jumbogala said:
Part of the reason I was confused was that I thought the pressure at the top of the water would be the atmospheric pressure. So if you have a glass of water, the pressure at the bottom of the glass should be more than atmospheric pressure... shouldn't it?
I suppose the pressure at the top of the straw should be 0 though.
Anyway, mass of the water is ?DA, and its weight is ?DAg.
P = F/A, so pressure at base of straw is P = ?DAg / A = ?Dg! Cool :)
I'm still confused why the pressure at the bottom of the glass is atmospheric pressure though.
Hello
Jumbogala,
As Borek points out below, it is a theoretical limit. It assumes the "suction" device is so strong that it can create a complete vacuum at the top of the water (even continually sucking out any residual vapor pressure, before it has a chance to reach equilibrium). Once there is a complete vacuum at the top portion of the straw, there is no way to draw the water column any higher without increasing the pressure at the bottom of the column (such as increasing the atmospheric pressure, for example). So yes, to find how high the column of water can
possibly rise, one must assume zero pressure at the top.
Borek said:
Actually 10.3m is not true - mouth muscles are not strong enough to suck that strong. So while this is kind of a theoretical limit of how far up water can be suck at the atmospheric pressure, it has nothing to do with the reality.
Hello
Borek,
Yes, it is a theoretical limit. With that I agree.

But that doesn't, and shouldn't, keep physics students from discussing theoretical
possibilities in the physics, restricting the discussion to the applicable physics, even if it might violate practical physiology. Examples such as Einstein's full size locomotive trains moving near the speed of light come to mind -- nothing to do with reality but still very useful as an analogy. Still, Einstein's analogies do have direct real-world applications for fast moving electrons and GPS/GLONASS satellites. Similarly, this drinking straw exercise has real-world applications for modeling barometers.
It is not the pressure at the bottom of the glass that counts, rather that at the water surface (outside the straw).
I agree completely. The bottom of the water column in question is at the same height as the
surface of the water in the glass. This is the vertical point were the water in the column equals atmospheric pressure -- so we define this point as the bottom of the column. And this is true even if part of the straw sinks further down to say, the bottom of the non-empty glass.
