Catastrophic disruption of layered ice-silicate bodies
Large icy Kuiper Belt Objects (KBOs) such as Pluto have observed densities on the order of 1.8 - 2.0 g cm-3. This indicates that they are made up of some combination of ice and silicate material; their size further implies that they will possess a differentiated structure with ice dominating towards...
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ndltd-bl.uk-oai-ethos.bl.uk-5899612015-03-20T05:00:03ZCatastrophic disruption of layered ice-silicate bodiesLightwing, Andrew2011Large icy Kuiper Belt Objects (KBOs) such as Pluto have observed densities on the order of 1.8 - 2.0 g cm-3. This indicates that they are made up of some combination of ice and silicate material; their size further implies that they will possess a differentiated structure with ice dominating towards the surface and silicate material dominating towards the core. A series of impact experiments using the University of Kent's light gas gun have been carried out in order to determine the impact strength of spherical layered ice-silicate targets that reflect the suspected structure of these bodies. Impacts are also carried out on unlayered ice-silicate targets and pure ice targets for the purposes of comparison. Impact velocities ranged from 1 to 7 km S-1 using a range of projectile sizes and materials including stainless steel, titanium, aluminium and copper. Data from previous work undertaken at the University of Kent is incorporated in order to provide a more complete picture of target behaviour.523.492University of Kenthttp://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.589961Electronic Thesis or Dissertation |
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523.492 Lightwing, Andrew Catastrophic disruption of layered ice-silicate bodies |
description |
Large icy Kuiper Belt Objects (KBOs) such as Pluto have observed densities on the order of 1.8 - 2.0 g cm-3. This indicates that they are made up of some combination of ice and silicate material; their size further implies that they will possess a differentiated structure with ice dominating towards the surface and silicate material dominating towards the core. A series of impact experiments using the University of Kent's light gas gun have been carried out in order to determine the impact strength of spherical layered ice-silicate targets that reflect the suspected structure of these bodies. Impacts are also carried out on unlayered ice-silicate targets and pure ice targets for the purposes of comparison. Impact velocities ranged from 1 to 7 km S-1 using a range of projectile sizes and materials including stainless steel, titanium, aluminium and copper. Data from previous work undertaken at the University of Kent is incorporated in order to provide a more complete picture of target behaviour. |
author |
Lightwing, Andrew |
author_facet |
Lightwing, Andrew |
author_sort |
Lightwing, Andrew |
title |
Catastrophic disruption of layered ice-silicate bodies |
title_short |
Catastrophic disruption of layered ice-silicate bodies |
title_full |
Catastrophic disruption of layered ice-silicate bodies |
title_fullStr |
Catastrophic disruption of layered ice-silicate bodies |
title_full_unstemmed |
Catastrophic disruption of layered ice-silicate bodies |
title_sort |
catastrophic disruption of layered ice-silicate bodies |
publisher |
University of Kent |
publishDate |
2011 |
url |
http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.589961 |
work_keys_str_mv |
AT lightwingandrew catastrophicdisruptionoflayeredicesilicatebodies |
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