(c) Describe the characteristics of the three zones of soil profile.
(a) Soil profile
A soil profile is a vertical section of soil from the ground surface down to the parent rock or bedrock, showing the different layers or horizons of the soil.
(b) Well-labelled diagram of a soil profile
A labelled vertical section of a soil profile.
(c) Characteristics of the three zones of a soil profile
A horizon (topsoil or zone of eluviation)
It is the uppermost layer of mineral soil, immediately below the surface litter.
It contains decaying plant and animal remains which form humus.
It is dark in colour and is usually the most fertile horizon.
It is the zone of greatest biological activity, containing many soil organisms and most plant roots.
Soluble minerals and fine materials are washed down from this horizon by percolating water.
B horizon (subsoil or zone of illuviation)
It lies below the A horizon and contains little humus.
It is the zone in which clay, iron, aluminium and other mineral materials leached from the A horizon accumulate.
It is often reddish, brownish or yellowish because of iron compounds.
It is usually denser and more compact than the topsoil.
Only deep-rooted plants commonly extend into this horizon.
C horizon (parent-material horizon)
It consists mainly of partly weathered rock fragments and other parent material from which the soil develops.
It contains very little or no humus and has little biological activity.
It is coarser and less developed than the A and B horizons.
It grades downward into hard, unweathered bedrock.
A soil profile is a vertical section of soil from the ground surface down to the parent rock or bedrock, showing the different layers or horizons of the soil.
(b) Well-labelled diagram of a soil profile
A labelled vertical section of a soil profile.
(c) Characteristics of the three zones of a soil profile
A horizon (topsoil or zone of eluviation)
It is the uppermost layer of mineral soil, immediately below the surface litter.
It contains decaying plant and animal remains which form humus.
It is dark in colour and is usually the most fertile horizon.
It is the zone of greatest biological activity, containing many soil organisms and most plant roots.
Soluble minerals and fine materials are washed down from this horizon by percolating water.
B horizon (subsoil or zone of illuviation)
It lies below the A horizon and contains little humus.
It is the zone in which clay, iron, aluminium and other mineral materials leached from the A horizon accumulate.
It is often reddish, brownish or yellowish because of iron compounds.
It is usually denser and more compact than the topsoil.
Only deep-rooted plants commonly extend into this horizon.
C horizon (parent-material horizon)
It consists mainly of partly weathered rock fragments and other parent material from which the soil develops.
It contains very little or no humus and has little biological activity.
It is coarser and less developed than the A and B horizons.
It grades downward into hard, unweathered bedrock.