On understanding the physics of the Enceladus south polar plume via numerical simulation

• Published in: Icarus (New York, N.Y. 1962) Vol. 253; pp. 205 - 222
• Main Authors: Yeoh, Seng Keat, Chapman, Todd A., Goldstein, David B., Varghese, Philip L., Trafton, Laurence M.
• Format: Journal Article
• Language: English
• Published: Elsevier Inc 01.06.2015
• Subjects: Altitude; Computer simulation; Enceladus; Grains; Mass ratios; Monte Carlo methods; Nanostructure; Satellites, atmospheres; Saturn, satellites; Vents; Satellites, atmospheres; Saturn, satellites; Enceladus
• ISSN: 0019-1035; 1090-2643
• DOI: 10.1016/j.icarus.2015.02.020

•We simulate the Enceladus two-phase plume to study its physics.•Plume spans several regimes, from continuum at vents to free-molecular higher up.•Grains barely affect the gas for ice/vapor mass ratios ⩽1.0.•Grains decouple from the gas ⩽100 vent diameters from the surface.•Velocity difference at vents only spreads μm-sized grains by ⩽12°. The Enceladus plume is composed of primarily water vapor and tiny ice grains. Various observations suggest that it most likely originates from vents along the Tiger Stripes. Consequently, understanding the expansion process of the two-phase flow from the vents into vacuum is crucial. Our goal is to investigate the important physical processes and the interaction between the gas and the grains associated with the expansion process. To do so, we compute the expansion flow from the vents out to higher altitudes using the direct simulation Monte Carlo (DSMC) method with two-way coupling between the gas and the grains. The expansion flow passes through multiple regimes, from continuum (very collisional) near the vents to free-molecular (collisionless) at higher altitudes. This transition occurs at a few kilometers high for meter-sized vents and is higher up for larger vents. During expansion, the Mach number increases rapidly in the first few vent diameters mainly due to a drop in gas temperature rather than an increase in gas speed. Collisions at the vent strongly affect the molecular speeds in the far-field (as the flow becomes free-molecular). If the flow is sufficiently collisional at the vent, the molecular speeds approach the ultimate speed of adiabatic expansion, which depends on the source conditions (∼1005m/s for the triple-point of water). The flow is highly supersaturated as it emerges from the vents, thus condensation grain growth is very likely. We find that condensation growth via heterogeneous nucleation above the vents is proportional to vent size and that fairly large vents several tens to hundreds of meters in size are required to produce the micron-sized grains detected by CDA (radii ⩾1.6μm) if the grains start with a negligible size at the vents. We also examine how the effects of grains on the gas vary with grain size, grain/gas (ice/vapor) mass ratio and gas–grain velocity difference at the vent. The effects of grains increase with mass ratio and velocity difference at the vent due to greater exchange of momentum and energy. Moreover, smaller grains have a stronger effect for the same mass ratio. However, the effects of grains are minimal for plausible mass ratios ⩽1.0. Our studies show that nanometer-sized grains decouple from the gas at altitudes of 10–100 vent diameters and spread more with the gas while micron-sized grains decouple at <10 vent diameters and remain in collimated beams. Even with large velocity differences at the vent, the micron-sized grains spread by ⩽12°. Consequently, the inferred spreading angles ⩾30° (Ingersoll, A.P., Ewald, S.P. [2011]. Icarus 216, 492–506; Postberg, F. et al. [2011]. Nature 474, 620–622) cannot be caused by velocity difference at the vent alone. Furthermore, nanometer-sized grains are accelerated close to gas speeds while micron-sized grains tend to retain the initial speeds they had at the vent. We determine that the largest grain size that can be accelerated from rest to escape speeds (>240m/s) is proportional to vent size and that small vents (<1m) are enough to accelerate large micron-sized grains to escape speeds.