Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Propagation of a curved weak shock

View through CrossRef
Propagation of a curved shock is governed by a system of shock ray equations which is coupled to an infinite system of transport equations along these rays. For a two-dimensional weak shock, it has been suggested that this system can be approximated by a hyperbolic system of four partial differential equations in a ray coordinate system, which consists of two independent variables (ζ, t) where the curves t = constant give successive positions of the shock and ζ = constant give rays. The equations show that shock rays not only stretch longitudinally due to finite amplitude on a shock front but also turn due to a non-uniform distribution of the shock strength on it. These changes finally lead to a modification of the amplitude of the shock strength. Since discontinuities in the form of kinks appear on the shock, it is necessary to study the problem by using the correct conservation form of these equations. We use such a system of equations in conservation form to construct a total-variation-bounded finite difference scheme. The numerical solution captures converging shock fronts with a pair of kinks on them – the shock front emerges without the usual folds in the caustic region. The shock strength, even when the shock passes through the caustic region, remains so small that the small-amplitude theory remains valid. The shock strength ultimately decays with a well-defined geometrical shape of the shock front – a pair of kinks which separate a central disc from a pair of wings on the two sides. We also study the ultimate shape and decay of shocks of initially periodic shapes and plane shocks with a dent and a bulge.
Title: Propagation of a curved weak shock
Description:
Propagation of a curved shock is governed by a system of shock ray equations which is coupled to an infinite system of transport equations along these rays.
For a two-dimensional weak shock, it has been suggested that this system can be approximated by a hyperbolic system of four partial differential equations in a ray coordinate system, which consists of two independent variables (ζ, t) where the curves t = constant give successive positions of the shock and ζ = constant give rays.
The equations show that shock rays not only stretch longitudinally due to finite amplitude on a shock front but also turn due to a non-uniform distribution of the shock strength on it.
These changes finally lead to a modification of the amplitude of the shock strength.
Since discontinuities in the form of kinks appear on the shock, it is necessary to study the problem by using the correct conservation form of these equations.
We use such a system of equations in conservation form to construct a total-variation-bounded finite difference scheme.
The numerical solution captures converging shock fronts with a pair of kinks on them – the shock front emerges without the usual folds in the caustic region.
The shock strength, even when the shock passes through the caustic region, remains so small that the small-amplitude theory remains valid.
The shock strength ultimately decays with a well-defined geometrical shape of the shock front – a pair of kinks which separate a central disc from a pair of wings on the two sides.
We also study the ultimate shape and decay of shocks of initially periodic shapes and plane shocks with a dent and a bulge.

Related Results

Generation and modulation of shock waves in two-dimensional polariton condensates
Generation and modulation of shock waves in two-dimensional polariton condensates
Due to the ability of exciton-polariton condensates formed in semiconductor microcavities to be achieved at room temperature and their characteristics such as non-equilibrium and s...
Refractory Shock. Casuistics
Refractory Shock. Casuistics
Shock Syndrome is an acute progressive circulatory insufficiency where the Heart is unable to circulate the blood in time unit, for supplying with O2 to the cells and to take out f...
Characteristics of dynamic crack propagation in a weak snowpack layer over its entire life cycle
Characteristics of dynamic crack propagation in a weak snowpack layer over its entire life cycle
<p>For a slab avalanche to release, a weak layer buried below a cohesive snow slab is required, and the system of weak layer and slab must support crack propagation o...
Blast Wave Mitigation Through Confined Volume and Porous Material
Blast Wave Mitigation Through Confined Volume and Porous Material
Abstract Over a period of time, the impact of shock waves on human bodies and structures has been studied. To understand the shock wave mitigation over confined volume and ...
The Propagation of Hydromagnetic Cylindrical Shock Waves in Weak Magnetic Field, With A Self-Gravitating Gas
The Propagation of Hydromagnetic Cylindrical Shock Waves in Weak Magnetic Field, With A Self-Gravitating Gas
<p>The effects of overtaking disturbances behind the flow on the propagation of diverging cylindrical shock Waves through an ideal gas in presence of a magnetic field having ...
Propagation characteristics of partially coherent decentred annular beams propagating through oceanic turbulence
Propagation characteristics of partially coherent decentred annular beams propagating through oceanic turbulence
The analytical expressions for the average intensity and the centroid position of partially coherent decentred annular beams propagating through oceanic turbulence are derived, and...
Probing the mechanism underlying preshock desensitization of heterogeneous explosives via meso-resolved simulations
Probing the mechanism underlying preshock desensitization of heterogeneous explosives via meso-resolved simulations
To analyze the mechanism underlying preshock desensitization of heterogeneous explosives, two-dimensional, meso-resolved simulations were conducted to capture the shock-to-detonati...
Measuring slope-scale crack propagation in weak snowpack layers
Measuring slope-scale crack propagation in weak snowpack layers
&lt;p&gt;For a snow avalanche to release, a weak layer has to be buried below a cohesive snow slab. The slab-weak layer configuration must not only allow failure initiation...

Back to Top