[Geysers] Constrictions, bubbles, and pressure
Ron Keam
r.keam at auckland.ac.nz
Tue Mar 21 18:01:25 PST 2006
Jeff's experiment is interesting. Here are some
comments which I hope will throw light on his
observations. They do not provide a complete
answer, but I have indicated the source of the
physical effects that are ignored in the simple
approximation described below.
With the unrestricted tube one presumably has a
uniform horizontal cross-section. The bubble
will contain a fixed amount of air. Because the
depths at which the bubble movements are being
considered will be over a fairly restricted
range, one can assume that its volume changes are
negligible. Therefore its vertical extension
will be approximately constant. Let that
constant extension be ß. If the bubble is on side
A of the U-tube, and the other side is B then the
level of water surface near the top of A will be
precisely ß higher than the level of the water
surface near the top of B. (Just use equality of
rho. g.h on both sides down to the bottom of the
U-tube.) When the bubble is passing through the
constriction its average cross-section is
reduced. Therefore, to keep its volume constant
its vertical extension must become greater than
ß. Thus the difference in level between the free
water surfaces in A and B must also increase.
This does not say whether the surface on side A
rises or the surface on side B falls. Evidently
from Jeff's observation it is the latter that is
seen. Once the bubble has passed through the
constriction the bubble resumes its vertical
extension ß and so also does the difference in
the level in A and the level in B.
NOTE: I have used an argument based on assuming
at each stage that static pressure gradients
apply. That ignores dynamic effects, and it is
they that will determine the actual observed
result - i.e. that it is that side B water level
decreases rather than side A rises (or that it is
some of both).
Ron Keam
>Here is an interesting experiment. I believe it shows that when a bubble
>rises through a constriction in
>a geyser system, the pressure drops briefly. If the pressure drops, the
>boiling rate should increase, and
>this might trigger an eruption.
>
>1) Obtain 4 feet of tygon tubing, surgical tubing, or similar material.
>2) Fill it with water.
>3) Get a bubble situated in the middle of the tubing section.
>4) Now hold both ends open, vertical, and next to each other. The bubble will
>rise up one side of the U
>tube.
>5) The water level in the side containing the bubble will be highest.
>6) Pinch the tubing above the bubble so that the bubble must flow through the
>constriction on its way
>to the surface.
>7) Note that the water levels change while the bubble is flowing through the
>constriction. The low side
>gets lower, but it rebounds once the bubble has passed through.
>
>I suspect this last observation means that the pressure dropped while the
>bubble moved through the
>constriction. Why this happens isn't clear to me.
>
>I welcome explanations.
>
>I must get back to doing something productive.
>
>Have fun.
>
>Jeff Cross
>jacross at lamar.colostate.edu
>
>
>_______________________________________________
>Geysers mailing list
>Geysers at wwc.edu
>https://mailman.wwc.edu/mailman/listinfo/geysers
--
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Ron Keam
The Physics Department
The University of Auckland
Private Bag 92-019
Auckland
New Zealand
Phone +64 9 373-7599 extension 87931
FAX +64 9 373-7445
EMail r.keam at auckland.ac.nz
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