69 research outputs found
The Formation of Ice Giants in a Packed Oligarchy: Instability and Aftermath
As many as 5 ice giants--Neptune-mass planets composed of 90% ice and rock
and 10% hydrogen--are thought to form at heliocentric distances of 10-25 AU on
closely packed orbits spaced ~5 Hill radii apart. Such oligarchies are
ultimately unstable. Once the parent disk of planetesimals is sufficiently
depleted, oligarchs perturb one another onto crossing orbits. We explore both
the onset and the outcome of the instability through numerical integrations,
including dynamical friction cooling of planets by a planetesimal disk whose
properties are held fixed. To trigger instability and the ejection of the first
ice giant in systems having an original surface density in oligarchs of Sigma ~
1 g/cm^2, the disk surface density s must fall below 0.1 g/cm^2. Ejections are
predominantly by Jupiter and occur within 10 Myr. To eject more than 1 oligarch
requires s < 0.03 g/cm^2. Systems starting with up to 4 oligarchs in addition
to Jupiter and Saturn can readily yield solar-system-like outcomes in which 2
surviving ice giants lie inside 30 AU and have their orbits circularized by
dynamical friction. Our numerical simulations support the idea that planetary
systems begin in more crowded and compact configurations, like those of
shear-dominated oligarchies. In contrast to previous studies, we identify s <
0.1 Sigma as the regime relevant for understanding the evolution of the outer
solar system, and we encourage future studies to concentrate on this regime
while relaxing our assumption of a fixed planetesimal disk.Comment: Accepted to ApJ Jan 27. Incorporates comments from the referee and
community at large. 15 pages, 14 figures, including 7 colo
Angular Momentum Transport in Particle and Fluid Disks
We examine the angular momentum transport properties of disks composed of
macroscopic particles whose velocity dispersions are externally enhanced
(``stirred''). Our simple Boltzmann equation model serves as an analogy for
unmagnetized fluid disks in which turbulence may be driven by thermal
convection. We show that interparticle collisions in particle disks play the
same role as fluctuating pressure forces and viscous dissipation in turbulent
disks: both transfer energy in random motions associated with one direction to
those associated with another, and convert kinetic energy into heat. The
direction of angular momentum transport in stirred particle and fluid disks is
determined by the direction of external stirring and by the properties of the
collision term in the Boltzmann equation (or its analogue in the fluid
problem). In particular, our model problem yields inward transport for
vertically or radially stirred disks, provided collisions are suitably
inelastic; the transport is outwards in the elastic limit. Numerical
simulations of hydrodynamic turbulence driven by thermal convection find inward
transport; this requires that fluctuating pressure forces do little to no work,
and is analogous to an externally stirred particle disk in which collisions are
highly inelastic.Comment: 15 pages; final version accepted by ApJ; minor changes, some
clarificatio
Particle Pile-ups and Planetesimal Formation
Solid particles in protoplanetary disks that are sufficiently super-solar in
metallicity overcome turbulence generated by vertical shear to gravitationally
condense into planetesimals. Super-solar metallicities result if solid
particles pile up as they migrate starward as a result of aerodynamic drag.
Previous analyses of aerodynamic drift rates that account for mean flow
differences between gas and particles yield particle pile-ups. We improve on
these studies not only by accounting for the collective inertia of solids
relative to that of gas, but also by including the transport of angular
momentum by turbulent stresses within the particle layer. These turbulent
stresses are derived in a physically self-consistent manner from the structure
of marginally Kelvin-Helmholtz turbulent flows. They are not calculated using
the usual plate drag formulae, whose use we explain is inappropriate.
