Abstract
Confined or channelized debris flow is one of the most powerful processes for transporting solid materials along the mountain torrent. It is defined as a type of mass movement that involves water-charged, predominantly coarse materials flowing rapidly down along a steep confined, pre-existed channel. Development of debris flow is broadly characterized by initiation, transportation, and deposition, depending on channel gradient, and size and gradation of solid mixture. In order to design debris flow control structure, exact measurement of velocity and corresponding impact force are required. Therefore, debris flow flume has been designed in this study to experimentally examine the flow characteristics of debris flow. A 200 mm (W) × 300 mm (H) × 2000 mm (L) flume has been used to conduct the experiments with a flume slope of 25°, 30°, 35°, 40°. Velocity of debris flow was estimated by image analysis of photographs, and runout length and width were measured using grids on deposition pan. Two types of debris mixture have defined, based on the portion of clay, sand, and gravel materials. Experiments showed that velocities of debris flow strongly related to flume slope, ranging 1.5–2.5 m/s. Runout length and width were affected by the flume slope and debris flow composition.
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Acknowledgements
This research was supported by the project on “The experimental analysis of debris flow impact force (II),” which was funded by National institute of Forest Science.
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Im, S., Eu, S., Kim, D. (2017). Understanding Debris Flow Characteristics Using Flume Experiments. In: Mikos, M., Tiwari, B., Yin, Y., Sassa, K. (eds) Advancing Culture of Living with Landslides. WLF 2017. Springer, Cham. https://doi.org/10.1007/978-3-319-53498-5_41
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DOI: https://doi.org/10.1007/978-3-319-53498-5_41
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