This is known as the phreatic surface or water table.
Impermeable Rock
The area between the zone of saturation and the zone of aeration is called the capillary fringe. In this zone, water is held in the soil pores by capillary action, and it serves as a transition area where both air and water coexist. Above the capillary fringe lies the zone of aeration, which contains mostly air and some moisture.
The area immediately below the water table is called the zone of saturation. This zone is where spaces between soil and rock particles are filled with water. Groundwater is found in this zone and can be extracted through wells.
The zone of saturation would not be completely solid. However, the pore spaces would be filled with water.
the zone of aeration
The upper surface of the zone of saturation where all the pores are filled with water is called the water table. This is the boundary between the saturated zone below and the unsaturated zone above, where the soil or rock is not fully filled with water.
This is known as the phreatic surface or water table.
The upper surface of the zone of saturation is known as the water table. This is the level beneath the Earth's surface where the soil and rock are fully saturated with water. Above the water table lies the unsaturated zone, where both water and air are present in the soil and rock.
Impermeable Rock
Groundwater
Ground Water, which seeps into the soil and fills the cracks unerground.
The limit of the highest tide is the upper limit of the tidal zone, and the lowest of the low tides is the lower bound.
the zone of aeration
No, the zone of saturation is below the zone of aeration in the ground. The zone of saturation is where all spaces between soil particles are filled with water, while the zone of aeration is where there are air pockets between the soil particles.
Yes, the zone of aeration is located above the zone of saturation. The zone of aeration contains spaces filled with both air and water, whereas the zone of saturation is where all available spaces are filled with water.
Groundwater is found below the surface in the zone of saturation, where all pores and spaces in the soil or rock are filled with water. This zone lies beneath the water table, which represents the upper surface of the groundwater.