David Nesvorny (Southwest Research Institute) David Nesvorny (Southwest Research Institute) Capture of Irregular Satellites during Planetary Encounters.

Slides:



Advertisements
Similar presentations
Origins of Regular and Irregular Satellites ASTR5830 March 19, :30-1:45 pm.
Advertisements

Origins of Regular and Irregular Satellites ASTR5830 March 21, :30-1:45 pm.
Planetary Rings All four jovian planets have ring systems girdling their equators. Many of the inner jovian moons orbit close to (or even within) the parent.
Kozai Migration Yanqin Wu Mike Ramsahai. The distribution of orbital periods P(T) increases from 120 to 2000 days Incomplete for longer periods Clear.
Depletion and excitation of the asteroid belt by migrating planets Kevin J. Walsh, Alessandro Morbidelli (SwRI,OCA-Nice) Sean N. Raymond (Obs. Bordeaux),
Chapter 15 The Formation of Planetary Systems
Planet Formation with Different Gas Depletion Timescales: Comparing with Observations Huigen Liu, Ji-lin Zhou, Su Wang Dept. of Astronomy.
 The outer planets are called Jovian or Jupiter- like.  These planets are made of gas and are several times more massive than the Earth.  The Jovian.
Planet Formation Topic: Formation of rocky planets from planetesimals Lecture by: C.P. Dullemond.
Dynamics of the young Solar system Kleomenis Tsiganis Dept. of Physics - A.U.Th. Collaborators: Alessandro Morbidelli (OCA) Hal Levison (SwRI) Rodney Gomes.
Chaos-assisted capture in the formation of Kuiper-belt binaries Sergey Astakhov UniqueICs, Saratov, Russia and NIC Forschungszentrum Jülich,Germany Ernestine.
The `Nice’ Model Öpik approximation Planet migration in a planetesimal disk The Nice model Consequences of the Nice Model: Epoch of Late Heavy Bombardment,
10Nov2006 Ge/Ay133 More on Jupiter, Neptune, the Kuiper belt, and the early solar system.
TERRESTRIAL PLANET FORMATION & THE FORMATION OF A WATER-RICH EARTH
Report from the Oort Cloud Simulations of the Formation of the Comet Reservoir Luke Dones Hal Levison Paul Weissman Martin Duncan.
Dynamics of Kuiper belt objects Yeh, Lun-Wen
Astronomy Pic of the Day. The Solar System Ingredients?
Trans-Neptunian Objects and Pluto Astronomy 311 Professor Lee Carkner Lecture 21.
The Outer Solar System Note the different scale of the inner and outer solar system. Note that Mercury and Pluto have the largest orbital inclinations.
Eccentric Extrasolar Planets: The Jumping Jupiter Model HD217107b as imagined by Lynette Cook Stacy Teng TERPS Conference Dec. 9, 2004.
2006 SQ 372 : A Planetary Interloper from the Inner Oort Cloud N. Kaib, A. Becker, L. Jones University of Washington.
The Size and Distance Scale Of The Solar System Our Earth is just one of several Planets that revolve around our Sun, the primary and central object of.
COMETS, KUIPER BELT AND SOLAR SYSTEM DYNAMICS Silvia Protopapa & Elias Roussos Lectures on “Origins of Solar Systems” February 13-15, 2006 Part I: Solar.
29 NOVEMBER 2007 CLASS #25 Astronomy 340 Fall 2007.
Lesson 8a Moons, Asteroids and Rings. Europa These interactions also keep Europa in a slight elliptical orbit as well. But since Europa is farther from.
A coherent and comprehensive model of the evolution of the outer solar system Alessandro Morbidelli (OCA, Nice) Collaborators: R. Gomes, H. Levison, K.
Mass Distribution and Planet Formation in the Solar Nebula Steve Desch School of Earth and Space Exploration Arizona State University Lunar and Planetary.
THE LATE HEAVY BOMBARDMENT AND THE FORMATION OF THE SOLAR SYSTEM
Outer Planets.  The outer planets are called Jovian or Jupiter- like.  Made of gas and are several times MORE massive than the Earth.  Grew to present.
Outer Solar System. Planets Outer solar system is dominated entirely by the four Jovian planets, but is populated by billions of small icy objects Giant.
Chapter 6.
Survey of the Solar System
Lecture 3 – Planetary Migration, the Moon, and the Late Heavy Bombardment Abiol 574.
Solar System. MILKY WAY 200 billion stars Diameter LY Height at center LY Solar System is LY from center.
