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The top saturated zone is called the water table.
water table
The water table sits on top of the soil zone.
The water table or phreatic surface.
The top of the saturated zone of groundwater is called the water table. It represents the boundary between the saturated and unsaturated zones in the ground.
The water table acts as the boundary between the aeration zone and saturation zone. Below the water table, the pores are fully saturated with water, while above the water table, there is both air and water in the soil pores.
The saturated zone is where the spaces between soil and rock particles are filled with water, while the unsaturated zone is where some of these spaces contain air as well as water. In the saturated zone, the water table is located at the top of this zone, whereas in the unsaturated zone, the water table is below the surface.
Groundwater is found in the zone known as the saturated zone, where all spaces between the soil and rock particles are filled with water. This zone lies beneath the water table, which is the top boundary of the saturated zone.
This condition is known as saturated zone or water-saturated zone. It occurs in areas where all pores in the rock are filled with water, creating a water-saturated environment. Groundwater is typically found in the saturated zone.
The water table is located at the top of the zone of saturation, where soil and rock are completely saturated with water. It is not generally found under the zone of saturation. The water table is typically above the layer of bedrock. It is usually located above the layer of bedrock, not below it.
water table
The level below which the ground is saturated with water is known as the water table. It represents the top of the saturated zone in an aquifer where the pore spaces between soil and rock particles are filled with water.