water table

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water table

The upper limit of the saturated area of the earth containing groundwater.The water table will be at varying depths depending on location and time of year.

References in periodicals archive ?
From the distributions it is clear that the control has a higher occurrence of a shallow perched water table than the raised beds.
Soils with a saturated hydraulic conductivity of the root-zone of at least 50 mm/h can have beds up to 4 m wide and still drain a perched water table in about 36 h (Hamilton 1995; Youngs 1999).
In the control as well as the raised beds the perched water table rapidly rose during rainfall events but there was a difference between the treatments in the height of rise and the rate of fall of the perched water table.
From the convex shape of the perched water table in Fig.
In 1988, however, rainfall exceeded pan evaporation almost every week from mid-May until late August; throughout this period the perched water table on top of the mottled zone remained quite high (Fig.
As the rootholes extend far upward, the higher the perched water table, the more water can flow into, and down, the rootholes penetrating into the mottled zone, and hence on to the restricting layer at the top of the pallid zone, causing water to perch there (cf.
This is demonstrated by the fact that, in the winter of 1987, which was not consistently wet, in nearby ploys that had been deep-ripped, build-up of the perched water table at 1.