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Clay

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Title: Clay  
Author: World Heritage Encyclopedia
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Subject: Economy of Estonia, Pencil, Pottery, Grain size, Angle of repose
Collection: Clay, Natural Materials, Phyllosilicates, Sculpture Materials, Sedimentology, Sediments, Soil-Based Building Materials, Types of Soil
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Clay

The Gay Head cliffs in Martha's Vineyard consist almost entirely of clay.

Clay is a fine-grained soil that combines one or more

  • Building the Phyllosilicates University of New Hampshire
  • The Clay Minerals Group of the Mineralogical Society
  • Information about clays used in the UK pottery industry
  • The Clay Minerals Society
  • Plasticity of clay
  • Organic Matter in Clays

External links

  • Hillier S. (2003) Clay Mineralogy. pp 139–142 In: Middleton G.V., Church M.J., Coniglio M., Hardie L.A. and Longstaffe F.J.(Editors) Encyclopedia of sediments and sedimentary rocks. Kluwer Academic Publishers, Dordrecht.
  • Ehlers, Ernest G. and Blatt, Harvey (1982). 'Petrology, Igneous, Sedimentary, and Metamorphic' San Francisco: W.H. Freeman and Company. ISBN 0-7167-1279-2.
  • Guggenheim, Stephen; Martin, R. T. (1995), "Definition of clay and clay mineral: Journal report of the AIPEA nomenclature and CMS nomenclature committees", Clays and Clay Minerals 43 (2): 255–256,  
  • Clay mineral nomenclature American Mineralogist.

References

  1. ^ a b Guggenheim & Martin 1995, pp. 255–256
  2. ^ a b Environmental Characteristics of Clays and Clay Mineral Deposits - USGS
  3. ^ Scarre, C. 2005. The Human Past, Thames and Hudson:London, P.238
  4. ^ Koçkar, Mustafa K.; Akgün, Haluk; Aktürk, Özgür, Preliminary evaluation of a compacted bentonite / sand mixture as a landfill liner material (Abstract). Department of Geological Engineering, Middle East Technical University, Ankara, Turkey
  5. ^ http://macawproject.org/component/content/article/44-main-menu/47-intro
  6. ^ Evolutionary biology: Dirty eating for healthy living by Jared M. Diamond

Footnotes

See also

Clay is one of the oldest building materials on wood. Between one-half and two-thirds of the world's population, in traditional societies as well as developed countries, still live or work in a building made with clay as an essential part of its load-bearing structure. Also a primary ingredient in many natural building techniques, clay is used to create adobe, cob, cordwood, and rammed earth structures and building elements such as wattle and daub, clay plaster, clay render case, clay floors and clay paints and ceramic building material. Clay was used as a mortar in brick chimneys and stone walls where protected from water.

As a building material

A traditional use of clay as medicine goes back to prehistoric times. An example is Armenian bole, which is used to soothe an upset stomach, similar to the way parrots (and later, humans) in South America originally used it.[6] Kaolin clay and attapulgite have been used as anti-diarrheal medicines.

Recent research indicates that macaws visit clay licks periodically to eat from them.[5]

Medicinal uses

Recent studies have investigated clay's absorption capacities in various applications, such as the removal of heavy metals from waste water and air purification.

Clay, being relatively impermeable to water, is also used where natural seals are needed, such as in the cores of dams, or as a barrier in landfills against toxic seepage (lining the landfill, preferably in combination with geotextiles).[4] (See Puddling.)

Clays sintered in fire were the first form of ceramic. Bricks, cooking pots, art objects, dishware, and even musical instruments such as the ocarina can all be shaped from clay before being fired. Clay is also used in many industrial processes, such as paper making, cement production, and chemical filtering. Clay is also often used in the manufacture of pipes for smoking tobacco. Until the late 20th century bentonite clay was widely used as a mold binder in the manufacture of sand castings.

Clay tablets were the first known writing medium. Scribes wrote by inscribing them with cuneiform script using a blunt reed called a stylus. Purpose-made clay balls were also used as sling ammunition.

Clays exhibit plasticity when mixed with water in certain proportions. When dry, clay becomes firm and when fired in a kiln, permanent physical and chemical changes occur. These reactions, among other changes, convert the clay into a ceramic material. Because of these properties, clay is used for making pottery, both utilitarian and decorative, and construction products, such as bricks, wall and floor tiles. Different types of clay, when used with different minerals and firing conditions, are used to produce earthenware, stoneware, and porcelain. Prehistoric humans discovered the useful properties of clay. Some of the earliest pottery shards recovered are from central Honshu, Japan. They are associated with the Jomon culture and deposits they were recovered from have been radiocarbon dated to around 14,000 BC.[3] Depending on the content of the soil, clay can appear in various colors, from a dull gray to a deep orange-red.

Clay layers in a construction site. Dry clay is normally much more stable than sand with regard to excavations.

Historical and modern uses

Quick clay is a unique type of marine clay indigenous to the glaciated terrains of Norway, Canada, Northern Ireland, and Sweden. It is a highly sensitive clay, prone to liquefaction, which has been involved in several deadly landslides.

deposit is common in former glacial lakes. When glacial lakes form, their water moves very little, and these eroded soils settle on the lake bed. This allows such an even distribution on the different layers of clay.[2]

Depending on the academic source, there are three or four main groups of clays: kaolinite, montmorillonite-smectite, illite, and chlorite. Chlorites are not always considered a clay, sometimes being classified as a separate group within the phyllosilicates. There are approximately 30 different types of "pure" clays in these categories, but most "natural" clays are mixtures of these different types, along with other weathered minerals.

Grouping

Primary clays, also known as kaolins, are located at the site of formation. Secondary clay deposits have been moved by erosion and water from their primary location.[2]

Clay minerals typically form over long periods of time from the gradual chemical weathering of rocks, usually silicate-bearing, by low concentrations of carbonic acid and other diluted solvents. These solvents, usually acidic, migrate through the weathering rock after leaching through upper weathered layers. In addition to the weathering process, some clay minerals form by hydrothermal activity. Clay deposits may form in place as residual deposits in soil, but thick deposits usually form as the result of a secondary sedimentary deposition process after they have been eroded and transported from their original location of formation. Clay deposits are typically associated with very low energy depositional environments such as large lakes and marine basins.

Deforestation for clay extraction in Rio de Janeiro city - Brazil. The picture is of Morro da Covanca - Jacarepaguá.

Formation

Contents

  • Formation 1
  • Grouping 2
  • Historical and modern uses 3
    • Medicinal uses 3.1
    • As a building material 3.2
  • See also 4
  • Footnotes 5
  • References 6
  • External links 7
Quaternary clay in Estonia.

Clays are distinguished from other fine-grained soils by differences in size and mineralogy. Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however some overlap in particle size and other physical properties, and many naturally occurring deposits include both silts and clay. The distinction between silt and clay varies by discipline. Geologists and soil scientists usually consider the separation to occur at a particle size of 2 µm (clays being finer than silts), sedimentologists often use 4-5 μm, and colloid chemists use 1 μm.[1] Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils' Atterberg limits. ISO 14688 grades clay particles as being smaller than 2 μm and silts larger.

Electron microscope photograph of smectite clay - magnification 23,500

containing variable amounts of water trapped in the mineral structure. phyllosilicate minerals are mostly composed of deposits Geologic clay [1]

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