I.Uranus and Neptune: Discoveries, atmospheres, interiors, rotation, magnetic fields, moons, rings, Uranus’ axis tilt and seasons. II.Pluto and Charon:
Chaotic Case Studies: Sensitive dependence on initial conditions in star/planet formation Fred C. Adams Physics Department University of Michigan With:
27 NOVEMBER 2007 CLASS #23 Astronomy 340 Fall 2007.
The law of orbits:  All planets move in elliptical orbits, with the sun at one focus.
Planets in Debris Disks Renu Malhotra University of Arizona Planet-Debris co-evolution Where can debris exist? Cases: Solar system, upsilon Andromedae,
Survey of the Solar System. Introduction The Solar System is occupied by a variety of objects, all maintaining order around the sun The Solar System is.
Completing the Inventory of the Outer Solar System Scott S. Sheppard Carnegie Institution of Washington Department of Terrestrial Magnetism.
Introductory Astronomy History – Solar Nebula 1. Dust to Planetesimals Grains of dust (solids) collide and adhere Larger grains grow to 10 9 planetesimals.
David Nesvorny David Vokrouhlicky (SwRI) Alessandro Morbidelli (CNRS) David Nesvorny David Vokrouhlicky (SwRI) Alessandro Morbidelli (CNRS) Capture of.
Cratering on Nix and Hydra William Bottke (SwRI).
Forming Earth and Our Solar System By David and Jake Thank You!
Angular Momentum in the Kuiper Belt Scott S. Sheppard Carnegie Institution of Washington Department of Terrestrial Magnetism.
Dynamics of comets and the origin of the solar system Origin of solar systems - 30/06/2009 Jean-Baptiste Vincent Max-Planck-Institut für Sonnensystemforschung.
in protoplanetary discs and OUTER SOLAR SYSTEM ARCHITECTURE
1B11 Foundations of Astronomy The Jovian Planets Silvia Zane, Liz Puchnarewicz
Trans-Neptunian Objects and Pluto Astronomy 311 Professor Lee Carkner Lecture 21.
The PSI Planet-building Code: Multi-zone, Multi-use S. J. Weidenschilling PSI Retreat August 20, 2007.
Late Work Due 12/20/13 Remember ain’t no butts about it! Sticking your head in the sand won’t make the deadlines go away 11 Days Remain.
The outer solar system: some points of physics A few points of physics I didn’t deal with earlier.
Neptune’s Resonances With Kuiper Belt Objects and What It Tells Us About the Early Solar System The Origin of Pluto’s Orbit: Implications for the Solar.
Chapter 13 Uranus and Neptune. Uranus was discovered in 1781 by Herschel; first planet to be discovered in more than 2000 years Little detail can be seen.
1 The Pluto System in the Context of Kuiper Belt Formation & Evolution A. Morbidelli (OCA – Nice)
ORIGIN OF THE LATE HEAVY BOMBARDMENT OF THE TERRESTRIAL PLANETS
New Views on the Lunar Late Heavy Bombardment
Cratering in the Solar System William Bottke Southwest Research Institute Boulder, Colorado.
Universe Tenth Edition Chapter 14 Uranus, Neptune, Pluto and the Kuiper Belt: Remote Worlds Roger Freedman Robert Geller William Kaufmann III.
Collision Enhancement due to Planetesimal Binary Formation Planetesimal Binary Formation Junko Kominami Jun Makino (Earth-Life-Science Institute, Tokyo.
THE SOLAR SYSTEM. BODIES IN THE SOLAR SYSTEM Our planet, Earth, is part of a system of planets that orbit a star, the sun. The solar system is comprised.
Terrestrial Planet Formation in Binary Star Systems ROSES Workshop 2005 February Jack J. Lissauer, NASA Ames Elisa V. Quintana, NASA Ames & Univ. Michigan.
Dynamical constraints on the nature of the Late Heavy Bombardment and models of its origin A.Morbidelli Observatoire de la Cote d’Azur, Nice, France.
Gas Planets. Vocabulary:  Gas Planet – a large planet that has a deep, massive atmosphere  Planetary Ring – a disk of matter that circles a planet and.
Formation of the Solar System Section 28.1 Modeling the Solar System This geocentric, or Earth-centered, model could not readily explain some aspects of.
Figure 4. Same as Fig. 3 but for x = 5.5.
Capture of Irregular Satellites during Planetary Encounters
Takashi Ito (CfCA/NAOJ, Tokyo) Renu Malhotra (LPL/U.Arizona)
Trojans and Co-Orbital Satellites Throughout the Solar System
Presentation transcript:

