Abstract
The effect of the friction has been studied on the one
dimensional motion of a viscous fluid. This friction is usually schematized in
various semiempirical formulae. In t-liis work the different scliematizations
of the friction were not studied separately but it was shown that a solution
exists for the fluid motion. The results give information on the damping of
the fluid motion in the case of the seiches.
dimensional motion of a viscous fluid. This friction is usually schematized in
various semiempirical formulae. In t-liis work the different scliematizations
of the friction were not studied separately but it was shown that a solution
exists for the fluid motion. The results give information on the damping of
the fluid motion in the case of the seiches.
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DOI: https://doi.org/10.4401/ag-4894
Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X