Abstract
CALCULATIONS concerning the flow of subterranean water have almost invariably hitherto been based upon the classical law of Darcy, published in 1856—a law which states that the quantity discharged is directly proportional to the head, and inversely proportional to the thickness of the stratum traversed. The terms are simple, and, for general purposes, are sufficiently close approximations to the truth.
Le Principe du Mouvement des Eaux Souterraines.
J. Versluys. Traduit du hollandais par F. Dassesse. Pp. 147. (Amsterdam: W. Versluys, 1912.) Price 7 francs.
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Le Principe du Mouvement des Eaux Souterraines . Nature 91, 134 (1913). https://doi.org/10.1038/091134a0
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DOI: https://doi.org/10.1038/091134a0