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Implementation of Tillotson Equation of State for Hypervelocity Impact of Metals, Geologic Materials, and Liquids

机译:金属,地质材料和液体超细兴奋地影响intotson方程的实施

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The Tillotson equation of state (EOS), which was originally developed for the hypervelocity impact of metals, was augmented with an additional region in expansion to provide full coverage of the density-energy space and a new cavitation model for liquids. This EOS was implemented into CTH, Sandia National Laboratories Eulerian, finite-volume, shock physics code, for the general purpose of simulating hypervelocity impacts of metals, geologic materials, and liquids; however, the salient features of this EOS in both compression and expansion are evaluated for water given the ubiquity of available data. Addition of a cavitation model allows for treatment of liquid spall when the local pressure drops below the vapor pressure in events such as underwater blasts and high speed projectiles or fragments in liquids. The EOS is evaluated by comparing the response to previously published dynamic compression experiments. Additionally, the model results are compared against the Mie-Gruneisen and SESAME equations of state already in the CTH database.
机译:最初为金属的超细兴趣产生的状态(EOS)的Tillotson方程被扩展的额外区域增强,以提供密度 - 能量空间和液体新空化模型的全面覆盖。该EOS实施到CTH,桑迪亚国家实验室欧拉,有限卷,休克物理规范,用于模拟金属,地质材料和液体的超胶质影响;然而,给出了鉴于可用数据的无处不经劲的水,评估了这种EOS在压缩和扩展中的突出特征。添加空化模型允许在局部压降低于诸如水下喷射和高速射弹或液体碎片的情况下局部压力下降时液体剥落。通过将响应与先前公布的动态压缩实验进行比较来评估EOS。另外,将模型结果与CTH数据库中已经存在的状态的MIE-Gruneisen和Sesame方程进行比较。

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