Work in the rest frame of a thin planar shock wave, with normal upstream and downstream velocities . Assume a steady flow, negligible gravitational change across its thickness, no radiative energy loss, and negligible viscous stress and heat flux at the two remote faces of a control volume. Dissipation within the shock is permitted and is essential to the physical discontinuity.
Integrating mass conservation through that volume gives equal mass flux per unit area:The dimensions of are . The normal momentum entering minus that leaving must balance the pressure forces. Equivalently, the conserved normal momentum flux is , givingFor conservation of energy, matter advects kinetic and internal energy while pressure performs work at rate per unit area. Writing for specific internal energy, the energy flux is . With specific enthalpy , its conservation givesThe division by is valid for a genuine through-flow shock. Together these are the three Rankine-Hugoniot conditions. The conserved energy flux has units , and both momentum fluxes have units of pressure.
For a calorically perfect ideal gas, and . The three jump conditions can be combined explicitly. Put , so andSubstitute these into the enthalpy equation and use , with the upstream adiabatic sound speed. Besides the trivial no-shock root , the physical compression root isFor unchanged composition, . A compressive shock has and increases the specific entropy. Thus an adiabatic shock conserves total energy but is not an isentropic process.
Articles by others on the same topic
There are currently no matching articles.