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Encyclopedia > Artesian
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Geological strata giving rise to an Artesian well

An artesian aquifer is an aquifer whose water is overpressurized. Water will thus flow out of an artesian well without pumping.


Why is a well artesian?

Because its recharge zone is higher than the head of the well.


Pascal's Law predicts the overpressure:

 Poverpressure = ρg(zrecharge - zwellhead) 

where ρ is the volumic mass of the fluid, g the acceleration due to gravity, and z is height.


Origin

Artesian wells are named after the town of Artois in France, where the first one was drilled by Carthusian monks in 1126. [1] (http://scholar.chem.nyu.edu/tekpages/artesian.html) (see also Note 1: )


Notes

Note 1: Frances and Joseph Gies, Cathedral, Forge, and Waterwheel subtitled "Technology and Invention in the Middle Ages". Harper Perennial, 1995 ISBN 0060165901, page 112.






  Results from FactBites:
 
Artesian aquifer - Wikipedia, the free encyclopedia (240 words)
An artesian aquifer is a confined aquifer containing groundwater that will flow upwards out of a well without the need for pumping.
In recharging aquifers, this happens because the water table at its recharge zone is at a higher elevation than the head of the well.
Artesian wells were named after the former province of Artois in France, where many artesian wells were drilled by Carthusian monks since 1126 (see also
KGS--Meade County--Artesian Water (5259 words)
The piezometric surface, or pressure-indicating surface, of an artesian aquifer is an imaginary surface that everywhere coincides with the static level, or head, of the water in the aquifer.
Precipitation that falls in the discharge area of an artesian basin has no effect upon the ground-water level, or pressure head, for in such areas the artesian water is effectively sealed from the surface by impervious beds or else the artesian pressure could not be maintained.
As the total annual discharge of artesian water is estimated to be 10,000 acre-feet, and if the recharge is assumed to be equal to the discharge, this indicates that an average recharge of about 0.27 inches may reach the water table in the areas described.
  More results at FactBites »


 

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