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From Wikipedia, the free encyclopedia

Caliche Forest on San Miguel Island.
Caliche Forest on San Miguel Island.

Caliche (/kəˈl/) 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 the High Plains of the western USA, in the Sonoran Desert and Mojave Desert, and in Eastern Saudi Arabia at Al-Hasa. Caliche is also known as calcrete or kankar (in India). It belongs to the duricrusts. The term caliche is Spanish and is originally from the Latin calx, meaning lime.[1]

Caliche is generally light-colored, but can range from white to light pink to reddish-brown, depending on the impurities present. It generally occurs on or near the surface, but can be found in deeper subsoil deposits, as well. Layers vary from a few inches to feet thick, and multiple layers can exist in a single location. A caliche layer in a soil profile is sometimes called a K horizon.[2][3]

In northern Chile and Peru, caliche also refers to mineral deposits that include nitrate salts.[4][5] Caliche can also refer to various claylike deposits in Mexico and Colombia. In addition, it has been used to describe some forms of quartzite, bauxite, kaolinite, laterite, chalcedony, opal, and soda niter.

A similar material, composed of calcium sulfate rather than calcium carbonate, is called gypcrust.


Caliche forms where annual precipitation is less than 65 centimeters (26 in) per year and the mean annual temperature exceeds 5 °C (41 °F). Higher rainfall leaches excess calcium completely from the soil, while in very arid climates, rainfall is inadequate to leach calcium at all and only thin surface layers of calcite are formed. Plant roots play an important role in caliche formation, by releasing large amounts of carbon dioxide into the A horizon of the soil. Carbon dioxide levels here can exceed 15 times normal atmospheric values. This allows calcium carbonate to dissolve as bicarbonate. Where rainfall is adequate but not excessive, the calcium bicarbonate is carried down into the B horizon. Here there is less biological activity, the carbon dioxide level is much lower, and the bicarbonate reverts to insoluble carbonate. A mixture of calcium carbonate and clay particles accumulates, first forming grains, then small clumps, then a discernible layer, and finally, a thicker, solid bed.[6] As the caliche layer forms, the layer gradually becomes deeper, and eventually moves into the parent material, which lies under the upper soil horizons.[citation needed]

However, caliche also forms in other ways. It can form when water rises through capillary action. In an arid region, rainwater sinks into the ground very quickly. Later, as the surface dries out, the water below the surface rises, carrying up dissolved minerals from lower layers. These precipitate as water evaporates and carbon dioxide is lost. This water movement forms a caliche that is close to the surface.[7] Caliche can also form on outcrops of porous rocks or in rock fissures where water is trapped and evaporates.[8] In general, caliche deposition is a slow process, requiring several thousand years,[3] but if enough moisture is present in an otherwise arid site, it can accumulate fast enough to block a drain pipe.[citation needed]

The depth of the caliche layer is sensitive to mean annual rainfall. When rainfall is around 35 centimeters (14 in) per year, the caliche layer will be as shallow as 25 centimeters (9.8 in). When rainfall is around 75 centimeters (30 in) per year, the caliche layer will be at a depth of around 125 centimeters (49 in). The caliche layer disappears complete in temperate climates if annual rainfall exceeds 100 centimeters (39 in).[9]

Examples of natural occurrence

Caliche — sedimentary rock, Ridgecrest, Kern County, California
Caliche — sedimentary rock, Ridgecrest, Kern County, California
Calcrete rubble was widely used for building construction in South Australia during the 19th century.
Calcrete rubble was widely used for building construction in South Australia during the 19th century.

While the formation of other caliches is relatively well understood, the origin of Chilean caliche is not clearly known. One possibility is that the deposits were formed when a prehistoric inland sea evaporated. Another theory is that it was deposited due to weathering of the Andes.

One of the world's largest deposits of calcrete is in the Makgadikgadi Pans in Botswana, where surface calcretes occur at the location of a now-desiccated prehistoric lake.[10]

Economic uses

Building applications

Caliche is used in construction worldwide. Its reserves in the Llano Estacado in Texas can be used in the manufacture of Portland cement; the caliche meets the chemical composition requirements and has been used as a principal raw material in Portland cement production in at least one Texas plant. Where the calcium carbonate content is over 80%, caliche can also be fired and used as a source of lime, which can then be used for soil stabilization.

Caliche berm surrounding a stock tank in Central Texas
Caliche berm surrounding a stock tank in Central Texas

When mixed with small amounts of either pozzolan or Portland cement, caliche can also be used as a building material that exceeds building code requirements for unfired masonry materials. For example, caliche was used to build some of the Mayan buildings in the Yucatán Peninsula in Mexico. A dormitory in Ingram, Texas, and a demonstration building in Carrizo Springs, Texas, for the United States Department of Energy were also built using caliche as part of studies by the Center for Maximum Potential Building Systems.

