Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-02T20:40:06.244Z Has data issue: false hasContentIssue false

A model problem for a supersonic gas jet from a moon

Published online by Cambridge University Press:  22 April 2016

H. G. Hornung*
Affiliation:
Graduate Aerospace Laboratories, California Institute of Technology, Pasadena, CA 91125, USA
*
Email address for correspondence: [email protected]

Abstract

Some celestial bodies such as planets, moons and comets (here referred to as moons for simplicity) emit jets of material at speeds that in some instances are large enough to escape gravity. Previous investigations have shown this problem to be highly complex, e.g. involving multi-phase flows, phase changes, radiation and gas rarefaction effects. In order to learn from exploring a manageable parameter space, and to provide a limiting case, the present study considers a much simpler model situation in which the material of the jet is an inviscid, non-heat-conducting, perfect gas that issues radially at the surface of the moon with sonic velocity. Theoretical considerations show that the escape velocity of a gas is much smaller than that of a solid body. An analytical solution is obtained for the maximum height reached by a jet in steady flow. A computational parameter study of unsteady, inviscid, axisymmetric flow, including the effect of an atmosphere, provides a rich picture of the features and behaviour of the model jet. The deficit of the computed maximum steady-state penetration height below the isentropic theoretical value may be explained by the effect of the atmosphere and of dissipation in shock waves that occur in the computed flows. Many of the features of the gas jet are qualitatively mirrored in an experiment using a water flow analogy in which the gravitational field is simulated by a surface of suitable shape.

Type
Papers
Copyright
© 2016 Cambridge University Press 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Ingersoll, A. P. & Ewald, S. P. 2011 Total particulate mass in Enceladus plumes and mass of Saturn’s E-ring inferred from Cassini ISS images. Icarus 216, 492506.CrossRefGoogle Scholar
Kieffer, S. W. & Sturtevant, B. 1984 Laboratory studies of volcanic jets. J. Geophys. Res. 89, 82538268.Google Scholar
Kieffer, S. W. & Sturtevant, B. 1988 Furrows formed during the lateral blast of Mt St Helens May 18, 1980. J. Geophys. Res. 93, 793816.Google Scholar
McDoniel, W. J.2015 Realistic simulation of Io’s Pele plume and its effect on Io’s atmosphere. PhD thesis, University of Texas at Austin.Google Scholar
McDoniel, W. J., Goldstein, D. B., Varghese, P. L. & Trafton, L. M. 2015 Three-dimensional simulation of gas and dust in Io’s Pele plume. Icarus 257, 251274.Google Scholar
Ogden, D. E. 2011 Fluid dynamics in volcanic vents and craters. Earth Planet. Sci. Lett. 312, 401410.Google Scholar
Ogden, D. E., Glatzmaier, G. A. & Wohletz, K. H. 2008 Effects of vent overpressure on buoyant eruption columns: implications for plume stability. Earth Planet. Sci. Lett. 268, 283292.Google Scholar
Orescanin, M. M., Prisco, D., Austin, J. M. & Kieffer, S. W. 2008 Flow of supersonic jets across flat plates: implications for ground-level flow from volcanic blasts. J. Geophys. Res. 119, 29762987.Google Scholar
Quirk, J. J. 1998 Amrita – a computational facility (for CFD modelling). In VKI CFD Lecture Series, vol. 29. von Karman Institute.Google Scholar
Yeoh, S. K., Chapman, T. A., Goldstein, D. B., Varghese, P. L. & Trafton, L. M. 2015 On understanding the physics of the Enceladus south polar plume via numerical simulation. Icarus 253, 205222.Google Scholar

Hornung supplementary movie

Numerical simulation of gas dynamic jet from a moon with inverse square gravity, pressure ratio 60, velocity ratio 0.9354, specific heat ratio 1.4. The graph shows pressure (green) density (blue) velocity (red) along the jet axis. The heavy blue line is the atmospheric pressure and density distribution

Download Hornung supplementary movie(Video)
Video 62.5 MB

Hornung supplementary movie

Shallow water analogy of gas dynamic jet with surface representing inverse square potential well

Download Hornung supplementary movie(Video)
Video 20.5 MB