The invention belongs to the technical field of
landslide prediction, and relates to a shallow earthquake-stress joint inversion tunnel portal
landslide prediction method, which comprises the following steps of: obtaining slope body first-arrival wave
travel time data through a high-frequency seismic source array, constructing a geologic model containing a rock
mass integrity
coefficient matrix, identifying rock
mass structure deterioration through
elastic wave velocity distribution, and predicting the
landslide at a tunnel portal through shallow earthquake-stress joint inversion. The method comprises the following steps: locking a potential unstable structure weak area in advance, then embedding a rock
mass integrity
coefficient matrix as priori knowledge into a
stress field for solving, and by establishing a
coupling relationship between
seismic wave propagation and stress, inverting slope
stress field distribution, capturing an early
stress redistribution signal caused by structural degradation of a deep rock mass, and finally obtaining an initial
stress redistribution signal of the deep rock mass. Early
perception of
mechanical instability precursor is realized; and then calculating
strain energy density distribution of the potential slip surface based on the stress and strain data, and accurately judging the potential slip surface before the slip surface is not completely
cut through by judging whether the
strain energy density exceeds a threshold value, whether a continuous sheet is formed and whether the
expansion rate exceeds the standard, thereby avoiding lagging caused by dependence on a displacement
signal.