In many areas, caliche is also used for road construction, either as a surfacing material, or more commonly, as base material. It is one of the most common road materials used in Southern Africa. Caliche is widely used as a base material when it is locally available and cheap. However, it does not hold up to moisture (rain), and is never used if a hard-rock base material, such as limestone, is available.

Sugar refining

A nearly pure source of calcium carbonate is necessary to refine sugar. It must contain at least 95% calcium carbonate (CaCO3) and have a low magnesium content. In addition, the material must meet certain physical requirements so it does not break down when burned. Although caliche does not generally meet all of the requirements for sugar refining, it is used in areas where another source of calcium carbonate, such as limestone, is not present. While caliche requires beneficiation to meet the requirements, its use can still be significantly cheaper than shipping in limestone.

Chilean caliche

In the Atacama Desert in northern Chile, vast deposits of a mixture, also referred to as caliche, are composed of gypsum, sodium chloride and other salts, and sand, associated to salitre ("Chile saltpeter"). Salitre, in turn, is a composite of sodium nitrate (NaNO3) and potassium nitrate (KNO3). Salitre was an important source of export revenue for Chile until World War I, when Europe began to produce both nitrates industrially in large quantities.

These deposits are the largest known natural source of nitrates in the world, containing up to 25% sodium nitrate and 3% potassium nitrate, as well as iodate minerals, sodium chloride, sodium sulfate, and sodium borate (borax). The caliche beds are from 0.2 to 5.0 m thick, and they are mined and refined to produce a variety of products, including sodium nitrate (for agriculture or industry uses), potassium nitrate, sodium sulfate, iodine, and iodine derivatives.

Caliche and agriculture

Problems caused by caliche

Caliche beds can cause problems for agriculture. First, an impermeable caliche layer prevents water from draining properly, which can keep roots from getting enough oxygen. Salts can also build up in the soil due to the lack of drainage. Both of these situations are detrimental to plant growth. Second, the impermeable nature of caliche beds prevents plant roots from penetrating the bed, which limits the supply of nutrients, water, and space so they cannot develop normally. Third, caliche beds can also cause the surrounding soil to be basic. The basic soil, along with calcium carbonate from the caliche, can prevent plants from getting enough nutrients, especially iron. An iron deficiency makes the youngest leaves turn yellow. Soil saturation above the caliche bed can make the condition worse.

A caliche layer with the presence of calcium carbonates indicates alkaline or high-pH conditions.

See also


  1. ^ Breazeale, J.F.; Smith, H.V. (15 April 1930). "Caliche in Arizona". Agricultural Experiment Station Bulletin. University of Arizona. 131: 419.
  2. ^ Gile, L. H.; Peterson, F. F.; Grossman, R. B. (February 1965). "The K Horizon". Soil Science. 99 (2): 74–82. Bibcode:1965SoilS..99...74G. doi:10.1097/00010694-196502000-00002. S2CID 129247211.
  3. ^ a b Allaby, Michael, ed. (2013). "Caliche". A dictionary of geology and earth sciences (Fourth ed.). Oxford: Oxford University Press. ISBN 9780199653065.
  4. ^ Chong et al. 2007, p. 211.
  5. ^ A Most Damnable Invention: Dynamite, Nitrates, and the Making of the Modern World, Stephen R. Bown, Macmillan, 2005, ISBN 0-312-32913-X, p. 157.
  6. ^ Blatt, Harvey; Middleton, Gerard; Murray, Raymond (1980). Origin of sedimentary rocks (2d ed.). Englewood Cliffs, N.J.: Prentice-Hall. pp. 273–275. ISBN 0136427103.
  7. ^ Blatt, Middleton & Murray 1980, pp. 274-275.
  8. ^ Breazeale & Smith 1930, pp. 420, 428-429.
  9. ^ Blatt, Middleton & Murray 1980, p. 274.
  10. ^ C. Michael Hogan (2008) Makgadikgadi, The Megalithic Portal, ed. A. Burnham [1]

Further reading

  • Price, William Armstrong. Reynosa Problem of Southern Texas, and Origin of Caliche. Bulletin of the American Association of Petroleum Geologists 17.5 (1933): 488–522.
  • Reeves, C.C., Jr. Caliche: Origin, Classification, Morphology and Uses. Lubbock, Texas: Estacado Books, 1976.
  • Reeves, C.C., Jr. and J.D. Suggs. Caliche of Central and Southern Llano Estacado, Texas: Notes. Journal of Sedimentary Petrology 34.3 (1964): 669–672.
  • Chong Diaz, Guillermo; Gajardo Cubillos, Aníbal; Hartley, Adrian J.; Moreno, Teresa (2006). "7. Industrial minerals and rocks". In Moreno, Teresa; Gibbons, Wes (eds.). Geology of Chile. Geological Society of London. pp. 21–114. ISBN 9781862392199.

External links

This page was last edited on 21 January 2021, at 12:24
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