Soils retrogression and degradation

related topics
{island, water, area}
{specie, animal, plant}
{theory, work, human}
{rate, high, increase}
{acid, form, water}
{math, energy, light}
{food, make, wine}
{war, force, army}
{build, building, house}
{woman, child, man}

Soil retrogression and degradation are two regressive evolution processes associated with the loss of equilibrium of a stable soil. Retrogression is primarily due to erosion and corresponds to a phenomenon where succession reverts back to pioneer conditions (such as bare ground). Degradation is an evolution, different of natural evolution, related to the locale climate and vegetation. It is due to the replacement of the primitive vegetation (known as climax) by a secondary vegetation. This replacement modifies the humus composition and amount, and impacts the formation of the soil. It is directly related to human activity. Soil degradation may also be viewed as any change or disturbance to the soil perceived to be deleterious or undesirable.[1]

At the beginning of a soil formation, only the bare rock outcrops. It is gradually colonized by pioneer species (lichens and mosses), then herbaceous vegetation, shrubs and finally forest. In parallel a first humus-bearing horizon is formed (the A horizon), followed by some mineral horizons (B horizons). Each successive stage is characterized by a certain association of soil/vegetation and environment, which defines an ecosystem.

After a certain time of parallel evolution between the ground and the vegetation, a state of steady balance is reached; this stage of development is called climax by some ecologists and "natural potential" by others. Succession is the evolution towards climax. Regardless of its name, the equilibrium stage of primary succession is the highest natural form of development that the environmental factors are capable of producing.

The cycles of evolution of soils have very variable durations, between tens- hundreds- and thousand-year-old for soils of quick evolution (A horizon only) to more than a million of years for soils of slow development. The same soil may achieve several successive steady state conditions during its existence, as exhibited by the Pygmy forest sequence in Mendocino County, California. Soils naturally reach a state of high productivity from which they naturally degrade as mineral nutrients are removed from the soil system. Thus older soils are more vulnerable to the effects of induced retrogression and degradation.

Contents

Ecological factors influencing soil formation

There are two types of ecological factors influencing the evolution of a soil (through alteration and humification). These two factors are extremely significant to explain the evolution of soils of short development.

  • A first type of factor is the average climate of an area and the vegetation which is associated (biome).
  • A second type of factor is more local, and is related to the original rock and local drainage. This type of factor explains appearance of specialized associations (ex peat bogs).

Full article ▸

related documents
Horn of Africa
Moraine
Geography of Mali
Hawar Islands
Great Artesian Basin
Blue Mountains (Australia)
Solent
Geography of New Zealand
Geography of Barbados
Central Valley (California)
Subarctic climate
Geography of Georgia (country)
Geography of Saint Lucia
Ogallala Aquifer
Porongurup National Park
Geography of Kazakhstan
Baffin Island
Houtman Abrolhos
Qattara Depression
Gulf of Mexico
Geography of South Korea
Soil salinity
Darling Scarp
Geography of Puerto Rico
Geography of Bahrain
Mediterranean Sea
Aqueduct
Mount Kinabalu
Geography of Tajikistan
Crater Lake