“…This tendency to make clusters is considered to govern flow characteristics of ice/water slurry such as the ice distribution ratio at a branching pipe. Fig ure 7 shows the ice fraction ratio of the upward branching pipe from the horizontal main pipe, C2/C1 for beads, chip ice and granulated snow (Kawada et al, 1997). The fraction in the branch pipe is smaller for par ticles with larger Vcr value.…”