The top saturated zone is called the water table.
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.
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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.
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The upper level of a saturated rock is called the water table. This is the boundary between the unsaturated zone above and the saturated zone below, where all the pores and fractures in the rock are filled with water.
The underground region in the saturated zone where all spaces between rock and soil particles are filled with water is called the groundwater zone or the phreatic zone. This is where groundwater is stored and flows through permeable materials such as rock fractures or gravel.
The water table or phreatic surface.
The water table sits on top of the soil zone.
The layer underground where all empty spaces are filled with water is called the saturated zone or the phreatic zone. This zone is located below the water table, which is the upper boundary of the saturated zone where water pressure is equal to atmospheric pressure. Groundwater is stored in the saturated zone and is a vital source of drinking water for many communities.
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.
Rain that falls on the surface seeps down through the soil and into a zone called the zone of aeration or unsaturated zone where most of the pore spaces are filled with air. As it penetrates deeper it eventually enters a zone where all pore spaces and fractures are filled with water. This zone is called the saturated zone. The surface below which all openings in the rock are filled with water (the top of the saturated zone) is called the water table .The water table occurs everywhere beneath the Earth's surface. In desert regions it is always present, but rarely intersects the surface.