Beware of the gusher!
The elevation of a water table is indicated by the elevation at which, free water rises in a test hole. Consequently, it should be realized that it takes time for the water to accumulate in the hole. The amount of time depends on the rate of flow, of the groundwater from the adjacent soils. If the soil is pervious; the water in the test hole will rise to the water table within a very short time; but if it is relatively impervious, considerable time may be required for the water to rise to the true water-table elevation.
Don't get in a tizy
A good rule of thumb, is to allow the test hole to stand for 24 hours after the hole has been dug before the elevation of the water is measured. If the soil and the region of the water table is characteristically known to be
freely pervious, this time-lag period is not necessary.
Big Surprise
If, while drilling a test bore and you make an unfortunate discovery like an artisan well. "Oh Boy," your day has just begun, and mandatory overtime for everybody; this is a horse of a different color, because the flow must be stopped and the hole plugged. It gets a little hairy at this point. A helical auger may be rotated in reverse, and soil packed back into the hole. If this is not possible or if flow continues; immediately after withdrawing the auger a bentonite clay plug may be driven in with a timber, which then is cemented with Portland cement. If the flow continues it will draw down the ground water level,
dry up wells, and cause surface erosion, ponding, and flooding. The worst case scenario is, a rapidly flowing uncased artisan well that will quickly erode a gaping hole that may be exceedingly difficult to plug.
Even when there is no artisan pressure, boring's in sand below the aquifer tend to cave in if the drilling tools are withdrawn, and may even cave in during the drilling operation, oweing this unfortunate circumstance to seepage of water into the drill hole, which causes a "quick" condition. This may impede penetration of the drill and result in excavation of an underground cavern. The unexpected collapse of such caverns may endanger near by foundations or the driller.
Adjustments to the Water table
A water table can be lowered artificially by providing an outlet for the groundwater at a level below its natural outlet by means of open ditches or by tile under-drains. It must be realized however, that the new water table will not be lowered to the new elevation of the drains themselves, except right in the vicinity of the drains, because the natural tendency for a water table to rise as the distance from an outlet or point of release increases. The steepness of the water table in the vicinity of the drain depends on the characteristics of the soil, being relatively flat in a permeable soil and relatively steep in a impermeable soil. Thanks for the comments. Have a good day!!
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