Integral form of a hydraulic equation of a stratified-density flow, when the lower flow is the collapsed rock mass intruding into the water reservoir under the action of seismic forces.
2015
In the published fundamental works about hydrodynamic theory of mud streams, avalanches and landslides, the calculation of their characteristics, seismic forces have not been taken into consideration. That is why we additionally introduce the seismic force into the dynamic equation since the crumbling slope is potentially dangerous, because it may be set in motion under the action of a seismic shock of certain intensity and direction. Fig. 1, Ref. 5.
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