The Water Vapor and Dust Plumes of Enceladus

dc.contributor.advisorHill, Thomas W.en_US
dc.contributor.committeeMemberReiff, Patricia H.en_US
dc.contributor.committeeMemberSemmes, Stephenen_US
dc.creatorDong, Yaxueen_US
dc.date.accessioned2014-08-05T20:41:09Zen_US
dc.date.available2014-08-05T20:41:09Zen_US
dc.date.created2014-05en_US
dc.date.issued2014-02-11en_US
dc.date.submittedMay 2014en_US
dc.date.updated2014-08-05T20:41:09Zen_US
dc.description.abstractEnceladus is the most active moon of Saturn. Its south polar plume, composed mostly of water vapor and ice grains, is one of the groundbreaking discoveries made by the Cassini spacecraft. During Cassini’s E2, E3, E5 and E7 encounters with Enceladus, the Ion and Neutral Mass Spectrometer (INMS) measured high neutral water vapor densities up to ~10^9 cm-3 (Waite et al., 2006; Teolis et al., 2010; Dong et al., 2011). We have constructed a physical model for the expected water density in the plumes, based on supersonic radial outflow from one or more of the surface vents. We apply this model to possible surface sources of water vapor associated with the multiple jets observed in the visible dust plumes (Spitale and Porco, 2007). Our model predictions fit well with the INMS measurements of neutral water vapor density along the E3, E5, and E7 trajectories. The fit is optimized by values of outflow velocity in the range ~550–750 m/s and values of total source rate in the range ~1.5 − 3.5 10^28 H2O molecules/s ~ 450 – 1050 kg/s. The model can be extended to incorporate the jet features within the plume observed during the E7 encounter. The dust (ice grain) plumes of Enceladus have been observed by multiple Cassini instruments. We propose a composite ice grain size distribution covering a continuous size range from nanometer to micrometers, by combining the CAPS (Cassini Plasma Spectrometer) nanograin size distributions (Hill et al., 2012) and the CDA (Cosmic Dust Analyzer) and RPWS (Radio and Plasma Wave Science) dust power-law size distribution (Kempf et al., 2008; Ye et al., 2012, 2013). We also study the grain charging process using the RPWS-LP (Langmuir Probe) data (Morooka et al., 2011). Based on the size distribution and charge per grain, the densities, source rate, motion, and currents of the ice grains can be calculated. We found that the grains ~2-20 nm dominate in both charge density and number density. The total grain mass density is likely to be ~ 1- 10 times that of the water vapor, and the grain mass loading rate is ~100 kg/s. The motion of the charged grains in Saturn’s magnetosphere implies a transition from ion-like motion to neutral-like motion as the grain size increases from ~nm to ~μm. The grains carry a total current of ~10^5 A at Enceladus, which leads to a different current system from that of the ion pick-up and associated Birkeland currents. The grain current system may be dominant or at least comparable to the ion pick-up current system in accounting for the magnetic perturbations observed near Enceladus.en_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.citationDong, Yaxue. "The Water Vapor and Dust Plumes of Enceladus." (2014) Diss., Rice University. <a href="https://hdl.handle.net/1911/76427">https://hdl.handle.net/1911/76427</a>.en_US
dc.identifier.urihttps://hdl.handle.net/1911/76427en_US
dc.language.isoengen_US
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.en_US
dc.subjectEnceladusen_US
dc.subjectNeutral cloudsen_US
dc.subjectDusten_US
dc.subjectSaturnen_US
dc.subjectMagnetosphereen_US
dc.subjectSpace physicsen_US
dc.titleThe Water Vapor and Dust Plumes of Enceladusen_US
dc.typeThesisen_US
dc.type.materialTexten_US
thesis.degree.departmentPhysics and Astronomyen_US
thesis.degree.disciplineNatural Sciencesen_US
thesis.degree.grantorRice Universityen_US
thesis.degree.levelDoctoralen_US
thesis.degree.nameDoctor of Philosophyen_US
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