7 Comments

"Since the internal diagonal of a unit cube has length √(3), that meant y was equal to √(3)−(1/75)1/6, or about 1.245. Finally, this “optimal” ratio x/y was roughly 0.3911. Right?"

"Wrong!"

This suggests solving for the density of the iceberg at which the wrong answer would become the right answer. Therefore,

(1-ρ) = x³√3/2 ≈ 0.866025x³ ===> x = [2(1-ρ)/√3]^⅓ and y = √3 - x for the vertex-high case so the center of mass is a distance (y-x)/2 = (√3 - 2x)/2 = ½√3 - [2(1-ρ)/√3]^⅓ below the surface.

For the floating-horizontal case, x = (1-ρ) and y = ρ, so (y-x)/2 = (2ρ-1)/2 = ρ - ½

So, to solve for the critical value of ρ, I set these two CM depths equal to obtain

½√3 - [2(1-ρ)/√3]^⅓ = ρ - ½

The solution of interest is ρ = 0.9264336, at which cubes in either orientation would have their centers of mass a distance of 0.4264336 below the surface and therefore be equally likely to float in either orientation. Not a huge difference from 0.90.

https://i.servimg.com/u/f89/19/74/46/40/densit10.jpg

Another question of interest is whether a cube with the equilibrium density calculated above would be bistable in one or the other of the two orientations considered, or would it prefer yet another orientation.

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Is the answer to the main Fiddler as obvious as I think it is?

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Man I wish I'd submitted my pyramid figure made in Geogebra.

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I guess up to isomorphism Round = Red.

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