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Montmorillonite swells on wetting because water enters

  • A.between its structural layers
  • B.the voids between its grains only
  • C.its silicon-oxygen tetrahedra
  • D.its exchangeable cation sites only

Answer: A

Correct answer: between its structural layers

Montmorillonite has weakly bonded layers, and water molecules and cations enter the space between them, forcing them apart. The volume change can be several times, and it is reversible on drying - which is why an expansive soil heaves in the wet season and shrinks and cracks in the dry.

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