Showing papers by "Alan P. Boss published in 2007"

A reappraisal of the habitability of planets around M dwarf stars.

Abstract: Stable, hydrogen-burning, M dwarf stars make up about 75% of all stars in the Galaxy. They are extremely long-lived, and because they are much smaller in mass than the Sun (between 0.5 and 0.08 MSun), their temperature and stellar luminosity are low and peaked in the red. We have re-examined what is known at present about the potential for a terrestrial planet forming within, or migrating into, the classic liquid–surface–water habitable zone close to an M dwarf star. Observations of protoplanetary disks suggest that planet-building materials are common around M dwarfs, but N-body simulations differ in their estimations of the likelihood of potentially habitable, wet planets that reside within their habitable zones, which are only about one-fifth to 1/50th of the width of that for a G star. Particularly in light of the claimed detection of the planets with masses as small as 5.5 and 7.5 MEarth orbiting M stars, there seems no reason to exclude the possibility of terrestrial planets. Tidally locked synchron...

Testing Disk Instability Models for Giant Planet Formation

Abstract: Disk instability is an attractive yet controversial means for the rapid formation of giant planets in our solar system and elsewhere. Recent concerns regarding the first adiabatic exponent of molecular hydrogen gas are addressed and shown not to lead to spurious clump formation in the author's disk instability models. A number of disk instability models have been calculated in order to further test the robustness of the mechanism, exploring the effects of changing the pressure equation of state, the vertical temperature profile, and other parameters affecting the temperature distribution. Possible reasons for differences in results obtained by other workers are discussed. Disk instability remains as a plausible formation mechanism for giant planets.

Gravitational Instabilities in Gaseous Protoplanetary Disks and Implications for Giant Planet Formation

Abstract: Protoplanetary gas disks are likely to experience gravitational instabilites (GI’s) during some phase of their evolution. Density perturbations in an unstable disk grow on a dynamic time scale into spiral arms that produce efficient outward transfer of angular momentum and inward transfer of mass through gravitational torques. In a cool disk with rapid enough cooling, the spiral arms in an unstable disk form self-gravitating clumps. Whether gas giant protoplanets can form by such a disk instability process is the primary question addressed by this review. We discuss the wide range of calculations undertaken by ourselves and others using various numerical techniques, and we report preliminary results from a large multi-code collaboration. Additional topics include – triggering mechanisms for GI’s, disk heating and cooling, orbital survival of dense clumps, interactions of solids with GI-driven waves and shocks, and hybrid scenarios where GI’s facilitate core accretion. The review ends with a discussion of how well disk instability and core accretion fare in meeting observational constraints.

Evolution of the solar nebula. VIII. Spatial and temporal heterogeneity of short-lived radioisotopes and stable oxygen isotopes

Abstract: Isotopic abundances of short-lived radionuclides such as 26Al provide the most precise chronometers of events in the early solar system, provided that they were initially homogeneously distributed. On the other hand, the abundances of the three stable isotopes of oxygen in primitive meteorites show a mass-independent fractionation that survived homogenization in the solar nebula. As a result of this and other cosmochemical evidence, the degree of spatial heterogeneity of isotopes in the solar nebula has long been a puzzle. We show here that based on hydrodynamic models of the mixing and transport of isotopic anomalies formed at, or injected onto, the surface of the solar nebula, initially high levels of isotopic spatial heterogeneity are expected to fall to steady state levels (~10%) low enough to validate the use of 26Al for chronometry, but high enough to preserve the evidence for mass-independent fractionation of oxygen isotopes. The solution to this puzzle relies on the mixing being accomplished by the chaotic fluid motions in a marginally gravitationally unstable disk, as seems to be required for the formation of gas giant planets, and by the inability of alternative physical processes to drive large-scale mixing and transport in the planet-forming midplane of the solar nebula. Such a disk is also capable of large-scale outward transport of the thermally annealed dust grains found in comets, and of driving the shock fronts that appear to be responsible for much of the thermal processing of the components of primitive meteorites, creating a self-consistent picture of the basic physical processes shaping the early solar nebula.

