摘要(英) |
Debris flow
originate when poorly sorted debris (rock, soil, woody debris, etc.) is
mobilized from hill slope and channels by adding sufficient moisture.
During heavy rainfalls, particular those brought by typhoons, the
colluvium is easily weakened, which often leads to a debris flow. The
debris flows presents a great threat to the down stream villages. In
this experimental study, it focus on characteristics of debris-flow
depositions using various block structures, the concrete slit dams,
steel grid dams, and gravity dams under a specified gradient, gravel
volume consistency and debris unit weight. It can be simulated in the
Lab to analyze the deposition characteristics of debris flow including
detention rate , grain separation effect and coarse grain separation
efficiency in various conditions. The test results can be considered for
the debris-flow hazards mitigation. The water flume experiments in
laboratory shows that: In debris flow simulation, when water flume
gradient is larger, there are more coarse grain concentration and higher
gravel volume consistency in the front part of debris flow. The coarse
grain concentration of the front debris flow could reach to 86.5% in 22
degrees. In debris flow retaining, the detention rate will be less by
increasing the water flume gradient and reducing the gravel volume
consistency. The detention rate of steel grid dams can reach 70%, and
the detention rate of gravity dams can reach 60%. But the most
influences of the concrete slit dams was gravel volume consistency, when
water flume gradient is 22 degrees and gravel volume consistency is 0.5,
the detention rate is only 36%. The concrete slit dams and steel grid
dams both can reach separation effect, but the gravity dams will silt
and lose the function of reducing debris volume. |