title: The effect of the earth's rotation on ground water motion.
abstract: The average pore velocity of ground water according to Darcy's law is a function of the fluid pressure gradient and the gravitational force (per unit volume of ground water) and of aquifer properties. There is also an acceleration exerted on ground water that arises from the Earth's rotation. The magnitude and direction of this rotation-induced force are determined in exact mathematical form in this article. It is calculated that the gravitational force is at least 300 times larger than the largest rotation-induced force anywhere on Earth, the latter force being maximal along the equator and approximately equal to 34 N/m(3) there. This compares with a gravitational force of approximately 10(4) N/m(3).
authors.affiliation: Department of Geography, University of California, Santa Barbara, CA 93106, USA. hugo@geog.ucsb.edu
authors.forename: Hugo A
authors.initials: HA
authors.lastname: Loáiciga
mesh_terms: D003312:Coriolis Force; D018534:Earth, Planet; D005618:Fresh Water; D006112:Gravitation; D012399:Rotation; D012987:Soil; D014872:Water Movements
chemical_list: D012987:Soil