Step 1: Understanding the Concept:
Clay expansion (swelling upon wetting and shrinkage upon drying) is driven by the internal crystal lattice structure and interlayer bonding strength.
Step 2: Detailed Explanation:
Montmorillonite is an expanding 2:1 layer silicate clay (composed of one alumina octahedral sheet sandwiched between two silica tetrahedral sheets).
Interlayer bonding between adjacent crystal layers is composed of weak Van der Waals forces.
Polar water molecules readily penetrate the expansive interlayer spaces, causing massive crystal swelling when wet, and wide, deep soil cracks upon drying (typical of Black Cotton Soils Vertisols).
Kaolinite (1:1) has strong hydrogen bonds preventing swelling.
Step 3: Final Answer:
Thus, swelling and shrinkage is distinct in Montmorillonite clay, matching option (D).