David Nesvorny (Southwest Research Institute) David Nesvorny (Southwest Research Institute) Capture of Irregular Satellites during Planetary Encounters Cassini image of Phoebe Cassini image of Phoebe

Irregular Satellites 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton)

Discovery Rate

Numbers & Sizes of Irregular Satellites Planet Number of known Irregular Satellites Smallest Detectable Radius (km) Jupiter551 Saturn352 Uranus95 Neptune615 To infer the numbers of irregular satellites at each planet the numbers of known satellites must be corrected for observational incompleteness To infer the numbers of irregular satellites at each planet the numbers of known satellites must be corrected for observational incompleteness

Corrected Size Distributions The numbers of irregular satellites present at individual planets may be SIMILAR. The numbers of irregular satellites present at individual planets may be SIMILAR. Jewitt & Sheppard

Irregular Satellites 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 1-km to 340-km diameters 1-km to 340-km diameters

Irregular Satellites 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 1-km to 340-km diameters 1-km to 340-km diameters Diversity of colors (neutral to reddish) Diversity of colors (neutral to reddish)

Colors of Irregular Satellites Observations show color diversity Observations show color diversity Colors range from neutral to reddish Colors range from neutral to reddish A hint of color gradient with heliocentric distance A hint of color gradient with heliocentric distance Neutral Neutral Reddish Reddish

Colors of Irregular Satellites Observations show color diversity Observations show color diversity Colors range from neutral to reddish Colors range from neutral to reddish A hint of color gradient with heliocentric distance A hint of color gradient with heliocentric distance

Irregular Satellites 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 1-km to 340-km diameters 1-km to 340-km diameters Diversity of colors (neutral to reddish) Diversity of colors (neutral to reddish) Irregular satellites have large, eccentric and predominantly retrograde orbits Irregular satellites have large, eccentric and predominantly retrograde orbits

Orbits of Irregular Satellites Retrograde Prograde

Irregular Satellites 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 104 known objects: 54 at Jupiter, 35 at Saturn, 9 at Uranus, 6 at Neptune (excluding Triton) 1-km to 340-km diameters 1-km to 340-km diameters Diversity of colors (neutral to reddish) Diversity of colors (neutral to reddish) Irregular satellites have large, eccentric and predominantly retrograde orbits Irregular satellites have large, eccentric and predominantly retrograde orbits Origin distinct from the one of regular moons (which formed by accretion in a circumplanetary disk) Origin distinct from the one of regular moons (which formed by accretion in a circumplanetary disk)

Origin of Irregular Satellites Capture from the circumsolar planetesimal disk (aerodynamic gas drag, planet’s growth and expansion of its Hill sphere, etc.) Capture from the circumsolar planetesimal disk (aerodynamic gas drag, planet’s growth and expansion of its Hill sphere, etc.) All have one important drawback: formed IR satellites are dynamically removed later when planets migrate in the planetesimal disk (e.g., Beauge et al. 2002) All have one important drawback: formed IR satellites are dynamically removed later when planets migrate in the planetesimal disk (e.g., Beauge et al. 2002) In the Nice model (planets migrate, Jupiter & Saturn cross 2:1, excited orbits of Uranus & Neptune stabilized by dynamical friction): any original populations of irregular satellites are removed during encounters between planets (Tsiganis et al. 2005) In the Nice model (planets migrate, Jupiter & Saturn cross 2:1, excited orbits of Uranus & Neptune stabilized by dynamical friction): any original populations of irregular satellites are removed during encounters between planets (Tsiganis et al. 2005)

New model for Capture We propose a new model: We propose a new model: ‘Irregular satellites were captured during planetary encounters when background planetesimals were deflected into bound orbits around planets as a result of 3-body gravitational interactions’ ‘Irregular satellites were captured during planetary encounters when background planetesimals were deflected into bound orbits around planets as a result of 3-body gravitational interactions’

Capture during Planetary Encounters Uranus Neptune Hill Sphere Numerous disk planetesimals

Capture during Planetary Encounters

Captured Irregular Satellites

Our Model We performed 50 new simulations of the Nice model, ~14 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~14 successful runs produced correct planetary orbits

Example simulations of Planet Migration Neptune Neptune Uranus Uranus Saturn Saturn Jupiter Jupiter

Capture during Planetary Encounters We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter

Encounter happens at ~23 AU Encounter happens at ~23 AU Excited orbits in the encounter zone: ~0.2, ~10 o Excited orbits in the encounter zone: ~0.2, ~10 o State of the planetesimal disk recorded at the last encounter in job #47

Capture during Planetary Encounters We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Typically several hundred planetary encounters Typically several hundred planetary encounters

In the #47 job: In the #47 job: 408 encounters between Uranus and Neptune 35 encounters between Saturn and Neptune 1-3 km/s encounter speeds Planetary encounters

Capture during Planetary Encounters We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Typically several hundred planetary encounters but not enough disk particles to record captures directly Typically several hundred planetary encounters but not enough disk particles to record captures directly

