WU Yong, HE Si-ming, PEI Xiang-jun, et al. Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall[J]. 2012, 33(10).
WU Yong, HE Si-ming, PEI Xiang-jun, et al. Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall[J]. 2012, 33(10).DOI:
Because large quantities of loose deposits were accumulated in gully after “5•12” Earthquake
the occurrence probability of gully debris flow is enhanced greatly in rainfall. However
due to the special conditions of provenance and disaster environment
the traditional theory cannot be used to expound the mechanism of gully debris flow and prevent the disaster effectively as ever after the event. Here
based on hydrology
the hydrological model of ground water table in loose deposits is established first. Then by aid of hydraulic theory
the change of hydraulic characteristics and the variation of hydraulic power with the rising of groundwater level are analyzed. Furthermore
the calculation formulas of hydrodynamic and hydrostatic pressure are also proposed. Finally
by applying infinite slope theory in calculation of sliding force
anti-sliding force and residual sliding force acting on each segment
the failure mechanism of accumulation body is illustrated clearly with an example. The result indicates the failure of loose deposits in rainfall is the result of increase of the hydraulic power with the rising of groundwater level. Those deposits which have small coefficient
gentle slope
narrow-deep gully and large basin would be easy to fail because of its high hydraulic pressure generating in rainstorm
and the failure modes can be divided into two types according to residual sliding force as pushing failure and hauling failure.