During downward freezing, dense brine collected into central columns, which gradually sank as they accumulated salt from adjacent regions. In upward freezing, brine instead migrated toward the ...
In the third stage, diffusion becomes the dominant mechanism. Brine pockets migrate slowly toward the warm end, and a cleaner ice layer gradually develops near the cold boundary. Tracking brine ...
Some results have been hidden because they may be inaccessible to you
Show inaccessible results
Feedback