Soil components.

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Presentation transcript:

Soil components

Student activity In your group list the components that make up soil. 2mins

Learning outcomes Discuss what components form soil Discuss and feel different textures of soil Look at the different soil particle sizes Explain the benefits and limitations of soil components

Soil components Soil is formed from the following components: Sand Silt Clay Living organisms Organic matter

Sand Forms free draining soils Water runs through it quickly Largest mineral particle size between 2mm and 0.06mm in diameter Feels gritty to touch Makes a rasping sound when rubbed together Particles do not stick together and cannot be made into a ball Soils warm quickly in the spring but also cool quickly in the autumn Forms soils which cannot hold on to nutrients No swelling or shrinkage in the soil Can be used to make glass

Silt Forms soils which can be hard to drain Holds on to a moderate amount of water Medium mineral particle size between 0.006 and 0.002mm in diameter Feels soapy or silky Makes a squeaky sound when rubbed together Particles don’t easily hold together- a ball of them breaks easily Soils warm and cool more quickly than clay but less quickly than sand Forms soils which can only hold limited nutrients Limited swelling or shrinkage in the soil Makes very fertile soils

Clay Forms soils which readily become waterlogged Becomes heavy when wet Smallest mineral particle size – diameter 0.002mm Feels smooth when dry and sticky when wet Makes very little sound when rubbed together Particles stick together and are easy to make into a ball Soil takes longer to warm up in the spring and cool down in the autumn Forms soils which can hold onto nutrients Soil swells when wet and shrinks when dry Can be used to make bricks or pots

Living organisms Are responsible for recycling minerals Are responsible for the rotting of dead material Can produce 20-40-tonnes of cast per hectare Examples include insects, bacteria and earthworms Bury stones and leaf litter Convert plant and animal debris to minerals and humus Examples include fungi and plant roots Absorb water from soil causing it to dry and clays to shrink Help to reduce damaging effects of pesticides Can create channels for the movement of oxygen and water

Organic matter Can increase the amount of air held in some mineral soils Releases nutrients slowly as it rots Sticks to soil particles Examples include farmyard manure, straw and horticultural peat Improved water holding capacity of mineral soils Creates an open soil structure Examples include leaf mould and compost Can make soils warmer-increase heat absorption Helps to retain nutrients in the soil Are responsible for the dark colours of soils