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- Clay abstract "Clay is a fine-grained soil that combines one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure.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, but there is some overlap in both particle size and other physical properties, and there are many naturally occurring deposits which include silts and also 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. 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.".
- Clay thumbnail Gay_head_cliffs_MV.JPG?width=300.
- Clay wikiPageExternalLink organic_matter_in_clays_detailed_overview_325.html.
- Clay wikiPageExternalLink crystal.htm.
- Clay wikiPageExternalLink www.clays.org.
- Clay wikiPageExternalLink 43-2-255.pdf.
- Clay wikiPageExternalLink plasticity.html.
- Clay wikiPageExternalLink cmg.html.
- Clay wikiPageExternalLink nomenclaturecl1.htm.
- Clay wikiPageExternalLink clays-used-in-the-pottery-industry.en.
- Clay wikiPageID "36980".
- Clay wikiPageRevisionID "606176768".
- Clay hasPhotoCollection Clay.
- Clay subject Category:Natural_materials.
- Clay subject Category:Phyllosilicates.
- Clay subject Category:Sculpture_materials.
- Clay subject Category:Sedimentology.
- Clay subject Category:Sediments.
- Clay subject Category:Types_of_soil.
- Clay comment "Clay is a fine-grained soil that combines one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure.Clays are distinguished from other fine-grained soils by differences in size and mineralogy.".
- Clay label "Arcilla".
- Clay label "Argila".
- Clay label "Argile".
- Clay label "Argilla".
- Clay label "Clay".
- Clay label "Glina".
- Clay label "Klei".
- Clay label "Ton (Bodenart)".
- Clay label "Глина".
- Clay label "صلصال".
- Clay label "粘土".
- Clay label "黏土".
- Clay sameAs Jíl.
- Clay sameAs Ton_(Bodenart).
- Clay sameAs Άργιλος.
- Clay sameAs Arcilla.
- Clay sameAs Buztin.
- Clay sameAs Argile.
- Clay sameAs Lempung.
- Clay sameAs Argilla.
- Clay sameAs 粘土.
- Clay sameAs 점토.
- Clay sameAs Klei.
- Clay sameAs Glina.
- Clay sameAs Argila.
- Clay sameAs m.0975t.
- Clay sameAs Q42302.
- Clay sameAs Q42302.
- Clay wasDerivedFrom Clay?oldid=606176768.
- Clay depiction Gay_head_cliffs_MV.JPG.
- Clay isPrimaryTopicOf Clay.
