2017
DOI: 10.1016/j.icarus.2017.01.007
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Scaling of impact-generated cavity-size for highly porous targets and its application to cometary surfaces

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Cited by 11 publications
(16 citation statements)
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“…The line corresponds to an empirical relationship shown by Eq. 14 obtained for the highly porous targets of foamed polystyrene, sintered glass bead, gypsum, and pumice (Okamoto and Nakamura, 2017). The data for gypsum and pumice used in the fitting of the empirical relationship are also shown in light blue (U > 4 km s -1 ) and dark blue (U < 4 km s -1 ).…”
Section: Acknowledgmentsmentioning
confidence: 97%
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“…The line corresponds to an empirical relationship shown by Eq. 14 obtained for the highly porous targets of foamed polystyrene, sintered glass bead, gypsum, and pumice (Okamoto and Nakamura, 2017). The data for gypsum and pumice used in the fitting of the empirical relationship are also shown in light blue (U > 4 km s -1 ) and dark blue (U < 4 km s -1 ).…”
Section: Acknowledgmentsmentioning
confidence: 97%
“…Laboratory high-velocity impact experiments, using millimeter-to-centimeter size projectiles to study cratering in the strength regime, were performed for various targets with porosities ranging from 0% to more than 90%. The morphology and dimensions, i.e., diameter and depth, were studied for weak cemented basalt targets (Housen, 1992), sandperlite-fly ash mixture targets (Housen and Holsapple, 2003), sintered glass bead targets (Love et al, 1993;Michikami et al, 2007;Hiraoka et al, 2008;Okamoto et al, 2015; Okamoto and Nakamura 2017), cement mortar targets (Michikami et al, 2017), gypsum targets Okamoto and Nakamura, 2017), and natural porous rocks (Baldwin, et al, 2007;Kenkmann, et al, 2011;Suzuki et al, 2012;Poelchau, M. H., 2014;Flynn, et al, 2015;Okamoto and Nakamura, 2017). Table 1 summarizes the target density, porosity, strength, impact velocity, and projectile material and diameter of these experiments.…”
Section: Targets In the Strength Regimementioning
confidence: 99%
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