Step 1: Understanding the Concept:
Clay particles carry a negative surface charge, creating an electrostatic double layer in the soil solution.
The balance between electrostatic repulsive forces (characterized by the zeta potential) and attractive van der Waals forces determines whether clay particles will flocculate or disperse.
Step 2: Detailed Explanation:
The charge and size of exchangeable cations regulate the thickness of the diffuse double layer and the magnitude of the zeta potential:
1. Divalent cations like calcium ($\text{Ca}^{2+}$) and magnesium ($\text{Mg}^{2+}$) have a high charge density and a relatively thin hydration shell.
They compress the diffuse double layer surrounding clay particles, lowering the electrostatic repulsion (zeta potential) below a critical threshold.
This compression allows attractive van der Waals forces to bring the clay particles together, resulting in flocculation (aggregation). Thus, Statement I is true.
2. Monovalent sodium ($\text{Na}^+$) has a lower charge density and a large hydrated ionic radius.
When sodium dominates the exchange complex, it expands the diffuse double layer and increases the zeta potential.
This increase in electrostatic repulsion prevents clay particles from coming close enough for van der Waals forces to act, leading to the dispersion of clay particles and the degradation of soil structure. Thus, Statement II is true.
Step 3: Final Answer:
Both Statement I and Statement II are true, which corresponds to Option (A).