Step 1: Understanding the Question:
This question explores the phenomenon of "Soil Water Hysteresis"—the fact that the relationship between soil moisture and matric potential depends on the soil's history (whether it is getting wetter or drier).
Detailed Explanation:
• Assertion A Analysis (True):
Hysteresis means "lagging behind." For a given matric potential (e.g., $100$ cm suction), a soil that is drying out will hold more water than a soil that is currently being wetted.
The desorption curve always lies above the sorption curve on a moisture characteristic graph.
• Reason R Analysis (True):
Contact angle hysteresis is one of the four main causes of soil water hysteresis.
The "advancing" contact angle (during wetting/imbibition) is larger than the "receding" contact angle (during drying/drainage).
Since the radius of curvature of the water meniscus depends on the contact angle (\( r = R \cos \alpha \)), the suction required to empty a pore (drying) is different from the suction required to fill it (wetting).
• Other Causes of Hysteresis:
- Ink-bottle effect: Pores have narrow necks and wide bodies.
- Trapped air: Air bubbles prevent some pores from re-wetting fully.
- Swelling/Shrinking: Soil structure changes as moisture changes.
• Logical Link:
Because the contact angle is different during the two processes, the water behaves differently at the same potential. Thus, Reason R is a valid physical explanation for Assertion A.
Step 2: Final Answer:
Both statements are scientifically correct, and the reason (contact angle hysteresis) is one of the primary drivers of the observed moisture hysteresis.