i admit to being pretty ignorant about thermochemistry
is there a relevant difference between crystals approaching equilibrium with a melt and crystals approaching equilibrium with a solution? because i had the impression that the mechanisms were the same and the line between these processes was actually a little bit fuzzy, what with things like hydrate crystals and aquo complexes
(i think you can't melt dolomite tho, at least near atmospheric pressure)
is there a relevant difference between crystals approaching equilibrium with a melt and crystals approaching equilibrium with a solution? because i had the impression that the mechanisms were the same and the line between these processes was actually a little bit fuzzy, what with things like hydrate crystals and aquo complexes
(i think you can't melt dolomite tho, at least near atmospheric pressure)