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Smectite clays layer rigidity

The clay minerals are distinguished by their size (<2-3 pm) and extremely active surface chemistry. A few clay minerals, such as micas, do occur in silt and larger sizes. The most common clay mineral groups are those of kaolinite, smectite, and illite. Kaolinitic minerals are characterized by a rigidly held, hydrogen-bonded, nonexpansive, double-layer... [Pg.224]

See other pages where Smectite clays layer rigidity is mentioned: [Pg.427] [Pg.84] [Pg.84] [Pg.88] [Pg.3] [Pg.3] [Pg.20] [Pg.99] [Pg.370] [Pg.379] [Pg.105]

See also in sourсe #XX -- [ Pg.3 ]

See also in sourсe #XX -- [ Pg.3 ]

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Clay layers

Clays smectites

LAYER RIGIDITY

Layered clays

Smectite

Smectite clays

Smectites