Saturated Soil
Title
Once the soil has been modeled, it is possible to study how the water moves through it. Studying the situation on the ground, it is seen that it is the pressure difference that indicates the movement. Due to the narrowness of the channels that are formed between the grains, the resulting flow is of the laminar type. With this it is possible to determine, depending on the microscopic parameters and macroscopic conditions, the resulting flow in the soil.
ID:211