Accounting for the relative inertia of solids to gas retards, but does not
prevent, particle pile-ups, and generates more spatially extended regions of
metal enrichment. Turbulent transport hastens pile-ups. We conclude that
particle pile-up is a robust outcome in sufficiently passive protoplanetary
disks. Connections to observations of circumstellar disks, including the Kuiper
Belt, and the architectures of planetary systems are made.Comment: Final revised version, accepted to ApJ. Error corrected in density
dependence of Epstein drift rate; correction caused quantitative changes,
particularly in high particle density limit. Qualitative conclusion that
particle pile-ups can trigger planetesimal formation within protostellar disk
lifetime is unaffecte
Three-Dimensional Dynamics of Narrow Planetary Rings
Narrow planetary rings are eccentric and inclined. Particles within a given
ring must therefore share the same pericenter and node. We solve for the
three-dimensional geometries and mass distributions that enable the Uranian
Alpha and Beta rings, and the Saturnian Maxwell and Colombo (Titan) rings, to
maintain simultaneous apsidal and nodal lock. Ring self-gravity, interparticle
collisions, and the quadrupole field of the host planet balance each other to
achieve this equilibrium. We prove that such an equilibrium is linearly stable.
Predictions for the Saturnian ringlets to be tested by the Cassini spacecraft
include: (1) ringlet masses are of order 1e19 g, (2) surface mass densities
should increase from ring midline to ring edges, and (3) rings are vertically
warped such that the fractional variation of inclination across the ring is of
order 10%. Analogous predictions are made for the Uranian rings. Simultaneous
apsidal and nodal locking forces the narrowest portion of the ring--its
``pinch,'' where self-gravitational and collisional forces are strongest--to
circulate relative to the node, and introduces previously unrecognized
time-varying forces perpendicular to the planet's equator plane. We speculate
that such periodic stressing might drive kilometer-scale bending waves at a
frequency twice that of apsidal precession. Such flexing might be observed over
a few weeks by Cassini.Comment: Final revised version, ApJ, in pres
The Circumbinary Ring of KH 15D
The light curves of the pre-main-sequence star KH 15D from the years
1913--2003 can be understood if the star is a member of an eccentric binary
that is encircled by a vertically thin, inclined ring of dusty gas. Eclipses
occur whenever the reflex motion of a star carries it behind the circumbinary
ring; the eclipses occur with period equal to the binary orbital period of 48.4
days. Features of the light curve--including the amplitude of central reversals
during mid-eclipse, the phase of eclipse with respect to the binary orbit
phase, the level of brightness out-of-eclipse, the depth of eclipse, and the
eclipse duty cycle--are all modulated on the timescale of nodal regression of
the obscuring ring, in accord with the historical data. The ring has a mean
radius near 3 AU and a radial width that is likely less than this value. While
the inner boundary could be shepherded by the central binary, the outer
boundary may require an exterior planet to confine it against viscous
spreading. The ring must be vertically warped to maintain a non-zero
inclination. Thermal pressure gradients and/or ring self-gravity can readily
enforce rigid precession. In coming years, as the node of the ring regresses
out of our line-of-sight toward the binary, the light curve from the system
should cycle approximately back through its previous behavior. Near-term
observations should seek to detect a mid-infrared excess from this system; we
estimate the flux densities from the ring to be 3 mJy at wavelengths of 10--100
microns.Comment: Final version, ApJ, v607, 913 (June 1); includes prediction for full
spectral energy distribution (new Figure 5
Brownian Motion in Planetary Migration
A residual planetesimal disk of mass 10-100 Earth masses remained in the outer solar system following the birth of the giant planets, as implied by the existence of the Oort cloud, coagulation requirements for Pluto, and inefficiencies in planet formation. Upon gravitationally scattering planetesimal debris, planets migrate. Orbital migration can lead to resonance capture, as evidenced here in the Kuiper and asteroid belts, and abroad in extra-solar systems. Finite sizes of planetesimals render migration stochastic ("noisy"). At fixed disk mass, larger (fewer) planetesimals generate more noise. Extreme noise defeats resonance capture. We employ order-of-magnitude physics to construct an analytic theory for how a planet's orbital semi-major axis fluctuates in response to random planetesimal scatterings. To retain a body in resonance, the planet's semi-major axis must not random walk a distance greater than the resonant libration width. We translate this criterion into an analytic formula for the retention efficiency of the resonance as a function of system parameters, including planetesimal size. We verify our results with tailored numerical simulations. Application of our theory reveals that capture of Resonant Kuiper belt objects by a migrating Neptune remains effective if the bulk of the primordial disk was locked in bodies having sizes 1000 km was less than a few percent. Coagulation simulations produce a size distribution of primordial planetesimals that easily satisfies these constraints. We conclude that stochasticity did not interfere with, nor modify in any substantive way, Neptune's ability to capture and retain Resonant Kuiper belt objects during its migration
Binaries in the Kuiper Belt
Binaries have played a crucial role many times in the history of modern
astronomy and are doing so again in the rapidly evolving exploration of the
Kuiper Belt. The large fraction of transneptunian objects that are binary or
multiple, 48 such systems are now known, has been an unanticipated windfall.
