Simply put, soil is the mixing of parent rock with organic matter. The rock weathers to create small and large fragments. This is done either by Physical Weathering, e.g. frost action and water abrasion, or by Chemical Weathering, e.g. dissolving action by carbon dioxide in water and oxidation. The rock in turn can receive a covering of organic matter, e.g. leaves and animal matter. It may come from plants like lichens which attach themselves to the rock surface.
Lichen growing on sandstone
The diagram below tries to show what happens over time. The top layer of organic matter slowly rotting and decomposing into smaller fragments and beginning to mix with the fragments of rock which are weathering from below. Over many hundreds of years the soil forms to create three distinct layer sor horizons. These are known as the A Horizon (primarily organic material), the C Horizon (the parent rock) and B Horizon ,the mixture layer in between.
Many factors will play a part in the soil formation to determine the properties and type:
- Type of parent rock
- Topography of the land
- Flora and Fauna
The latter are the all important organisms which promote the decomposition, movement and mixing of the layers. Part of this flora will be bacteria and fungi that complete the decomposition process to generate humus. This dark, sticky material determines the rich quality of the soil and is predominant in the B Horizon. Texture is important and determines the pore-space, which in turn, influences the proportion of air and water present. For example, sand is a coarse inorganic material which produces large air spaces such that water will quickly drain through the soil. This may carry away many of the nutrients of the soil, a process called leaching. Clay particles are much finer creating very small pores and so drainage is poor with minimal leaching. A mixture of particle sizes will producer a better quality soil called loam.
To classify the soil types one needs to look at the structure of the layers and so a section through the soil must be dug, called a profile. Below are several examples. One of the clearest examples of seeing the layering is on sandy ground where leaching is most likely. This soil type is called a podsolwhere the leaching creates an acidic pH. A brown earth soil is common in deciduous woodlands and is typically neutral whilst a rendzina is found on chalk, an alkaline soil.
A profile through a podsol. Notice the distinctive layers called horizons
Podsolization occurs when leaching of the soil is high. This requires a high rainfall and because of the large air spaces present in sandy soils water drains (leaches) through rapidly. This carries away the soluble mineral ions reducing the content of the topsoil. These impoverished soils have well defined layers or horizons. At the surface is the A horizon which is divided up into 3 sub-horizons. AO horizon has a build up of raw humus and litter which is undecomposed. Its base is moist and black; calcium content negligible and is acidic A1 is the point where dark humus mixes with the sand; some minerals are present. The A2 horizon is a wide band of very pale sand; this is due to the removal (leaching) of the minerals. It is dry and stained with minerals, e.g. iron gives orange patches. The B horizon, up to a metre down from the surface is a dark band, due to the deposition of humus. This may be further divided with the deposition of minerals as a hard “pan” which is usually a complex of iron oxide. This iron pan may be a hard, impenetrable layer reminiscent of concrete. Depending on the topography of the land it will cause waterlogging giving rise to wet heath or direct water into valleys where a bog will develop. The C horizon is an orange parent rock of sandstone
Iron Pan exposed by a river (image above). The profile has been cut by the river and the “shelf-like” hard layer along the base of the section, on which the spade is standing, is the exposed iron pan.
Brown Earth Soils
This profile shows less of a layering and is typical of deciduous woodland.