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Clay minerals are formed from tetrahedral and octahedral structural units, which combine to create various sheets and ultimately different clay minerals like kaolinite, montmorillonite, and illite. The document discusses the formation, properties, and structures of these minerals, including their swelling and shrinkage characteristics based on their bonding. Additionally, it covers soil structure types and the classification of soil water, including gravitational, adsorbed, and capillary water.

Author

arun017nitjsr

Language

EN