Step 1: Understanding the Concept:
Soil water hysteresis is the phenomenon where the relationship between soil matric potential and water content is non-unique and depends on the wetting or drying history of the soil.
Step 2: Detailed Explanation:
- Assertion (A) is correct: A soil always retains more water at a given matric suction during drying (desorption) than during wetting (sorption).
- Reason (R) is correct: During imbibition (wetting), the advancing contact angle is larger ($\alpha_a > \alpha_r$).
Since the capillary suction head is related to the contact angle by:
\[ h = \frac{2\gamma \cos\alpha}{\rho_w g r} \]
A larger contact angle during wetting ($\alpha_a$) leads to a smaller $\cos\alpha$, reducing capillary suction at a given water content compared to drying.
Thus, the contact angle effect is a key thermodynamic cause of hysteresis, explaining why wetting curves lie below drying curves.
Step 3: Final Answer:
Both (A) and (R) are correct, and (R) is the correct explanation of (A).