2018 Volume 24 Pages 487-492
This paper describes the characteristics of the debris flow with woody debris which occurred in the Shirakidani River in Asakura City, Japan on July 5th, 2017. Field survey and numerical simulation were made in this research. The field survey shows the amount of sediment and woody debris outflowing from the mountain area and the results are compared with the numerical simulation. One-dimensional simulation model is developed for the debris flow with woody debris. This model considers two-layer flow; the lower layer expresses sediment-water mixture and the upper layer shows wood-sediment-water mixture. The numerical simulation indicates the peak flow discharge Q=70m3/s and peak sediment concentration C= 0.2 along the river valley. The sediment runoff volume is estimated about 160,000m3 and this result agrees with field survey.