Kuiper Belt Dynamics and Interactions

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Kuiper Belt Dynamics and Interactions Minor Planet Center Ruth Murray-Clay Harvard-Smithsonian Center for Astrophysics

Kuiper belt µm ejected by radiation pressure larger grains migrate in via PR drag until they are destroyed by collisions Migrating grains interact dynamically with the planets. Larger grains move slower.

Dynamical structure of the Kuiper belt mean-motion resonances low eccentricity, low inclination population regions of instability large inclinations Deep Ecliptic Survey; Chiang, Lithwick, Murray-Clay et al., PPV

Ruth Murray-Clay: Kuiper Belt Dynamics and Interactions Mean-motion resonances provide stability Pluto is protected from encounters with Neptune by the 3:2 mean-motion resonance 40 y (AU) 20 0 ï20 ï40 ï40 ï20 0 20 x (AU) 40

Observed resonant KBOs cross the orbit of Neptune but avoid its angular location Minor Planet Center

Migration results from scattering planetesimals Fernandez and Ip 1984; Malhotra 1993, 1995; Gomes et al. 2004 Oort cloud, Ejection Sun Jupiter Neptune back-reaction from each scattering kicks the planet a small amount global asymmetries in angular momentum transfer cause migration

Outward migration of Neptune can produce resonant capture Malhotra 1995; Chiang et al. 2003 Deep Ecliptic Survey; Chiang, Lithwick, Murray-Clay et al., PPV

Net torque during encounter Ruth Murray-Clay: Kuiper Belt Dynamics and Interactions Resonant Capture No net torque during encounter Eccentricity excitation: perturbation pattern speed not equal to orbital speed

Kuiper belt Ruth Murray-Clay: Kuiper Belt Dynamics and Interactions Dust feels extra forces µm ejected by radiation pressure larger grains migrate in via PR drag until they are destroyed by collisions Migrating grains interact dynamically with the planets. Larger grains move slower and are easier to capture into resonance and destroy by collisions.

Example outcome for the Kuiper belt Kuchner & Stark, in prep. azimuthal distribution of dust radial distribution optical emission

What can we do with a view from 5 AU? 1) Test our basic theoretical understanding of dust dynamics in debris disks. Kuchner & Stark, in prep. optical non-axisymmetric distribution sub-mm longer wavelengths trace source population

Understanding these properties is essential for probing extrasolar planets Fomalhaut Kalas et al. 2008 debris disk interaction has been used to constrain the mass of a wide-separation planet Kuchner & Stark, in prep. In more massive disks, dust collides before it migrates in from the source population.

What can we do with a view from 5 AU? 2) Constrain theories of Kuiper belt formation by looking at variations in dust properties with inclination. Low inclination Plutinos are distinct (as are low-inclination classicals) Resonant capture via migration does not change inclinations. Eccentricities and inclinations in resonance are not correlated. Resonant capture requires generating the two populations first. Almeida et al. 2009 Test if color difference is from collision rate.

Nice model capture of resonant KBOs Population as Neptune s eccentricity is damped (plus a little migration). Nice model Observations Levison et al. 2008

What can we do with a view from 5 AU? 3) Constrain how well we can use KBOs as collisionless test particles. For example, a break in the size distribution due to present-day collisions could lead to different resonant populations of large and small bodies. Bernstein et al. 2004

Kuiper belt dynamics and interactions: What can we do with a view from 5 AU? Measure the azimuthal distribution of dust to test our basic understanding of dust dynamics in debris disks. Look for differences in dust production rates and spectra with inclination distribution to test Kuiper belt formation scenarios. Constrain current collision rates and match to the size distribution and to dynamics of mid-sized bodies.