Dissipative Instability of Shock Waves

被引:4
作者
Chefranov, S. G. [1 ,2 ]
机构
[1] Russian Acad Sci, Obukhov Inst Atmospher Phys, Moscow 119017, Russia
[2] Technion Israel Inst Technol, Dept Phys, IL-32000 Haifa, Israel
基金
以色列科学基金会; 俄罗斯科学基金会;
关键词
EQUATION-OF-STATE; STABILITY; HUGONIOT; WATER; GASES; GPA;
D O I
10.1134/S1063776120030036
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
A new condition is obtained for the linear instability of a plane front of an intense shock wave in an arbitrary medium, which is determined by the finiteness of the viscosity. It is shown that the shock front instability occurs due to dissipative instability of the flow behind the front, which is analogous to the flow instability in the boundary layer. It is found that in the low-viscosity limit, one-dimensional longitudinal perturbations increase much faster than two-dimensional (corrugation) perturbations. The results are compared with the available data of experimental observation and numerical simulation of instability of shock waves. The comparison shows a better agreement between the new absolute shock instability as compared to the condition of such instability in the classical D'yakov theory disregarding viscosity.
引用
收藏
页码:633 / 642
页数:10
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