Caliche: Difference between revisions

From WikiMD's Wellness Encyclopedia

CSV import
Tags: mobile edit mobile web edit
 
CSV import
Tags: mobile edit mobile web edit
 
Line 31: Line 31:
[[Category:Soil]]
[[Category:Soil]]
{{geology-stub}}
{{geology-stub}}
<gallery>
File:San-miguel-island-caliche.jpg|Caliche formation on San Miguel Island
File:Caliche_-_Sedimentary_Rock_Ridgecrest_Kern_County_California.jpg|Caliche sedimentary rock in Ridgecrest, Kern County, California
File:Limestone_rubble_wall_with_brick_quoins.jpg|Limestone rubble wall with brick quoins
File:Caliche-5731.jpg|Caliche
</gallery>

Latest revision as of 04:38, 18 February 2025

Caliche is a sedimentary rock, a hardened natural cement of calcium carbonate that binds other materials—such as gravel, sand, clay, and silt. It occurs worldwide, in aridisol and mollisol soil orders—generally in arid or semiarid regions, including in central and western Australia, in the Kalahari Desert in Africa, and in the southwestern United States. It is often used in construction in regions where it is abundant because it is strong and durable, and it is also used as a source of calcium for agricultural purposes and can be utilized in the production of cement.

Formation[edit]

Caliche layers form when minerals, especially calcium carbonate, precipitate out of water percolating through the ground. This process can occur at or near the surface to form a hard, cement-like layer. Caliche formation can be a slow process, taking thousands to millions of years, or it can occur relatively quickly in areas with high evaporation rates, where soil water moves upwards, carrying dissolved minerals which precipitate to form caliche.

Characteristics[edit]

Caliche is characterized by its light color, usually white to light brown, though the presence of other minerals can lead to various colors, including reddish or yellowish hues. It is hard and compact, making it difficult to excavate. The thickness of caliche layers can vary significantly, from a few centimeters to several meters, depending on environmental conditions and the length of time over which formation occurs.

Uses[edit]

In construction, caliche is valued for its stability and strength, making it a popular choice for building foundations, roads, and as a construction material in its own right. In regions where it is plentiful, it can be a cost-effective alternative to imported materials.

Agriculturally, caliche is mined for its calcium content, which is used to neutralize acidic soils. Its use in agriculture is especially common in areas where soil acidity is a problem for crop production.

In the production of cement, caliche can serve as a significant source of calcium carbonate, a key ingredient in the manufacturing process.

Environmental Considerations[edit]

While caliche can be beneficial for construction and agriculture, its extraction and use can have environmental impacts. Disturbance of land during mining can lead to habitat destruction and increased erosion. Additionally, the dust generated from mining and processing caliche can contribute to air quality issues.

See Also[edit]

References[edit]

<references group="" responsive="1"></references>

Stub icon
   This article is a geology stub. You can help WikiMD by expanding it!