About: Clay mineral X-ray diffraction

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Clay minerals are one of the most diverse minerals but all have a commonalty of crystal or grain sizes below 2 μm. Chemically, clays are defined by crystal structure and chemical composition. Sometimes fine grain sediments are mistakenly described as clays; this is actually a description of the "clay-size fraction" rather than the mineralogy of the sediment. There are three crystallographic clay groups: platy clays (phyllosilicates), fibrous clay minerals, and amorphous clay. Phyllosilicates are the most abundant clays and are categorized based on the layering of a tetrahedral and octahedral layer. For most clays, the octahedral layer is centered with Al3+, Fe3+, or Mg(OH)2, but sometimes Zn2+, Li+, and Cr3+ can substitute as well. Si4+ is normally the center of the tetrahedral layer but A

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rdfs:label	Clay mineral X-ray diffraction (en)
rdfs:comment	Clay minerals are one of the most diverse minerals but all have a commonalty of crystal or grain sizes below 2 μm. Chemically, clays are defined by crystal structure and chemical composition. Sometimes fine grain sediments are mistakenly described as clays; this is actually a description of the "clay-size fraction" rather than the mineralogy of the sediment. There are three crystallographic clay groups: platy clays (phyllosilicates), fibrous clay minerals, and amorphous clay. Phyllosilicates are the most abundant clays and are categorized based on the layering of a tetrahedral and octahedral layer. For most clays, the octahedral layer is centered with Al3+, Fe3+, or Mg(OH)2, but sometimes Zn2+, Li+, and Cr3+ can substitute as well. Si4+ is normally the center of the tetrahedral layer but A (en)
foaf:depiction
dcterms:subject	X-ray crystallography
Wikipage page ID	42430141 (xsd:integer)
Wikipage revision ID	1095011943 (xsd:integer)
Link from a Wikipage to another Wikipage	Amorphous solid Quartz Mortar and pestle X-ray crystallography Homogeneous Lithium Standard deviation Clay mineral Octahedral Phyllosilicates Magnesium hydroxide Zinc Suspension (chemistry) Aluminium Centrifuge Chromium Diffraction pattern Iron Chloride Chlorite Coefficient of variation X-ray diffraction X-rays Silicate Mineralogy Sediments X-ray crystallography Microscope slide Silicon Tetrahedral Serpentine group Settling velocity Sieving Vacuum filter Bragg’s law dbr:Clay_Mineral_Society
sameAs	Clay mineral X-ray diffraction Clay mineral X-ray diffraction Clay mineral X-ray diffraction
dbp:wikiPageUsesTemplate	dbt:Multiple_issues dbt:Reflist dbt:Technical dbt:Tone
thumbnail	wiki-commons:Special:FilePath/Cross_Section_of_Kaolinite_and_Pyophyllite.png?width=300
has abstract	Clay minerals are one of the most diverse minerals but all have a commonalty of crystal or grain sizes below 2 μm. Chemically, clays are defined by crystal structure and chemical composition. Sometimes fine grain sediments are mistakenly described as clays; this is actually a description of the "clay-size fraction" rather than the mineralogy of the sediment. There are three crystallographic clay groups: platy clays (phyllosilicates), fibrous clay minerals, and amorphous clay. Phyllosilicates are the most abundant clays and are categorized based on the layering of a tetrahedral and octahedral layer. For most clays, the octahedral layer is centered with Al3+, Fe3+, or Mg(OH)2, but sometimes Zn2+, Li+, and Cr3+ can substitute as well. Si4+ is normally the center of the tetrahedral layer but Al3+ will often partially substitute and create a charge imbalance. Two-layer clays are composed of a tetrahedral layer and an octahedral layer (T-O) while three-layer clays contain an octahedral layer sandwiched by two tetrahedral layers (T-O-T). When substitution of Al3+ for Si4+ creates a charge imbalance, an interlayer cation will fill in between tetrahedral layers to balance the charge of the clay. (en)
prov:wasDerivedFrom	wikipedia-en:Clay_mineral_X-ray_diffraction?oldid=1095011943&ns=0
page length (characters) of wiki page	13639 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Clay_mineral_X-ray_diffraction
is Link from a Wikipage to another Wikipage of	Purnima Sinha Clay Clay Mineral X-Ray Diffraction
is Wikipage redirect of	Clay Mineral X-Ray Diffraction
is academic discipline of	Purnima Sinha
is foaf:primaryTopic of	wikipedia-en:Clay_mineral_X-ray_diffraction

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