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.................. In my Materials class the other day, we
were discussing polymers, and the discussion turned to glass transition
temperatures, and, as interesting discussions are wont to do, it further
turned to the structure of glass - silicate glass (I know it is not a
polymer in most views, but this is a good class!!). Anyway, the professor
(who shall remain nameless) said that glass was above its glass transition
temperature at room temperature, and therefore could be expected to flow,
albeit slowly. He suggested that this was in fact the case, as very old
glass was thicker at the bottom than at the top. Most of you are familiar
with this argument. I brought up that this has been suggested as an
artifact of production methods, but I do not happen to remember where I
read this. I believe it was in a broad JCE article. Could someone who has
that handy little electronic index check this out for me? Meanwhile, if
anyone has references, either for the flow, or against it, please give them
to me, as i would like to be able to possibly continue this discussion on
the resumption of class, or perhaps to present this to the class (part of
our grade is based on two presentations - actually, almost all of it).
Thanks for all the help.
The most amazing thing about rock-hounding and | Lloyd Carroll
mineral collecting is that you could - even right | lcarroll@unity.ncsu.edu
now!! - be standing, sitting or walking over the | NC State University
most beautiful thing you have ever seen - or, | Raleigh, NC
more correctly, that no one has ever seen. |
We viewed the MU film on Resonance yesterday. An issue was made of the
viscosity of glass. Two of my students said they had read that the
variation in glass thickness in very old buildings was not a sign of glass
flowing, but rather a manufacturing event.
Can anyone give me information on this?
Thanks,
Ken Fox
AP/IB Physics Teacher
Smoky Hill High School