Capture during Planetary Encounters We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Typically several hundred planetary encounters but not enough disk particles to record captures directly Typically several hundred planetary encounters but not enough disk particles to record captures directly Bulirsch-Stoer integrations, 3 million objects (clones of original disk particles) were injected into the encounter zone at each recorded encounter Bulirsch-Stoer integrations, 3 million objects (clones of original disk particles) were injected into the encounter zone at each recorded encounter

Capture during Planetary Encounters We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits We performed 50 new simulations of the Nice model, ~20 successful runs produced correct planetary orbits Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Planetary orbits and state of the planetesimal disk were recorded during every planetary encounter Typically several hundred planetary encounters but not enough disk particles to record captures directly Typically several hundred planetary encounters but not enough disk particles to record captures directly Bulirsch-Stoer integrations, 3 million objects (clones of original disk particles) were injected into the encounter zone at each recorded encounter Bulirsch-Stoer integrations, 3 million objects (clones of original disk particles) were injected into the encounter zone at each recorded encounter Our model accounts for the encounter sequence where satellites are captured, removed or may switch between parent planets Our model accounts for the encounter sequence where satellites are captured, removed or may switch between parent planets

Number of Captured Satellites Generations of satellites captured during early planetary encounters do not contribute much to the final population Generations of satellites captured during early planetary encounters do not contribute much to the final population ~1368 stable satellites captured around Neptune in this experiment (out of 3 million test particles) ~1368 stable satellites captured around Neptune in this experiment (out of 3 million test particles) ~ capture probability per one particle in the disk ~ capture probability per one particle in the disk Uranus Neptune Uranus Neptune

Capture during Planetary Encounters

Good agreement between model and real orbits. Good agreement between model and real orbits. Orbit distributions of captured objects Satellites of Uranus Satellites of Neptune

Orbit distributions of captured objects Satellites of Jupiter Satellites of Saturn Good agreement between model and real orbits. Good agreement between model and real orbits.

35 Earth masses, Bernstein et al.’s SFD of present Kuiper belt, & our capture efficiency 35 Earth masses, Bernstein et al.’s SFD of present Kuiper belt, & our capture efficiency Planetary encounters produce more small irregular satellites than needed, their SFD slope is steep Planetary encounters produce more small irregular satellites than needed, their SFD slope is steep Indicates that the SFD of irregular satellites may have changed by collisional disruptions Indicates that the SFD of irregular satellites may have changed by collisional disruptions Comparison with SFD of known irregular moons

Conclusions Planetary encounters in the Nice model remove pre-existing irregular satellites and create large populations of the new ones Planetary encounters in the Nice model remove pre-existing irregular satellites and create large populations of the new ones The difference between model and real SFDs indicates that the SFDs of the irregular satellites changed by collisional disruptions The difference between model and real SFDs indicates that the SFDs of the irregular satellites changed by collisional disruptions Results consistent with spectroscopic observations of IR moons that show diverse colors Results consistent with spectroscopic observations of IR moons that show diverse colors

Captures via Exchange Reactions Observed large fraction of binaries in Kuiper Belt Observed large fraction of binaries in Kuiper Belt Exchange reactions suggested by Agnor & Hamilton (2006) as an attractive model to capture Neptune’s Triton Exchange reactions suggested by Agnor & Hamilton (2006) as an attractive model to capture Neptune’s Triton We have studied exchange reactions for irregular satellites via numerical simulations of the late phase of planet migration and via millions of scattering experiments We have studied exchange reactions for irregular satellites via numerical simulations of the late phase of planet migration and via millions of scattering experiments

Speeds typically a few km/s Speeds typically a few km/s To capture by exchange, orbit speed of the binary needs to be comparable or larger than the encounter speed To capture by exchange, orbit speed of the binary needs to be comparable or larger than the encounter speed Requires large, planetary-sized mass of the binary Requires large, planetary-sized mass of the binary Distribution of encounter speeds between planets and planetesimals

2 Mars-mass primary and several million encounter experiments 2 Mars-mass primary and several million encounter experiments We varied binary’s semimajor axis, inclination and orientation of its orbit relative to the target plane We varied binary’s semimajor axis, inclination and orientation of its orbit relative to the target plane Encounters taken from migration runs Encounters taken from migration runs Good capture efficiency but produced orbits have large e or small a Good capture efficiency but produced orbits have large e or small a Orbits of objects captured by exchange reactions

Exchange reactions during binary-planet encounters require a planetary-sized primary Exchange reactions during binary-planet encounters require a planetary-sized primary Captured objects have very large eccentricities and/or small semimajor axis values Captured objects have very large eccentricities and/or small semimajor axis values Requires additional mechanism that can expand captured orbits (at Neptune, captured and tidally-evolving Triton may scatter stuff around, Cuk & Gladman 2005 ) Requires additional mechanism that can expand captured orbits (at Neptune, captured and tidally-evolving Triton may scatter stuff around, Cuk & Gladman 2005 )Conclusions