jeol. tabansuyu düzeyi, yeraltı suyu düzeyi

listen to the pronunciation of jeol. tabansuyu düzeyi, yeraltı suyu düzeyi
Turkish - English
water table
The level, underground, below which the ground is saturated with water
A point below the surface of the land, below which the earth is saturated with water
the top surface of groundwater where all the spaces between soil particles and rocks are filled with water The boundary bewteen where the ground is saturated with water and where the ground is filled with water and air
The upper level of water saturation in the ground
The depth, usually expressed in feet, from the surface of your land to the level at which natural ground water is found
underground surface below which the ground is wholly saturated with water; "spring rains had raised the water table
The upper limit or surface of the groundwater which follows approximately the profile of the land-surface
The upper limit of the portion of the ground wholly saturated with water
The upper surface of ground water, below which all materials are considered to be saturated with water
The level below the earth's surface at which the ground becomes saturated with water The water table is set where hydrostatic pressure equals atmospheric pressure
level below the earth's surface at which the ground becomes saturated with water
The top of the water surface in the saturated part of an aquifer
the upper surface of the saturated zone of groundwater
the water surface in an unconfined aquifer; the level below which the pore spaces in the soil or rock are saturated with water; the upper surface of the zone of saturation
The natural accumulation of water either above or below ground, often used for well purposes May also refer to the distance from the surface of the land to the location of the water
The upper surface of a body of unconfined ground water at which the water pressure is equal to the atmospheric pressure
The upper surface of groundwater Below it, the soil is saturated with water
9, that is, for the table at the top of the foundation and the beginning of the upper wall
A fluctuating demarcation line between the unsaturated (vadose) zone and the saturated (phreatic) zone that forms an aquifer It may rise or fall depending on precipitation (rainfall) trends The water table is semiparallel to the land surface above but is not always a consistent straight line Because of impervious beds of shale, etc , local water tables can be perched above the area's average water table
underground surface below which the ground is wholly saturated with water; "spring rains had raised the water table"
jeol. tabansuyu düzeyi, yeraltı suyu düzeyi
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