Given below are two statements, one is labelled as

Solution

When water moves from a fine-textured soil (e.g., clay or silt) to a layer of coarse sand, the larger pore spaces in the sand allow for faster water movement. This temporary increase in downward movement occurs until the soil suction, or the force that pulls water into the soil, is reduced enough for equilibrium to be reached. Macrospores are larger pores or channels present in coarse-textured soils, such as sand, that can quickly transport water.