Soil formation

 

Soil formation

Soils have a life cycle; they are born, mature and become of age. In cases, they may even "die" (disappear or get buried).

Soil formation starts by desintegrating the rock under the influence of climate. Rainwater will dissolve rock elements, temperature fluctations will cause differential expansion and contraction of rock-forming crystals, and the freezing and thawing of water captured in the rock will widen existing cracks and cavities. Pioneer vegetation, at first lichens, will settle and their roots will further loosen the rock. Moreover, decaying plant debris will produce organic acids, which further attack the rock. Organic matter will start to accumulate and be mixed with the mineral material provided by the rock. A soil is born.

Over time, rock minerals will be dissolved or transformed. Elements released from the rock will precipitate and new minerals may be formed. For example, iron will be oxidized and precipitate as iron oxides or hydroxides, giving the soil reddish or yellowish-brownish colours. Soil fauna will settle and mix (‘homogenize’) the soil. The soil will grow in depth through newly formed soil material at the bottom. The soil matures.

Given sufficient time under stable environmental conditions, soils will reach a steady state, whereby soil build-up matches their breakdown. Production of humus from decaying vegetational debris will equal its consumption by soil microbae, fauna and flora. Transformation of rock minerals into soil minerals will keep pace with the removal of earlier formed soil minerals. Slow surface wash of topsoil is matched by new formation of soil material from the bedrock. The soil has aged.

Dramatic events can interrupt the life cycle of soils. A soil may be covered suddenly by a volcanic eruption or by submergence under water. They may disappear in part or altogether by water or wind erosion. 

On steep slopes the newly formed loose soil material will be removed fairly easily by runoff of rainwater or gravitational forces. Therefore, soils in mountainous regions are often shallow. On footslopes and in more level areas soil material will accumulate and this leads to deeper soils.