Submitted by OneTreePhil t3_yx9z3q in askscience
I was thinking about the giant free "ponds" in Larry Niven's Integral Trees. On a planet, pressure as a function of depth is fairly straightforward. But if the water is held together only by cohesive forces, how does it change with "depth"? In the book they were free floating and various sized
Water is less dense as a solid so pressure causes it to melt, so I'm not thinking there could be a solid core by pressure. I'm wondering, if there was a drop of water 14 miles across (so the center is as far from the surface s the Challenger Deep), what would the pressure be at the center? Could we scuba all the way through?
Maybe it would help to imagine a spherical "drop" of water of radius (depth) x, in free fall, with enough of a "balloon" around it to prevent heat loss and evaporation but not add and "squeeze pressure." How would pressure change through the pond? How big would it have to be to noticeably influence itself by gravitational effects?
cowox93112 t1_iwp22tg wrote
Free fall is equivalent to being in a region of space without gravity. Let's also assume a vacuum around it such that we can neglect external air pressure etc.
There is one force left, namely cohesion. It will attempt to minimize the droplet surface, morphing the it into a spherical shape. The pressure at the center is given by P= 4 gamma/R with R being the droplet radius. It is tiny for any sizeable droplet. It also gets smaller for larger droplets. until the droplet becomes massive enough to generate its own sizeable gravity.