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Climate
Most important factor
It determines
Rate of weathering + biological activity
Hot climates
Rapid chemical weathering + decomposition of organic matter
Cold climates
Less biological activity + freeze-thaw action
Wet climates
Leaching + waterlogging
Dry climates
Draught + evaporation leads to salinisation and calcification
Salinisation and calcification
Build up of salt and calcium
Ex. (salinisation and calcification)
Saltpans of Botswana and Bonneville Salt Flats
Parent Material
Original bedrock
This is where
Mineral matter in the soil first developed
Different rocks develop
Different soil characteristics
Igneous rock develops
Acidic soils
Sedimentary rock develops
Large variety
Topography
Soil formation is affected by gradient, altitude and aspect
Each of these affect
Depth and drainage of soil
Flat upland areas tend to be
Cold and wet (waterlogging)
Sloping land tend to experience
Soil erosion (much thinner)
Low lying flat areas tend to be
Abundant in humus (fertile)
Number of organisms determine
The fertility of soil
Decomposition of what occurs
Organic material (plant roots, burrowing animals, bacteria)
Animals such as rabbits
Help aerate and mix the soil as they burrow through horizons
Fungi and bacteria lead to
Humification
Time
Soils take a very long time to form
Young soil
Not well developed
Older soil
Well developed profiles
Most of Ireland’s soils are
Less than 10,000 y/o