The main goal of this paper is to clarify the effects of rockfall volume on
its fluidization. For this purpose, outdoor rockfall experiments were carr
ied out to analyze runout distances and individual movements of rockfall bl
ocks and numerical simulations were conducted for these experiments to lear
n more about the mechanism of rockfall fluidization. The rockfall experimen
ts were conducted using an artificial slope on which granite slabs were sur
faced and overlaid with cubiformed granite blocks. The size and number of b
locks were varied in this series of experiments. Further, numerical simulat
ions were carried out in which the coordinates of individual rockfall block
s were traced in three-dimensional space from rockfall initiation to final
deposition. It became clear from the experiments and simulations that the r
unout distance had a positive correlation with the rockfall volume (number
of rockfall blocks) and the runout distance of the gravity center of deposi
ted rockfall mass had a negative correlation with the rockfall volume. To c
larify the mechanism of these two phenomena, the positions of individual bl
ocks from initial arrangements to final depositions were traced in the expe
rimental and numerical simulations. This revealed that the relative positio
ns of each block along the slope direction were not changed during rockfall
movement. The reason for the block-sequence preservation was that front fa
cing blocks in the initial cube arrangement accelerated and rear facing blo
cks decelerated along the slope by internal collision between blocks. Furth
er, as the rockfall volume increased, the opportunities for impact among th
e rockfall blocks increased with the front facing blocks pushed farther. Wh
ereas the gravity-center of the deposited rockfall mass had an inclination
to travel shorter distances as rockfall blocks increased according to the i
ncrease of kinetic energy dispersed by the collision of blocks. (C) 2000 El
sevier Science B.V. All rights reserved.