The formation of a singularity in a compressible gas, as described by the Euler equation, is characterized by the steepening and eventual overturning of a wave. Using self-similar variables in two space dimensions and a power series expansion based on powers of , being the singularity time, we show that the spatial structure of this process, which starts at a point, is equivalent to the formation of a caustic, i.e. to a cusp catastrophe. The lines along which the profile has infinite slope correspond to the caustic lines, from which we construct the position of the shock. By solving the similarity equation, we obtain a complete local description of wave steepening and of the spreading of the shock from a point. The shock spreads in the transversal direction as and in the direction of propagation as , as also found in a one-dimensional model problem.
Spatial structure of shock formation / Eggers, J.; Grava, Tamara; Herrada, M. A.; Pitton, Giuseppe. - In: JOURNAL OF FLUID MECHANICS. - ISSN 0022-1120. - 820:June 2017(2017), pp. 208-231. [10.1017/jfm.2017.205]
Spatial structure of shock formation
Grava, Tamara;Pitton, Giuseppe
2017-01-01
Abstract
The formation of a singularity in a compressible gas, as described by the Euler equation, is characterized by the steepening and eventual overturning of a wave. Using self-similar variables in two space dimensions and a power series expansion based on powers of , being the singularity time, we show that the spatial structure of this process, which starts at a point, is equivalent to the formation of a caustic, i.e. to a cusp catastrophe. The lines along which the profile has infinite slope correspond to the caustic lines, from which we construct the position of the shock. By solving the similarity equation, we obtain a complete local description of wave steepening and of the spreading of the shock from a point. The shock spreads in the transversal direction as and in the direction of propagation as , as also found in a one-dimensional model problem.File | Dimensione | Formato | |
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