little evidence of weathering.
C Horizon:
~parent material~
-Can be dug with a shovel but retains the structural features of the sediment or rock from which the soil formed.
O Horizon:
Fresh and partially decomposed organic layer at the soil surface. “Litter layer”
A Horizon:
Dominated by mineral particles but darkened by the accumulation of organic matter (i.e.“Topsoil. ” )
E Horizon:
- The “leached and bleached”horizon = zone of eluviation.
- The E horizon is a layer from which nearly all of the clay and iron have been removed and organic matter have not accumulated.