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Lecture #31: Satellites and Rings II The Main Point • Ring Systems – Overview of rings: All of the giant planets have rings, which are just billions of small dusty, rocky, or icy moons traveling in similar orbits around a planet according to Kepler’s laws. • Jupiter, Jupiter Saturn Saturn, Uranus, Uranus Neptune. Neptune – What are rings made of? – How do they form? • Reading: Chapter 11.3. Astro 102/104 1 Astro 102/104 2 Planetary Ring Systems Overview • All four of the giant planets have rings. • Each ring system consists of billions of small "moonlets" orbiting close to their planet. • Ring systems exhibit complex structures and patterns caused by interactions with larger moons. Properties of Ring Systems ________________________________________________________________________________________________________________________________________ Planet Jupiter Saturn Uranus Neptune Astro 102/104 Outer Radius (km) Rplanet 128,000 1.8 140,000 2.3 51,000 2.2 63,000 2.5 Mass (kg) ~1010 1019 1014 1012 Reflectivity (%) ~5 60 ~5 ~5 3 Astro 102/104 4 1 What are Rings? Rings and Tides • Rings exist inside the "tidal stability limit" of a planet. • Within this limit, known as the Roche limit, limit a planet's gravity should break up satellites. • Only very small moons and rings exist within this zone. • Billions of moons! • marble-sized to house-sized (Saturn) • dust-sized (Jupiter, Uranus, Neptune) • Rings g are collections of huge g numbers of small bodies,, each moving on its own, independent, Keplerian orbit. • Because of Kepler's Third Law, inner ring particles must move faster than outer ring particles (differential rotation): - Rings don't rotate as a solid body. • Particles collide & interact gravitationally with each other: - Waves and other phenomena are generated in the process. Cloud Tops Each planet's ring system drawn to a different scale. Astro 102/104 5 Astro 102/104 6 Saturn's Rings Where Do Rings Come From? • Small impacts on small moons create dust-sized ring particles that disperse into an orbiting disk. • Occasional larger impacts on small moons can shatter the moon and release many man boulder-sized bo lder si ed ring particles. One of the most beautiful sights in the solar system! Saturn's Ring System _________________________________________________________________________________________________________________________________ Ring F A Cassini Division B C Outer Edge (km) Rplanet 140,180 2.324 136,780 2.227 122,170 2.025 117,580 1.949 92,000 1.525 Width (km) 90 14,600 4,590 25,580 17,490 CB A F Cassini Division Astro 102/104 7 Astro 102/104 8 2 Cassini Images of Saturn’s Rings • There are actually thousands of rings and gaps. • Gaps can be cleared by so-called gap moons orbiting within the rings. • Other gaps are due to orbital resonances with small inner moons. • Two nearby gap moons can shepherd a narrow ring. • Some rings are dense & bright, others thin & transparent. Astro 102/104 Rings in their natural color Cassini s first image Cassini’s of the F ring "Spokes" seen in the rings are thought to result from interactions between ring particles and Saturn’s magnetosphere. 9 False color image of two densityAstro waves in Saturn's 102/104 A ring Jupiter's Rings Rings are Thin! • • Saturn's rings are about 6 times wider than Earth. • But they are less than 100 meters thick! • Sometimes the rings appear edge-on from Earth. • Discovered from infrared telescopes and Voyager 1. Very different from Saturn's! • Three main components: – Very dark, very small particles. – Halo alo • Broad, faint inner torus. Saturn "ring plane crossing" observed with HST in 1996. – Main Ring • 7000 km wide. • Edge radius is 129,000 km. – Gossamer Rings • Broad, faint outer disks. • Astro 102/104 10 11 Dust particles from the small inner satellites of Jupiter appear to be the source of ring material. Astro 102/104 13 3 How were Jupiter’s rings observed? Light Scattering Observing rings at different viewing geometries provides a way to determine the sizes of ring particles. • Jupiter's rings are very dark and very faint. • Hard to see against the glare of Jupiter itself. • The best images were obtained when the Galileo spacecraft flew into Jupiter's shadow and looked back towards the Sun • Amazing navigation feat! Astronomers have also used radar to estimate the sizes of ring particles. Confirmed by Voyager radio occultation data. Astro 102/104 14 Uranian Rings Distance (km) ------------38000 41840 42230 42580 44720 45670 47190 47630 48290 50020 51140 15 Neptune's Rings Ring ------Diffuse Inner Plateau Main 10 main narrow rings, 1 diffuse ring. Ring ------1986U2R 6 5 4 Alpha Beta Eta Gamma Delta 1986U1R Epsilon Astro 102/104 Width (km) ---------2,500 1-3 2-3 2-3 7-12 7-12 0-2 1-4 3-9 1-2 20-100 Astro 102/104 Distance (km) -------41900 53200 53200 62930 Width (km) ----15 15 5800 < 50 Name ------Galle LeVerrier Lassell, Arago Adams (distance is from Neptune's center to the ring's inner edge) • 3 main narrow rings, 1 diffuse. • Main rings appear “clumpy”: • Once thought to be arcs, not rings. • Voyager showed that they are rings. 16 Astro 102/104 17 (distance is from Uranus' center to the ring's inner edge) 4 Keeping it all together: Shepherds Ring Composition Small inner moons of the giant planets can gravitationally "shepherd" the ring particles, maintaining their stability. • Saturn's rings are bright and slightly red: – Spectra show evidence for water ice. – Red component p unknown... "dirt"? "organics"? g • Jupiter's, Uranus', and Neptune's rings are all very dark and gray: Pandora and Prometheus, Shepherding Saturn's tenuous F ring Two Uranian shepherds Astro 102/104 18 – Not water ice? – "Carbonaceous" material? Dark "organics"? • Differences due to different ring origins? Astro 102/104 19 Next Lecture... Summary • The Trans-Neptunian Region • All of the outer gas giant planets have ring systems. • Saturn's rings are made up of billions of chunks of dirty ice, each obeying Kepler’s laws. • The rings of Jupiter Jupiter, Uranus Uranus, and Neptune are composed of smaller (dust-sized) and much darker particles of unknown composition. • Rings occupy regions within the tidal stability zones of their planets: – Pluto: • Discovery. • Physical Ph i l characteristics. h i i • Charon. – Other Kuiper Belt Objects. • Reading: Chapter 12.3 – Ongoing impacts on small moons create ring particles and explain why rings are common. Astro 102/104 20 Astro 102/104 21 5