Factors affecting soil variation in the UK Flashcards
definition of soil
- dynamic natural body composed of mineral and organic material and living forms in which plants grow
- collection of natural bodies occupying part of the earths surface that supports plants and are influenced by climate, relief, time and parent material
soil variation
the type of mineral and organic inputs, and the speed at which they are transformed, moved or lost from the soil profile will depend on local environmental conditions and will determine the type oo soil
soil formation
- climate
- biology
- parent material
- topography
- time
- management
how does parent material influence soil properties?
influenced by particle size and state of consolidation
- influenced by mineralogy and chemical composition
main type of parent material
SEDENTARY - igneous, metamorphic or sedimentary TRANSPORTED - sedimentary - geologically recent, Quaternary - predominant soil and landscape forming material in the UK
Generalised map of parent materials in the UK
UPLANDS
- mostly pre-glacial and include all 3 rock types
LOWLANDS
- Quaternary sediments of glacial, aeolian, alluvial, colluvial or biogenic laid down in various stages
Physical and chemical properties of drift depend on
- the mineralogy of the rocks from which the drift was derived
- the extent of weathering prior to deposition
- the transport processes that deposited the drift
Transport processes that deposit drift materials
- ice: glacial
- water: glacial, alluvial
- wind: aeolian
- Gravity: colluvial
Glacial drift
GLACIAL TILL
- deposited by ice sheets during the cold stage
FLUVIO-GLACIAL DEPOSITS
- deposited by melt water during the warm stages
Aeolian Drift
- glacial origin
- not common in the UK
- often mixed with glacial drift
- very important in the USA
Colluvial drift
- accumulated material (mostly <10,00 years) on the sides and bases of slopes and valleys
- coarse and stoney
- agriculturally unimportant
Alluvial drift
- recently deposited by flooding streams and rivers that runt heir current course
- particle size ranges from large stones and boulders to fine clays
- particles are sorted into different sizes during the flood, with the larger material being deposited near the river channel and finer materials further away
Climate
Temperature
- function of latitude and altitude
- mild winters in the UK lowlands
- cool summers in the UK, especially with increasing altitude
Precipitation
- Annual rainfall ranges from 50mm in lowland east and south to 5000mm in mountains in the west
Relief
The shape of the land affects the evolution of the soil by causing local different in
- climate
- ground surface stability
- moisture regimes (hydrological sequences)
influences of vegetation and management
- acidity inputs
- organic matter accumulation
- soil surface stability
- soil moisture