Lecture 2: Formation of soils from parent materials Flashcards
Climate (Cl-O-R-P-T)
-most influential factor on parent material because it determines what kind and how intense the weathering will occur in that area
-temperature: every 10 degree rise in temp double the rate of biochemical rxns
-effective precipitation: water must penetrate the regolith to be effective in soil formation
Organisms (Cl-O-R-P-T)
the type of vegetation that is growing in that area, as well as the land use, affects the soil layers. (eg. a plowed field vs a forest)
Relief (Cl-O-R-P-T)
Soils on a slope LOSE material due to gravity. Soils in flat areas GAIN materials especially from the fallen materials of the slope.
Time (Cl-O-R-P-T)
Younger soils typically have less layers than older soils. Older soils also may not have as many nutrients.
When does pedogenesis begin?
When horizons that are not present in the parent material begin to appear in the soil profile
What is pedogenesis?
Soil formation
The 4 basic processes of pedogenesis
-Additions
-Losses
-Translocations
-Transformations
Topsoil Letters
A (or E)
Subsoil
B
Regolith
C (or R)
Topsoil: A Horizon
-darker
-mineral soil + organic matter
-water flows through (loses minerals bc of this)
Topsoil: E Horizon
-grey to white
-mostly sand
-zone of intense leaching
-Fe- and Al- oxides have been eluviated
-common under forest because of HUMIDITY and ACIDIC soil pH
Subsoil: B Horizon
-accumulation of mineral particles leached from topsoil like clay and salts
-less organic matter
denser
-more difficult for plant roots and water to penetrate
-usually red, brown, or orange
Regolith: C Horizon
-most like parent material
-very little biological activity and weathering
-can be dug with a shovel
Regolith: R Horizon
-hardpan (compacted)
-composed of compacted and/or cemented clay with calcium carbonate, iron oxide, manganese or silica
-unaltered parent material, consolidated bedrock
-impermeable
-can’t be dug with a shovel