- #1
Rooner1
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- TL;DR Summary
- The units of the Diffusion Coefficient (cm2/sec) don't look like a mass transfer units.
I want to compare diffusion of a tracer gas with a low exposure limit (e.g. isoflurane) to the advection of air by a ventilation system. When will diffusion exceed advection? I can't make sense of diffusion constant to compare transfer rates or velocities.
At room temperature the diffusion coeeficient is generally around 0.2 cm2/sec for many gases. So what does that mean for the dispersal of a tracer gas (like ether vapors or isoflurane) in a calm indoor environment? What are the full units that are cancelling out? I'd love some citations if you have them.
There was a similar post about diffusion coefficient in 2010, and the reply finished with, "I can't get much more intuitive than that", which seems to be circular thinking when his explanation was rather obtuse. He said it was a velocity x density, which would be cm/s x gm/cm3, which would cancel out to be gm/sec.cm2.
I'm a moderately decent chemist, with units anyways, and the explanations of diffusion of gases at tracer levels in air is generally highly simplistic, like the sensing of vailla as it diffuses through a room, or highly theoretical and involving Boltzman constants, degrees Kelvin, etc. Can this be simplified and still approximate decent rigor?
At room temperature the diffusion coeeficient is generally around 0.2 cm2/sec for many gases. So what does that mean for the dispersal of a tracer gas (like ether vapors or isoflurane) in a calm indoor environment? What are the full units that are cancelling out? I'd love some citations if you have them.
There was a similar post about diffusion coefficient in 2010, and the reply finished with, "I can't get much more intuitive than that", which seems to be circular thinking when his explanation was rather obtuse. He said it was a velocity x density, which would be cm/s x gm/cm3, which would cancel out to be gm/sec.cm2.
I'm a moderately decent chemist, with units anyways, and the explanations of diffusion of gases at tracer levels in air is generally highly simplistic, like the sensing of vailla as it diffuses through a room, or highly theoretical and involving Boltzman constants, degrees Kelvin, etc. Can this be simplified and still approximate decent rigor?