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the zone of aeration
The unique characteristics of water bodies in the equatorial zone is that they are polar and geometry bent.
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 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.
The sun’s rays hit the surface directly.
The aquifer zone that lies between the water table and Earth's surface is called the unsaturated zone or vadose zone. This zone contains soil and rock layers where pores are not completely filled with water, allowing for the movement of both water and air.
Its when a Aquifer recharges bc the surface has to much water realeasing the discharge of water.
aeration zone
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.
The open water zone is beneath the littoral zone and is only as light can reach. The deep water zone is below the open water zone where no light reaches
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The midnight zone, also known as the abyssopelagic zone, is typically found in cold water. This zone lies between about 3,280 to 13,124 feet (1,000 to 4,000 meters) below the ocean surface, where temperatures are generally colder due to the lack of sunlight and proximity to deep ocean currents.