Step 1: Understanding the Concept:
Irrigation water containing elevated concentrations of sodium (\(\text{Na}^+\)) relative to divalent cations (\(\text{Ca}^{2+}\) and \(\text{Mg}^{2+}\)) affects soil physical properties.
High exchangeable sodium on soil particles leads to soil dispersion (deflocculation) rather than flocculation.
Step 2: Detailed Explanation:
1. Sodium is a highly hydrated monovalent ion with a weak charge density. When it dominates the exchange complex, it causes soil colloid swelling and dispersion of soil aggregates (deflocculation).
2. Dispersed clay particles clog macro-pores in the soil. This structural deterioration creates a dense, compacted layer that impairs water infiltration and limits soil aeration.
3. This block in soil aeration decreases oxygen diffusion rate (ODR), resulting in poor oxygen supply to the root system, which validates the Assertion.
4. Since sodium causes dispersion (deflocculation) and not flocculation, the Reason is scientifically incorrect.
Step 3: Final Answer:
Assertion (A) is correct and Reason (R) is false.