Calculating Wave Amplitude & Wavelength in Water Pools

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The discussion focuses on modeling the wave amplitude and wavelength generated by a mass falling into a pool of water or a continuous fountain stream. It emphasizes that the resultant wave characteristics depend on the energy of the impacting object, its properties, and the water's characteristics like viscosity and surface tension. The analogy to a capacitor discharging into a transmission line is made, suggesting that energy from the mass converts into waves that spread out, decreasing in amplitude with distance. The waves produced are identified as gravity waves, and the impact of a continuous water stream is noted to stabilize the system, ceasing further wave radiation. Overall, the complexity of water wave behavior is highlighted, indicating the need for further research in this area.
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How would we model/calculate the circular waves in a pool of water (wavelength and amplitude) from a mass falling into it from a given height, and from a fountain of water falling into it continuously?
How would we model/calculate the circular waves in a pool of water (wavelength and amplitude) from a mass falling into it from a given height, and from a fountain of water falling into it continuously?

Is there is a way to describe the initial configuration of the wave based on the stimulus. For example, what is the resultant wave amplitude and wavelength from a X kilogram solid sphere at a velocity of Y meters persecond hitting a Z square centimeter area of water, versus the stimulus being a single sphere of water contacting the same area of surface at a similar speed, versus a continuous stream of water as in a fountain hitting the water.

I'm guessing that the resultant wave is dependent on the energy of the object that hits the water surface, modified by some characteristic of the incident object and also of the ppol of liquid(water) that it falls into, such as its shape, viscosity, surface tension, perhaps even refractive index.
 
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Maybe we can find a part analogy with the case of discharging a capacitor into a transmission line. Here the energy of the capacitor is transferred into a wave which travels away from it. I think that the capacitor discharges into the characteristic resistance (impedance) of the line, and the product CR will determine the time for the discharge to happen and the duration of the first half wave. So for a mass falling into water, maybe the energy is converted into a wave, and travels away from the centre. The energy is now spreading out over a plane 2D surface, so the energy density will decrease in proportion to distance, and the amplitude will decrease with the square root of distance.
As Lord Kelvin mentioned, water waves are not straightforward things to study.
 
Welcome to PF.

The ripples that spread out across the surface are gravity waves.
https://en.wikipedia.org/wiki/Gravity_wave

Where a continuous stream of water penetrates a water surface, the surface is dragged down by the viscosity shear in the boundary layer of the water. Once the system is stable, no more gravity waves will be radiated.
 
His areas of research are perhaps a little different, but I'll page @Dr. Courtney to see if he has worked with gravity waves in his impulse research...
 
My idea is that I want to use immerse Whitetail Antlers in a fishtank to measure their volumetric displacement (the Boone and Crockett system is the current record measurement standard to place in a juxtaposition with) I would use some sight glass plumbed into the side of the tank to get the change in height so that I can multiply by the tank cross-section. Simple Idea. But... Is there a simple mechanical way to amplify the height in the sight glass to increase measurement precision...

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