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Artesian aquifer

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Geological strata giving rise to an Artesian well
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Geological strata giving rise to an Artesian well

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

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Why is a well artesian?

Because the water table at its recharge zone is at a higher elevation than the head of the well.

Pascal's Law predicts the hydrostatic pressure:

P = \rho \cdot g \cdot (z_{recharge}-z_{wellhead})

where ρ is the density of the fluid, g the acceleration due to gravity, and z is the elevation.

Origin

Artesian wells are named after the former province 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: )

See also

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.es:Pozo artesiano et:Arteesiakaev th:บ่อน้ำบาดาล

Wikipedia (http://en.wikipedia.org/wiki/Main_Page) Artesian (http://en.wikipedia.org/wiki/Artesian) version history (http://en.wikipedia.org/w/index.php?title=Artesian&action=history) GNU Free Documentation Lizenz (http://en.wikipedia.org/wiki/Wikipedia:Text_of_the_GNU_Free_Documentation_License) CC-by-sa (http://creativecommons.org/licenses/by-sa/2.5/)

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