Soil processes (W3) Flashcards
Physical weathering of minerals
Physical weathering is the brittle fracture of rocks by the physical processes of: unloading and growth and expansion of ice.
Decomposition of organic matter
Decomposition of organic matter describes the process by which soil organisms use soil organic compounds as a food source.
Example. Breakdown of leaf litter.
Stage 1. Primary decomposers break up litter detritus.
Stage 2. Secondary decomposers break down organic matter into smaller molecular structures
Stage 3. Corpses and faeces of decomposers provide substrate for further decomposition.
Waterlogging
saturated with water. slows down rate of organic matter decomposition
Soil ripening
Soil ripening occurs when a soil that is waterlogged or flooded dries out.
Changes can be physical, chemical or biological.
Pedoturbation
Physical mixing of soil profile (e.g. by soil creep)
Infiltration
Process by which water enters the soil and transports chemicals into the soil profile
percolation
When water moves downwards through the soil.
gleying
Gleyed soils are produced when waterlogging is irregular or seasonal
Physical ripening
cracking followed by redox changes due to air entry
Chemical ripening
oxidation of organic matter, iron and manganese
Bioturbation
biological mixing of the soil by plants and animals
Cryoturbation
physical mixing of the soil by frost
eluviation
General term for the transfer of soil material in solution from one horizon, comprising two processes:
leaching and chetvulation
Leaching (eluviation)
movement of soluble organic and inorganic soil components (solutes) in percolating water.
Cheluviation (eluviation)
soluble organic complexes move metal cations through soil profile (especially iron and aluminium)
Illuviation
introduction of salt by water by percolation from another horizon.
What are the 6 soil horizons?
- O (organic)
- A (surface)-Mixed inorganic-organic layer of eluviation (leaching)
- Ea- Bleached horizon from which clays and iron oxides have been removed
- B (Subsoil)- Iron-rich horizon of illuviation (i.e. accumulating material)
- C (Substratum)- Weathered parent material on which soil is forming
- R (Bedrock)
Podzol
infertile acidic soil
Classification of world soils, FAO Soil Classification
- Classification of major soil groups based on their properties and dominant soil forming factors.
-Organic soils 1 soil order:
HISTOSOLS
-Mineral soils 11 soil orders
Organic soils: HISTOSOLS
Consist of organic debris which accumulates at the surface under wet or dry conditions