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Saturn neutral particle modeling Overview of Enceladus/Titan research with possible application to Mercury Johns Hopkins University Applied Physics Laboratory H. Todd Smith
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Show examples of how we used neutral particle modeling with data analysis for studying the Saturnian system Titan and Enceladus neutral particle source investigation Initial ground work for possible assistance with Mercury neutral particle prediction and analysis Introduction
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Investigating neutral particle sources and processes in Saturnian system Particle distribution Source & interaction characterization Titan (nitrogen/methane) Enceladus (water, nitrogen species) Pre-Cassini arrival predictions (data limited to 3 fly-bys and Earth based observations) Post-arrival interpretation using data analysis and modeling Current Research
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Predicted nitrogen source - Titan - Dense atmosphere (~95% Nitrogen) - Larger than Mercury - No intrinsic magnetic field Anticipated nitrogen source (Pre-Cassini)
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3-D neutral particle model Multi-species, multi-resolution Modeled aspects All gravitational effects and collisions Particle interactions with photons, electrons & ions Output 3-D Neutral particle density and topology Ion production Model predictions Computational Model Overview
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Neutral densities too low for direct detection (must detect ionization products – CAPS) Titan could produce N + in inner magentosphere (6-10 Rs) N 2 shows same basic trend but with lower densities Modeling Predicted Titan-Generated Nitrogen Tori
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Nitrogen detected using CAPS! (…but not where anticipated) Analysis indicated source at Titan’s orbit CAPS N+ data
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Things are not as expected - Mainly H2O ice - Geologically young surface - New images indicate source of E-ring Credit: NASA/JPL/Space Science Institute Dominant nitrogen source in vicinity of Enceladus orbit
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Enceladus observations concur Enceladus “plumes” detected Tiger stripes – south pole Possible nitrogen source (Water dominated) Principal source of E-ring Subsurface composition questions Cassini Ion Neutral Mass Spectrometer (mass 28 detection ~4%) What processes produce these plumes Neutral particles provide clues to mechanisms Water should remain frozen under pressure/temperature conditions Ammonia (& possibly N 2 ) could explain plume activity (controversial) (despite large efforts, no previous detections of ammonia) Credit: NASA/JPL/Space Science Institute
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What is the source species for N + N 2 Enceladus source (if present) could produce observed N + CAPS N+ data
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Ammonia detected Figure 5. Upper limit for N 2 + and NH x + based on CAPS LEF observations. Results shown as the upper limit N 2 + (red bars) and NH x + (black line) percentage of all heavy ions as a function of radial distance from Saturn in planetary radii (Rs). Error bars represent 1-sigma errors for peak widths. (Enceladus orbits at ~4 Rs while Titan is ~20Rs from Saturn).
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Using modeling to understand Enceladus source mechanisms Column Narrow torus Scattered torus OH Observations * Johnson et al., The Enceladus and OH Tori at Saturn, ApJ Letters, 644:L137-L139, 2006
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3-D neutral particle distributions assisting with field data interpretation Io Enceladus
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Constraining Enceladus source using neutral particle data and modeling Larger than expected ejection velocity (~750 m/s) Ejection angle limited (< 30 degrees from pole) Variable source rate (~3-10 x 10 27 /sec)
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Enceladus dominant source in Saturn’s magnetosphere…WHY?? Possible causes and focus of latest research Atmospheric interactions are more complex than estimates (effecting atmospheric loss) Plasma environment more complex Hydrodynamic methane escape?
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Modifying model for the Mercury system Sample data in 3-D model along spacecraft trajectory Local densities and source characterization Global distributions Spatial and temporal variation Insight into interaction process Coordinate with other modeling efforts to avoid duplication of effort Pre-arrival predictions to optimize instrument utilization Post-arrival modeling to help interpret observations Possible research
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