2022
DOI: 10.1016/j.icarus.2022.115139
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Propagation and attenuation of pulses driven by low velocity normal impacts in granular media

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Cited by 13 publications
(5 citation statements)
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“…This means that when measuring the velocity of transmission of the peak in kinetic energy or pressure produced by the pulse, the results should not vary by much, even if, as can be observed, the peak in pressure tends to precede the arrival of the peak in kinetic energy. Figures 7(a) and (c) show that as time passes, there is a decay of the pulse amplitude and a broadening of the pulse, similar to what has been observed at higher confining pressures (Langlois & Jia 2015;Quillen et al 2022). Pulse broadening arises due to variations and irregularities in the force contact network, such as variations in travel times along different force contact chains (Owens & Daniels 2011) and irregularities in the force contact network Figure 8 shows the velocity of transmission of the peak of the energy of the impact through the granular medium versus the confining pressure applied to the system.…”
Section: Transmission Of a Pulsesupporting
confidence: 70%
“…This means that when measuring the velocity of transmission of the peak in kinetic energy or pressure produced by the pulse, the results should not vary by much, even if, as can be observed, the peak in pressure tends to precede the arrival of the peak in kinetic energy. Figures 7(a) and (c) show that as time passes, there is a decay of the pulse amplitude and a broadening of the pulse, similar to what has been observed at higher confining pressures (Langlois & Jia 2015;Quillen et al 2022). Pulse broadening arises due to variations and irregularities in the force contact network, such as variations in travel times along different force contact chains (Owens & Daniels 2011) and irregularities in the force contact network Figure 8 shows the velocity of transmission of the peak of the energy of the impact through the granular medium versus the confining pressure applied to the system.…”
Section: Transmission Of a Pulsesupporting
confidence: 70%
“…Max Slope, ρ S = 2.2 g cm −3 , β = 1.0 (e ≈ 0.008) instrument, will measure the dynamical slopes as one of its science objectives (Michel et al 2018;Karatekin & Le Bras 2021;Ritter et al 2021). The seismic pulse delivered by the DART impact may significantly alter surface features on Dimorphos (Quillen et al 2022b;Thomas & Robinson 2005). We also note that the global shape of Dimorphos may also be immediately altered by the DART impact itself .…”
Section: Discussionmentioning
confidence: 81%
“…When Hera arrives, its optical instruments and CubeSats, especially the Juventas CubeSat and its onboard GRAvimeter for small Solar System bodies (GRASS) instrument, will measure the dynamical slopes as one of its science objectives (Michel et al 2018;Karatekin et al 2021;Ritter et al 2021). The seismic pulse delivered by the DART impact may significantly alter surface features on Dimorphos (Quillen et al 2022b;Thomas & Robinson 2005). We also note that the global shape of Dimorphos may also be immediately altered by the DART impact itself .…”
Section: Discussionmentioning
confidence: 81%