Chapter 5 - Physical Characterisitcs Of Soil Flashcards
What does soil consist of
Mineral matter 45%
Air 25%
Water 25%
Organic matter 5%
What is ion exchange
Takes place in soils where ions are attracted to soil particles and are held on the surface of these particles
Also know as adsorption
What is organic matter and humus
Organic matter - the remains of plants and animals
Humus - the dark coloured decomposed plant and animal matter found in the soil. It is rich in nutrients and contributes to soil structure
What is soil texture
Is a measure of the proportion of sand silt and clay in a soil sample
Important as it cannot be changed
What is Loam soil
A soil that has equal amounts of sand silt and clay
What are the five physical properties of soil
Texture Structure Porosity and density Colour Temperature
What is flocculation and how does it occur
The clustering together of soil particles to form floccules
The floccule is a chain of collided particles held together forces of attraction between water and colloids
The floccule then trap larger particles such as sand and silt forming aggregates
What is cement action and separation
Cementation - the binding together of soil particles
Separation - occurs when soil aggregates are separated within the soil
What is soil porosity
Refers to the total volume of soil occupied by soil pores
Good soil should have 50% of its volume occupied by soil pores
Pores are filled with air and water
How does soil compaction occur
Occurs when soil particles are pressed together aggregates are destroyed which reduces pore space
What is absorbed water (hydroscopic water)
A positively charged water that forms a thin film around a negative soil particle
It cannot be removed from soil and is unavailable to plants
What is capillary water and gravitational water
Capillary water - held in by the pores when the soil aggregates and in the pores between the soil aggregates
Gravitational water- moved through the soil by gravity
What is field capacity and permanent wilting point
Field capacity - amount of water in a soil after the gravitational water has been drained away
Permanent wilting point - the point at which no more capillary water can be removed from the soil by plants
What is Available water capacity
Field capacity - permanent wilting point
What does soil colour indicate
The amount of humus and parent material content
High humus = good soil structure
Dark soils absorbs more sunlight so heat up quickly
Grey - lacking humus low fertility leeching
Red - presence of iron may have been leeched to form an iron pan