McDonnell, J.A.M; Catling, D.J. and Clegg, R.A.
|DOI (Digital Object Identifier) Link:||http://doi.org/10.1016/S0273-1177(01)00367-2|
|Google Scholar:||Look up in Google Scholar|
The availability of hydrocodes with crack growth modelling provides an opportunity to study the extended spallation region for brittle targets such as ices, where conchoidal fracture dominates the volume of crater excavation. Autodyn version 220.127.116.11 using Johnson-Holmquist crack modelling is explored in this role to investigate ejecta size and velocity distributions following validation in quasi-static runs which mimic laboratory measurements of glass and water ice. It is found that the code can model, with realistic values, bulk material properties and fracture patterns. Ejecta size and velocity distributions are presented which indicate low ejecta velocities which would lead to regolith development on 500m diameter objects in the Jovian or Saturnian system. The code is also able to track momentum reaction during impact and establish catastrophic collision limits of icy or rocky bodies under meteoroid impacts.
|Item Type:||Journal Article|
|Academic Unit/Department:||Other Departments > Other Departments
|Depositing User:||Users 6044 not found.|
|Date Deposited:||06 Jul 2006|
|Last Modified:||14 Jan 2016 15:56|
|Share this page:|