1997
DOI: 10.1007/s003480050069
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Experimental investigation of the interaction between weak shock waves and granular layers

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Cited by 64 publications
(21 citation statements)
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“…The one-dimensional, unsteady version of these equations was solved numerically. A comparison between the predictions of the numerical simulations and the experimental results presented by Ben-Dor et al (1997) showed good agreement.…”
Section: Introductionsupporting
confidence: 65%
“…The one-dimensional, unsteady version of these equations was solved numerically. A comparison between the predictions of the numerical simulations and the experimental results presented by Ben-Dor et al (1997) showed good agreement.…”
Section: Introductionsupporting
confidence: 65%
“…Formation of unsteady fields of the gas pressure in granular media and the effect of gas filtration on the evolution of pressure waves in porous granular media were considered in detail in [16][17][18]. A numerical description of the wave processes observed in [16,17] was proposed in [18], based on the assumption that the "skeleton" of the granular medium is not deformed. It was shown [18] that the assumption of the rigid behavior of the "skeleton" of the granular medium does not allow a comprehensive description of all features of the wave processes, in particular, the effect of amplification of the dynamic load on a screened wall.…”
Section: Introductionmentioning
confidence: 99%
“…Using the method developed in [12,13], Ben Dor et al [16][17][18] continued the experimental study of the laws of interaction of weak air shock waves with a layer of a granular medium that covers a solid wall. In contrast to [12,13], the total stress of the mixture and the pressure of the pore gas were measured in [16][17][18] not only at the end of the shock tube but also in several cross sections of the granular medium layer.…”
Section: Introductionmentioning
confidence: 99%
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“…A gently perturbed 1D chain of spherical grains is known to admit a new kind of solitary wave propagation [7,8]. The propagation of mechanical energy at shallow depths in dry granular beds depend on the force chains that span the granular fabric [9] and remains an area of broad interest in many contexts such as landmine detection [10], shock absorption [11], and thermal conductivity especially in the context of geothermal applications [12] and geophysics at ultrashallow depths [13].…”
Section: Introductionmentioning
confidence: 99%