Dr. Heiner Friedrich explains: «Because the process happens so rapidly, and at such a small
length scale we needed to cryogenically arrest the sample at various stages of the process.
Not exact matches
«But this size effect disappears when you get to a large enough
length scale on tectonic plates, so we
need to consider other things like when temperature and water begin to play a role.»
IMO, the only way to make it better, is to «
scale» the
length needed «earn payment.»
On larger
length scales, transport in liquids and gases is normally due to another transport phenomenon, convection, and to study diffusion on the larger
scale, special efforts are
needed.
The diagram
needs temperatures,
length scales, heat flows and a few equations.