Re: water pressure
- From: Maarten van Reeuwijk <maarten@xxxxxxxxxxxxxxxxxxxxxxxxxxxx>
- Date: Tue, 27 Dec 2005 17:15:48 +0100
Maarten van Reeuwijk wrote:
> 360 km / h. To simulate a tsunami I would recommend having a thin layer of
> fluid which you bring into motion by moving a board back and forth in the
> water at one end.
Another option is to really simulate the shock that induces the tsunami, for
example by somehow raising the floor of your aquarium. See below for
inspiration (from http://wcatwc.arh.noaa.gov/physics.htm)
Earthquakes generate tsunamis when the sea floor abruptly deforms and
displaces the overlying water from its equilibrium position. Waves are
formed as the displaced water mass, which acts under the influence of
gravity, attempts to regain its equilibrium. The main factor which
determines the initial size of a tsunami is the amount of vertical sea
floor deformation. This is controlled by the earthquake's magnitude, depth,
fault characteristics and coincident slumping of sediments or secondary
faulting. Other features which influence the size of a tsunami along the
coast are the shoreline and bathymetric configuration, the velocity of the
sea floor deformation, the water depth near the earthquake source, and the
efficiency which energy is transferred from the earth's crust to the water
column.
HTH, Maarten
--
===================================================================
Maarten van Reeuwijk dept. of Multiscale Physics
Phd student Faculty of Applied Sciences
maarten.ws.tn.tudelft.nl Delft University of Technology
.
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