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The need to model high-speed flows of compressible media with shock waves in the presence of dense curtains or layers of particles arises when studying various processes, such as the dispersion of particles from a layer behind a shock wave or propagation of combustion waves in heterogeneous explosives. These directions have been successfully developed over the past few decades, but the corresponding mathematical models and computational algorithms continue to be actively improved. The mechanisms of wave processes in two-phase media differ in different models, so it is important to continue researching and improving these models.

The paper is devoted to the numerical study of the propagation of disturbances inside a sand bed under the action of successive impacts of a normally incident air shock wave. The setting of the problem follows the experiments of A. T.Akhmetov with co-authors. The aim of this study is to investigate the possible reasons for signal amplification on the pressure sensor within the bed, as observed under some conditions in experiments. The mathematical model is based on a one-dimensional system of Baer –Nunziato equations for describing dense flows of two-phase media taking into account intergranular stresses in the particle phase. The computational algorithm is based on the Godunov method for the Baer – Nunziato equations.

The paper describes the dynamics of waves inside and outside a particle bed after applying first and second pressure pulses to it. The main components of the flow within the bed are filtration waves in the gas phase and compaction waves in the solid phase. The compaction wave, generated by the first pulse and reflected from the walls of the shock tube, interacts with the filtration wave caused by the second pulse. As a result, the signal measured by the pressure sensor inside the bed has a sharp peak, explaining the new effect observed in experiments.

The study of elastic waves in porous media is relevant for mineral exploration, the use of porous screens for shock wave damping, and the study of the structure of the earth’s crust. The elastic properties of a porous medium, which can be judged by the propagation velocity of various types of waves, depend on the degree of consolidation of the porous medium. For example, bulk media (sand, glass beads, granular materials) have a low sound velocity (about 100 m/s); compaction of such media is accompanied by a slight increase in velocity, while their consolidation (sandstone, gas hydrate cementation) leads to a multiple increase in the acoustic wave velocity, on the order of 2000–3000 m/s. This paper theoretically investigates the dynamics of a wave pulse in a shock tube containing a layer of a bulk medium. Numerical modeling was performed under experimental conditions. A description of a shock tube experimental setup is provided. The setup consists of a high-pressure volume (HPV), a low-pressure volume (LPV), and a bulk medium section. A shock wave pulse (SWP) is generated by the rupture of a diaphragm between the HPV and LPV. The SWP dynamics are recorded by piezoelectric sensors located flush on the inside of the tube. In the shock tube, equipped with a bulk medium section, the wave experiences multiple reflections from the surface of the porous medium under study and the upper end of the tube. The reflected signals are used as probe pulses to study changes in the porous medium caused by repeated passages of the shock wave pulse, with a period of approximately 10 ms. A mathematical model is used that includes the equations of conservation of mass, momentum, and energy for the gas phase and solid particles with closure relations. The process is described for one-dimensional planar motion of the gas and dispersed phases. The numerical solution utilizes an approximation of the equations based on the control volume method. Numerical results have shown that the proposed model accurately describes, qualitatively and quantitatively, the occurrence of a sharp, short-term increase in the total voltage (peak) during repeated pulse passage through a layer of bulk material, as observed in experiments.