However, compared with its fresh counterpart, the frozen
crumb exhibited a significantly smaller area under the ice-melting
transitions. It is indicative of a lowercfw(content of freezable water)
in the frozen samples. This difference can be seen more quantitatively inFig. 2(Inset) where the deducedcfw is plotted. So, due to
the loss of the crumb water that migrates toward the crust (see