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I don't understand the teakettle method. What's the observable?
What's the connection to kinetic theory? Steam comes jetting
out of the teakettle ... don't "ballistic" advection effects
completely overwhelm any diffusion effects?
I don't understand the baggie-weighing method. How is the
observable connected to the size of atoms? What role does
condensation of atmospheric humidity play in the method?
(Is that the point, or is that a nuisance-effect?)
Dan MacIsaac, Associate Professor of Physics, SUNY-Buffalo State College