Parent material

Parent material is the underlying geological material (generally bedrock or a superficial or drift deposit) in which soil horizons form. Soils typically inherit a great deal of structure and minerals from their parent material, and, as such, are often classified based upon their contents of consolidated or unconsolidated mineral material that has undergone some degree of physical or chemical weathering and the mode by which the materials were most recently transported.

Consolidated

Parent materials that are predominantly composed of consolidated rock are termed residual parent material. The consolidated rocks consist of igneous, sedimentary, and metamorphic rock, etc.^[1]

Residual

Soil developed in residual parent material is that which forms in consolidated geologic material.^[1]^[2]

Unconsolidated

This parent material is loosely arranged, particles are not cemented together, and not stratified. This parent material is classified by its last means of transport. For example, Material that was transported to a location by glacier, then deposited elsewhere by streams, is classified as stream-transported parent material, or glacial fluvial parent material.

Ice transported

Glacial till (Morrainal)

The material dragged with a moving ice sheet. Because it is not transported with liquid water, the material is not sorted by size. There are two kinds of glacial till:

Basal till - carried at the base of the glacier and laid underneath it. This till is typically very compacted and does not allow for quick water infiltration.
Ablation till - carried on or in the glacier and is laid down as the glacier melts. This till is typically less compacted than basal till. ^{[citation needed]}

Glacio-lacustrine

Parent material that is created from the sediments coming into lakes that come from glaciers. The lakes are typically ice margin lakes or other types formed from glacial erosion or deposition. The bedload of the rivers, containing the larger rocks and stones is deposited near the lake edge, while the suspended sediments are settle out all over the lake bed.

Glacio-fluvial

Consist of boulders, gravel, sand, silt and clay from ice sheets or glaciers. They are transported, sorted and deposited by streams of water. The deposits are formed beside, below or downstream from the ice.

Glacio-marine

These sediments are created when sediments have been transported to the oceans by glaciers or icebergs. They may contain large boulders, transported by and dropped from icebergs, in the midst of fine-grained sediments.

Water transported

Within water transported parent material there are several important types.

Alluvium

Parent material transported by streams of which there are three main types. Floodplains are the parts of river valleys that are covered with water during floods. Due to their seasonal nature, floods create stratified layers in which larger particles tend to settle nearer the channel and smaller particles settle nearer the edges of the flooding area.^[1] Alluvial fans are sedimentary areas formed by narrow valley streams that suddenly drop to lowlands and widen dramatically. Sedimentary in these types of deposits tend to be larger closer to the uplands and finer near the edges of the fan.^[1] Delta deposits, the third of type of alluvium, are finer sediments that are discharged from streams into lakes and eventually settle near the mouth of the river.^[1]

Lacustrine

Parent material deposited by a lake. Beach ridges may be present where ancient lakes once washed up sand. Lacustrine material is well sorted and fine-textured, having finer silts and clays. Soils formed from lacustrine parent material have low permeability in part because of this high clay content.

Marine

Ocean deposited parent materials, called marine sediments, are collections of material that have been carried by rivers and streams to the ocean and eventually sink to the bottom. Such materials can vary in texture.^[1]

Gravity transported

Colluvium or colluvial debris is the collection of large rock fragments that have traveled downslope by gravity.^[1]

Wind transported

Parent materials can also be transported by wind, there are three important types.

Loess

Silt sized sediments transported by the wind.

Aeolian

Sand sized particles transported by the wind typically as dunes.

Volcanic tephra

The most common parent material coming from volcanoes is volcanic ash carried away by the wind and settling different distances from the volcano.^{[citation needed]}

Organic

Organic deposits (or cumulose deposits) are developed in place from plant residue (for example sphagnum moss) that has typically been preserved by a high water table, or potentially due to another factor that slows decomposition.

Climate and weathering

Climate is generally considered the most important factor influencing physical and chemical weathering processes. ^{[citation needed]}

Physical weathering is especially important during the early stages of soil development. Rock can be disintegrated by changes in temperature which produces differential expansion and contraction. Changes in temperature can also cause water to freeze. The forces produced by water freezing can be as great as 2.1 × 10⁵ kPa, which can split rocks apart, wedge rocks upward in the soil, and heave and churn soil material.

Chemical weathering: the principal agent is percolating rainwater charged with carbon dioxide from the atmosphere. Parent material becomes hydrolyzed by the acidic solution to produce minerals and to release cations.

References

^ ^a ^b ^c ^d ^e ^f ^g Barnes, Burton; Zak, Donald; Denton, Shirley; Spurr, Stephen (1980). Forest Ecology. New York, NY: John Wiley & Sons, Inc. ISBN 978-0-471-30822-5.
^ Brady, Nyle; Weil, Ray (1996). The Nature and Properties of Soils. Upper Saddle River, NJ: Prentice Hall. ISBN 978-0-13-016763-7.

[ForestEcology-1] ^ ^a ^b ^c ^d ^e ^f ^g Barnes, Burton; Zak, Donald; Denton, Shirley; Spurr, Stephen (1980). Forest Ecology. New York, NY: John Wiley & Sons, Inc. ISBN 978-0-471-30822-5.

[NPSoils-2] Brady, Nyle; Weil, Ray (1996). The Nature and Properties of Soils. Upper Saddle River, NJ: Prentice Hall. ISBN 978-0-13-016763-7.

[1]

[2]

v t e Soil classification
World Reference Base for Soil Resources (1998–)	Acrisols Alisols Andosols Anthrosols Arenosols Calcisols Cambisols Chernozem Cryosols Durisols Ferralsols Fluvisols Gleysols Gypsisols Histosol Kastanozems Leptosols Lixisols Luvisols Nitisols Phaeozems Planosols Plinthosols Podzols Regosols Retisols Solonchaks Solonetz Stagnosol Technosols Umbrisols Vertisols
USDA soil taxonomy	Alfisols Andisols Aridisols Entisols Gelisols Histosols Inceptisols Mollisols Oxisols Spodosols Ultisols Vertisols
Other systems	FAO soil classification (1974–1998) Unified Soil Classification System AASHTO Soil Classification System Référentiel pédologique (French classification system) Canadian system of soil classification Australian Soil Classification Polish Soil Classification 1938 USDA soil taxonomy List of U.S. state soils List of vineyard soil types
Non-systematic soil types	Sand Silt Clay Loam Topsoil Subsoil Soil crust Claypan Hardpan Gypcrust Caliche Parent material Pedosphere Laimosphere Rhizosphere Bulk soil Alkali soil Bay mud Blue goo Brickearth Brown earth Calcareous grassland Dark earth Dry quicksand Duplex soil Eluvium Expansive clay Fill dirt Fuller's earth Hydrophobic soil Loess Lunar soil Martian soil Mud Muskeg Paleosol Peat Prime farmland Quicksand Serpentine soil Spodic soil Stagnogley Subaqueous soil Takir Terra preta Terra rossa Tropical peat Yedoma
Types of soil