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INVESTIGATION AND MODELLING OF LARGE SCALE CRATERING EVENTS – LESSONS LEARNT FROM EXPERIMENTAL ANALYSIS

机译:大型策划活动的调查和建模-从实验分析中学到的经验教训

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Initiated as part of the 2010 Spin Your Thesis campaign, a new ESA Education programme, a group from theUniversity of Glasgow Space Advanced Research Team successfully conducted a series of impact crateringexperiments under a highly accelerated reference frame. This aimed to: reproduce and define the physical conditionsof large-scale cratering events onto highly porous asteroids; provide cratering response data for the validation andadvancement of numerical models; and support the generation of a reliable scaling theory for cratering events.Impact cratering is a fundamental process that has shaped and continues to shape the formation and evolution of oursolar system and other planetary systems. Although much is known on the impact dynamics of rocky, brittle bodies,such as asteroids, little is known on the physical response of highly porous bodies. Consequently the physicalresponse of porous bodies can not be compared to conventional models. Therefore throughout the experimentcampaign, variation into the target material's porosity and projectile density was examined. All in-situmeasurements were recorded relative to the crater's morphological profile and ejecta distribution. This occurredunder increasing levels of acceleration, thereby validating that the experiment occurred within the crater dominatedgravity regime. This paper details the programmatics issues of the initiative, experiences and lessons learnt from thestudent perspective. From its initial proof-of-concept the Spin Your Thesis campaign provided a solid foundationfrom the development of an experimental idea, enabling high scientific return and personal development.
机译:作为2010年“旋转您的论文”运动的一部分,该组织发起了一项新的ESA教育计划,该计划由 格拉斯哥大学太空高级研究小组成功进行了一系列撞击坑试验 在高度加速的参考框架下进行实验。目的是:重现和定义身体状况 在高度多孔的小行星上发生大规模的陨石坑事件;提供缩孔反应数据以进行验证,并 数值模型的发展;并支持为陨石坑事件生成可靠的缩放理论。 撞击坑是一个基本过程,已经塑造并继续塑造着我们的形成和演化 太阳系和其他行星系统。尽管人们对岩石脆性物体的冲击动力学了解很多, 例如小行星,对高度多孔的物体的物理反应知之甚少。因此,身体 多孔体的响应不能与传统模型相比。因此在整个实验中 运动后,检查了目标材料的孔隙率和射弹密度的变化。全部原位 记录相对于陨石坑的形态轮廓和喷射分布的测量值。这发生了 在不断增加的加速度下,从而验证了实验在火山口内占主导地位 重力政权。本文详细介绍了该计划的程序设计问题,从该计划中学到的经验和教训 学生的观点。从最初的概念验证开始,“旋转您的论文”活动就奠定了坚实的基础 从实验想法的发展,可以实现高科学回报和个人发展。

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