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The 24 pages that link to Clay mineral, each with the reason it gives.

• Silicate mineralBroader topic: Clay minerals connect silicate weathering to soils, sediments, and industrial materials.

• MineralBroader topic: Clay minerals shape soils and are widely used in ceramics and construction.

• Soil structureRelated: Their surface charges and swelling behavior shape aggregate formation and pore geometry.

• Chemical weatheringBroader topic: Clay minerals are common products of silicate alteration by water.

• Cation-Exchange CapacityNarrower topic: Clay mineral type and abundance strongly shape a soil’s CEC.

• ClayBroader topic: Their layered structures give clay its characteristic plasticity and water interaction.

• AluminosilicateBroader topic: Layered aluminosilicate sheets give clays their distinctive swelling and surface behavior.

• CompactionRelated: Their small size and platy shape make clay-rich sediment especially compressible.

• Soil aggregationRelated: Their surfaces attract ions and organic compounds that help bind fine particles.

• Isomorphous substitutionBroader topic: Layered clays commonly host substitutions that generate permanent charge.

• Silicate weatheringRelated: They are frequent solid products of silicate mineral alteration.

• KaolinNarrower topic: Kaolin is a clay-rich material made chiefly from one clay mineral.

• ShaleRelated: These minerals commonly dominate shale’s fine-grained matrix.

• SlateRelated: Clay minerals in slate’s precursor rocks help develop its fine-grained fabric.

• KaoliniteNarrower topic: Kaolinite is one member of this broad mineral class.

• Chlorite groupCompared with: Fine-grained chlorite can be mistaken for clay minerals in sediment and rock analysis.

• MudstoneRelated: Clay minerals commonly make up much of mudstone’s finest fraction.

• Soil chemistryBroader topic: Their charged layers and edges provide major sites for ion exchange and adsorption.

• Earth pigmentRelated: Clay minerals often form the matrix that holds pigment particles together.

• GeophagiaBroader topic: Some geophagic earths are clay-rich, and their mineral structure can affect what they bind.

• MudrockRelated: Clay minerals make up much of mudrock’s finest fraction and strongly affect its behavior.

• Fire (ceramics)Narrower topic: Clay minerals lose water and change structure as ceramic bodies are fired.

• HectoriteNarrower topic: Hectorite is a clay mineral whose fine grains and water interactions shape its behavior.

• Modelling clayNarrower topic: They are the mineral basis of many traditional water-based clays, unlike oil and polymer formulations.