Separations and relative magnitudes measured in discovery images give important
information on the statistical properties of the binary population that can be
related to competing models of binary formation. Orbits, derived for 13
systems, provide a determination of the system mass. Masses can be used to
derive densities and albedos when an independent size measurement is available.
Angular momenta and relative sizes of the majority of binaries are consistent
with formation by dynamical capture. The small satellites of the largest
transneptunian objects, in contrast, are more likely formed from collisions.
Correlations of the fraction of binaries with different dynamical populations
or with other physical variables have the potential to constrain models of the
origin and evolution of the transneptunian population as a whole. Other means
of studying binaries have only begun to be exploited, including lightcurve,
color, and spectral data. Because of the several channels for obtaining unique
physical information, it is already clear that binaries will emerge as one of
the most useful tools for unraveling the many complexities of transneptunian
space.Comment: Accepted for inclusion in "The Kuiper Belt", University of Arizona
Press, Space Science Series Corrected references in Table
Dust Dynamics, Surface Brightness Profiles, and Thermal Spectra of Debris Disks: The Case of AU Mic
AU Microscopii is a 12 Myr old M dwarf that harbors an optically thin,
edge-on disk of dust. The scattered light surface brightness falls with
projected distance b from the star as b^-a; within b = 43 AU, a = 1-2, while
outside 43 AU, a = 4-5. We devise a theory to explain this profile. At a
stellocentric distance r = r_BR = 43 AU, we posit a ring of parent bodies on
circular orbits: the "birth ring," wherein micron-sized grains are born from
the collisional attrition of parent bodies. The "inner disk" at r < r_BR
contains grains that migrate inward by corpuscular and Poynting-Robertson (CPR)
drag. The "outer disk" at r > r_BR comprises grains just large enough to remain
bound to the star, on orbits rendered highly eccentric by stellar wind and
radiation pressure. How the vertical optical depth tau scales with r depends on
the fraction of grains that migrate inward by CPR drag without suffering a
collision. If this fraction is large, the inner disk and birth ring share the
same optical depth, and tau scales as r^-5/2 in the outer disk. By contrast,
under collision-dominated conditions, the inner disk is empty, and tau scales
as r^-3/2 outside. These scaling relations, which we derive analytically and
confirm numerically, are robust against uncertainties in the grain size
distribution. By simultaneously modeling the surface brightness and thermal
spectrum, we break model degeneracies to establish that the AU Mic system is
collision-dominated, and that its narrow birth ring contains a lunar mass of
decimeter-sized bodies. The inner disk is devoid of micron-sized grains; the
surface brightness at b < 43 AU arises from light forward scattered by the
birth ring. Inside b = 43 AU, the disk's V-H color should not vary with b;
outside, the disk must become bluer as ever smaller grains are probed.Comment: Final proofed version to be published in ApJ; no significant changes
from version
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