Having found values for the pressures and as a function of the initial conditions , , and , the problem is completely solved. Indeed, using the shock adiabatic relation is known. With this, the values of , , and are determined by means of eq.(28.12), eq.(28.13), eq.(29.9) and eq.(29.10) respectively. The values for all the pressures and specific volumes are obtained using eqs.(28.6)-(28.8) and eqs.(29.4)-(29.6). The velocities of the flow, as defined in fig.(V.1), are calculated either by mass flux conservation on crossing a shock, or by the formula for the velocity discontinuity in eq.(27.6). The hydrodynamical values of the pressure and density inside the rarefaction wave come from eqs.(27.2)-(27.5).
In order to analyse the variations of the hydrodynamical quantities as a function of position and time, let us now describe the problem in a system of reference in which the gas far away to the right of the cloud is always at rest, as illustrated in fig.(V.4). Let and be the coordinates of the left and right tangential discontinuities, and the coordinates of the reflected and transmitted shocks produced after the first initial discontinuity, the position of the transmitted shock after the second initial discontinuity and and the left and right weak discontinuities which bound the rarefaction wave. The new velocities are defined by Galilean transformations:
|
The direction of motion of the flow is shown in fig.(V.4) and it follows from eq.(28.17), eq.(28.20) and eq.(30.2) that points to the left in this system of reference. Since, in the same frame, and point to the right, continuity across a weak discontinuity demands to behave in the same way.
The tangential discontinuities and the shocks produced by the initial discontinuities move with constant velocity throughout the gas. This implies that the time at which the first initial discontinuity takes place is:
where represents the initial width of the cloud. Hence, the positions of all different discontinuities for are:
and for , eqs.(30.8)-(30.9) are valid together with
The time at which the left tangential discontinuity collides with the left boundary of the rarefaction wave is given by , and thus:
Fig.(V.5) shows the variation of the pressure and density as a function of time and position in a system of reference in which the gas far away to the right of the cloud is at rest.
The width of the cloud varies with time, and it follows from eq.(30.9) and eq.(30.13) that this variation is given by:
where is the Heaviside step function. This linear relation is plotted in fig.(V.6).
Sergio Mendoza Fri Apr 20, 2001