cmb
- 1,128
- 128
xxChrisxx said:If water is in thin film it is being used as hydrostatic bearing (which isn't the same as floating), meaning it's simply transferring the load through to an external container due to it being incompressible and the pressure increasing.
You don't appear to be acknowledging the caveats everyone has made. We have excluded 'films' in this, for precisely the reason you are repeating.
But you can have a column of water just a few mm diameter and the pressure in that water at 14m depth is the same as that at 14m depth in the ocean - it is at one atmosphere pressure (gauge).
Think about the cuboid boat, as in diagram above. The vertical sides do nothing for 'lift'. The upper side is exposed to 1 atm pressure, the lower is at 2 atm pressure (assume it is 14m down). Let's say it has a 14 million lb displacement, so at a differential pressure above and below of 1 atm it will need a hull surface area of 14 million lb/14psi = 1 million square inches.
If it has, let's say, only 500,000 sq in, then it will not be buoyant until it settles down to 28m depth. (If it is less than 28m high to the gunnels, then it'll sink!)
This is all self-balancing and all in order; a floating object will become 'buoyant' when its average density below the water line is at a sufficient differential less than the water that it can lift the rest of the object above the water line. If it's density is too high to achieve that balance at any depth, then it will sink. If the density is too low to achieve the balance at any depth, it will float out of the water and keep going up!