2017
DOI: 10.1016/j.proeng.2017.09.754
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Comparison of Crater Behavior of Water Ice by Low and High Density Projectiles under Hypervelocity Impact

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Cited by 2 publications
(2 citation statements)
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“…As shown in Figure 7, when the impact velocity is 100 m/s and 300 m/s, the axial velocity at the impact point of the projectile varies in pulsation because the bullet attached to the impact point of the projectile produces elastic deformation after the end of the impact process [30], while the axial velocity of 300 m/s fluctuates more indeed because the deformation generated during 300 m/s impacts greater than 100 m/s impact. When the impact velocity reaches more than 500 m/s, the axial velocity of the projectile increases sharply and then gradually stabilizes; the projectile spreads around in the form of fragments, and the impact point acquires a certain velocity, causing harm easily with the velocity of the fragments exceeding the initial velocity [31].…”
Section: Impact Of Projectile Velocity On the Damage Effectmentioning
confidence: 99%
“…As shown in Figure 7, when the impact velocity is 100 m/s and 300 m/s, the axial velocity at the impact point of the projectile varies in pulsation because the bullet attached to the impact point of the projectile produces elastic deformation after the end of the impact process [30], while the axial velocity of 300 m/s fluctuates more indeed because the deformation generated during 300 m/s impacts greater than 100 m/s impact. When the impact velocity reaches more than 500 m/s, the axial velocity of the projectile increases sharply and then gradually stabilizes; the projectile spreads around in the form of fragments, and the impact point acquires a certain velocity, causing harm easily with the velocity of the fragments exceeding the initial velocity [31].…”
Section: Impact Of Projectile Velocity On the Damage Effectmentioning
confidence: 99%
“…Light gas guns can be used to simulate, under controlled laboratory conditions, both the ejection of material from beneath a layer of ice and to simulate the hypervelocity impacts that would occur in a Stardust type sample return mission. Previous work utilising light gas guns and ice targets has examined the crater morphology of impacts into ice (Grey et al 2001;Harriss and Burchell 2017;Sheng-wei et al 2017) and have shown the survival of organic compounds in ejecta material when solid ice targets experience hypervelocity impacts (Bowden et al 2009). However, using targets composed of a layer of ice over a liquid (which can be doped with potential organic compounds) could be used to generate a plume of liquid being ejected from beneath the ice.…”
Section: Plume and Sample Collectionmentioning
confidence: 99%