pinnafiltratsiooniks
Pinnafiltratsiooniks, often referred to as surface infiltration, describes the process by which water penetrates the topmost layer of soil. This is a crucial initial step in the overall infiltration process, which is the movement of water into the ground. The rate of surface infiltration is influenced by several factors, including the soil's texture, structure, moisture content, and the presence of surface cover like vegetation or litter.
Porous soils with good structure, such as sandy loams, tend to exhibit higher surface infiltration rates than
Understanding surface infiltration is vital in hydrology and environmental science. It plays a key role in