×
Top
Download PDF
FAQ

Meaning of Eluviation

Bookmark added to your notes.
View Notes
×

Eluviation meaning is the downward percolation of water through soil horizons that transports soil content from upper layers to lower levels, and illuviation is the deposition of this material (illuvial deposit) in lower levels. Eluviation is the movement of water that removes dissolved or suspended material from a layer or layers of soil when rainfall exceeds evaporation. Leaching is the term used to describe the loss of material in the solution.

Eluviation Definition

The transportation of dissolved or suspended material within the soil by the movement of water as rainfall exceeds evaporation.


Eluvium or alluvial deposits are volcanic deposits and soils formed by in situ weathering or weathering combined with gravitational movement or deposition in geology.


Eluviation or leaching is the method of removing materials from geological or soil horizons. There is a distinction between how this word is used in geology and soil science. Eluviation is the downward percolation of water through soil horizons that transports soil content from upper layers to lower levels, and illuviation is the deposition of this material (illuvial deposit) in lower levels. The extracted material is meaningless in geology, and the deposit (alluvial deposit) is the material that remains. When precipitation exceeds evaporation, eluviation occurs.


An alluvial zone or illuvial horizon is a soil horizon created by eluviation. The illuvial horizon is a light-colored region in a standard soil profile that is either at the lower part of the A horizon or within a distinct horizon (E horizon) below the A, where the process is most strong and rapid (depending on background and literature). While eluviation theoretically occurs in both, some sources consider the alluvial zone to be the A horizon plus the (distinct) E horizon. The strict illuvial horizon (E horizon) is usually light grey, clay-free, low in organic matter, and high in salt and sand particles made up of quartz and other resistant minerals.


Alluvial ore deposits, including tungsten and gold placer deposits, are created by settling and enriched by winnowing or removing lower-density materials. Alluvial deposits are diamonds found within the yellow ground (weathered parts of kimberlites). Residual or alluvial deposits of cassiterite and columbite-tantalite can also be found. The Pitinga tin deposit, an alluvial deposit in Brazil, is one of the world's largest tin mines. In Ontario, weathering supergene enrichment of an apatite-rich carbonatite has resulted in a large alluvial phosphate ore deposit.

Eluviation of Soil

Water pushes tiny colloidal-sized materials into the soil as it moves through it. Eluviation is the movement or leaching of materials such as clay, iron, or calcium carbonate. The region of eluviation, also known as the E horizon or eluviation layer of soil, is the area where the materials have been extracted. Alluvial zones have fewer nutrients for plant growth. In forested soils, E horizons are common.


Different forms of soil exist, each with its own set of characteristics. Any soil has layers, or horizons, as you can see if you dig far enough (O, A, E, B, C, R). When you combine the horizons, you get a soil profile. Each profile, like a biography, tells a tale about a soil's life. Most soils have three main horizons (A, B, and C), as well as an organic horizon in some cases (O). The following are the horizons:


O (Humus or Organic): Organic matter, primarily decomposing leaves. Some soils have a thin O horizon, while others have a dense O horizon or none at all.


A (Topsoil): Mostly minerals from the parent material, with some organic matter. Plants and other organisms can thrive in this material.


E (Eluviate): Leached of clay, minerals, and organic matter, leaving a concentration of sand and silt particles of quartz or other resistant materials – contained in older soils and forest soils. 


B (Subsoil): Minerals leached (moved down) from the A or E horizons and deposited in the B.


C (Parent Material): The deposit that formed the soil at the Earth's surface.


R (Bedrock): A mass of rock, such as granite, basalt, quartzite, limestone, or sandstone, that serves as the parent material for some soils when it is close enough to weather. This isn't dirt, because it's under the C horizon.

[Image will be Uploaded Soon]

FAQ (Frequently Asked Questions)

1. Explain the difference between illuviation and Eluviation?

Ans: illuvium-Illuvium is material that has been displaced through a soil profile by rainwater from one layer to another. Illuvium is material that has been displaced through a soil profile, from one layer to the next, by rainwater. Eluviation is the process of removing material from a soil layer. The substance may be transported mechanically or chemically. Illuviation is the name for the method of illuvium deposition. In contrast to alluviation, which is a horizontal running water movement, it is a water-assisted vertical transport. Alluvial deposits are the product of this process. Alluvial deposits, such as cutans, are a form of alluvial deposit. Organic matter, silicate clay, and iron and aluminum hydrous oxides are among the elements found in illuvium. Alluvial deposits of clays, oxides, and organics from distinctive soil horizons are known as "B horizons'' or "zones of illuviation" in the subsoil. Eluviation is the process of removing material from a soil layer. The substance may be transported mechanically or chemically. Illuviation is the name for the method of illuvium deposition.

2. What is Soil illuviation? Explain the Process of illuviation.

Ans: Illuviation is the buildup of dissolved or suspended soil materials in one region or substrate as a result of percolation (leaching) from another. Clay, iron, and humus typically wash out and leave a line of a different consistency and color. These lines are critical for determining the age and composition of rock strata. Water flows into the soil, causing illuviation. It transports clay, iron, hummus, calcium carbonate, and other minerals into small particles. These particles settle in the subsoil or zones close to the surface. Illuvial zones are the name given to these regions. The illuvium is the substance that has been transferred.