Step 1: Understanding the Concept:
Water movement in unsaturated soils is driven by matric suction (capillary forces).
Fine-textured soils have small pores (micropores) that exert high suction forces, while coarse-textured soils (like sand) have large pores (macropores) that exert very low suction forces.
Step 2: Detailed Explanation:
Let us analyze both statements:
- Assertion A: "When the water moving downward through a fine textured soil encounters a layer of coarse sand, the downward movement is temporarily increased..."
This statement is incorrect.
When a wetting front moving through a fine-textured soil encounters a layer of coarse sand, the downward movement actually stops or is delayed temporarily.
This phenomenon is known as a capillary barrier.
Because the micropores in the fine soil have a high affinity for water, the water will not move into the larger macropores of the coarse sand until the fine soil layer directly above the sand becomes nearly saturated (reducing its matric suction to near zero). Only then can water flow into the sand.
- Reason R: "Presence of large macropores in the coarse sand are too large to take in water from the unsaturated micropores of the soil rapidly."
This statement is correct.
Under unsaturated conditions, the matric suction of the micropores in the fine soil is much higher than that of the macropores in the coarse sand.
The large pores in the sand cannot exert enough suction to pull water out of the smaller pores of the fine soil, preventing rapid water movement across the boundary.
Therefore, Assertion A is false, but Reason R is true.
Step 3: Final Answer:
The correct option is (D).