Abstract
After reviewing the equations used for the study of the
seiches of lakes, in this work the types of oscillation of four artificial lakes
situated in the Aosta Valley (Place Moulin, Beauregard), in the Cuneo
area (Piastra) and in the Adda river (Alpe Gera), reservoir have been
studied.
The periods valued with Hidaka's method have been compared with
those obtained from lakes of very simple geometrical form.
Finally the numerical integration of Chrvstal's equation has been
calculated and the amplitudes corresponding to the various nodes were traced
by a plotter, directly linked to the calculator.
seiches of lakes, in this work the types of oscillation of four artificial lakes
situated in the Aosta Valley (Place Moulin, Beauregard), in the Cuneo
area (Piastra) and in the Adda river (Alpe Gera), reservoir have been
studied.
The periods valued with Hidaka's method have been compared with
those obtained from lakes of very simple geometrical form.
Finally the numerical integration of Chrvstal's equation has been
calculated and the amplitudes corresponding to the various nodes were traced
by a plotter, directly linked to the calculator.
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DOI: https://doi.org/10.4401/ag-5111
Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X