Water rises most rapidly in sandy soil. This is because sandy soil has large spaces or pores between the sand particles, which allows water to flow through quickly, increasing the rate of water movement. In contrast, clayey soil has very small spaces or pores, which causes water to move more slowly through the soil. Loamy soil is a mixture of sand, silt, and clay, which can have varying rates of water movement depending on the proportions of each component. Humus soil refers to soil that has a high content of organic matter, which can help improve soil structure and water-holding capacity, but may not necessarily affect the rate of water movement.