Abstract
The conservation equations for the flow field developed behind a
spherical shock wave propagating into a dusty medium (gas seeded with
small uniformly distributed solid particles) are solved numerically by
using the random choice method. The solutions obtained were compared
with a similar pure-gas case. It was found that the dust presence
weakens the shock wave, i.e., the gas velocity, temperature, and
pressure immediately behind the shock-wave front were lower than those
obtained in a similar pure-gas case. The presence of dust changed the
flow field behind the shock wave. The typical spherical-wave pressure
signature (a monotonic reduction in the pressure after the jump across
the shock-wave front) changed to a different shape. The pressure
increased after the shock-wave front until it reached a maximum value
followed by a monotonic pressure reduction. The maximum pressure was
attained between the shock-wave front and the contact surface. Higher
values of total pressure were obtained in the dusty-gas case. The
initial uniform spatial distribution of the dust particles changed into
a bell-shaped pattern with a pronounced peak.
Original language | English |
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Title of host publication | Workshop on Space Fluid Dynamics and Related Problems |
Pages | 48-57 |
State | Published - 1990 |
Keywords
- Earth Atmosphere
- Flow Equations
- Shock Wave Propagation
- Spherical Waves
- Two Phase Flow
- Dust
- Partial Differential Equations
- Pressure Distribution
- Temperature Distribution
- Velocity Distribution