Testing Disk Instability Models for Giant Planet Formation

Abstract: Disk instability is an attractive yet controversial means for the rapid formation of giant planets in our solar system and elsewhere. Recent concerns regarding the first adiabatic exponent of molecular hydrogen gas are addressed and shown not to lead to spurious clump formation in the author's disk instability models. A number of disk instability models have been calculated in order to further test the robustness of the mechanism, exploring the effects of changing the pressure equation of state, the vertical temperature profile, and other parameters affecting the temperature distribution. Possible reasons for differences in results obtained by other workers are discussed. Disk instability remains as a plausible formation mechanism for giant planets.

Signatures of Planet Formation in Gravitationally Unstable Disks

Abstract: In this Letter, we calculate simulated scattered light images of a circumstellar disk in which a planet is forming by gravitational instability. The simulated images bear no correlation to the vertically integrated surface density of the disk, but rather trace the density structure in the tenuous upper layers of the disk. Although the density at high altitudes does not bear a direct relation to activity at the midplane, the very existence of structure at high altitudes along with high time variability is an indicator of gravitational instability within the disk. The timescale for variations is much shorter than the orbital period of the planet, which facilitates observation of the phenomenon. Scattered light images may not necessarily be able to tell us where exactly a planet might be forming in a disk but can still be a useful probe of active planet formation within a circumstellar disk. Although these phenomena are unlikely to be observable by current telescopes, future large telescopes, such as the Giant Magellan Telescope, may be able to detect them.

Astronomical and Meteoritic Evidence for the Nature of Interstellar Dust and Its Processing in Protoplanetary Disks

Abstract: Here we compare the astronomical and meteoritic evidence for the nature and origin of interstellar dust, and how it is processed in protoplanetary disks. The relative abundances of circumstellar grains in meteorites and interplanetary dust particles (IDPs) are broadly consistent with most astronomical estimates of Galactic dust production, although graphite/amorphous C is highly underabundant. The major carbonaceous component in meteorites and IDPs is an insoluble organic material (IOM) that probably formed in the interstellar medium, but a solar origin cannot be ruled out. GEMS (glass with embedded metal and sulfide) that are isotopically solar within error are the best candidates for interstellar silicates, but it is also possible that they are Solar System condensates. No dust from young stellar objects has been identified in IDPs, but it is difficult to differentiate them from Solar System material or indeed some circumstellar condensates. The crystalline silicates in IDPs are mostly solar condensates, with lesser amounts of annealed GEMS. The IOM abundances in IDPs are roughly consistent with the degree of processing indicated by their crystallinity if the processed material was ISM dust. The IOM contents of meteorites are much lower suggesting that there was a gradient in dust processing in the Solar System. The microstructure of much of the pyroxene in IDPs suggests that it formed at temperatures >1258 K and cooled relatively rapidly (~1000 K/hr). This cooling rate favors shock heating rather than radial transport of material annealed in the hot inner disk as the mechanism for producing crystalline dust in comets and IDPs. Shock heating is also a likely mechanism for producing chondrules in meteorites, but the dust was probably heated at a different time and/or location to chondrules.

Collapse and fragmentation of molecular cloud cores. IX. Magnetic braking of initially filamentary clouds

Abstract: The collapse and fragmentation of initially filamentary, magnetic molecular clouds are calculated in three dimensions with a gravitational, radiative hydrodynamics code. The code includes magnetic field effects in an approximate manner: magnetic pressure, tension, braking, and ambipolar diffusion are all modeled. The parameters varied are the ratio of the ambipolar diffusion time to the free-fall time at the center of the filamentary cloud (tad/tff = 10, 20, or 106 ~ ∞), the cloud's reference magnetic field strength (Boi = 0, 200, or 300 μG—the latter two values leading to magnetically subcritical clouds), the ratio of rotational to gravitational energy of the filament (10-4 or 10-2), and the efficiency of magnetic braking (represented by a factor fmb = 0, 10-4, or 10-3). Three types of outcomes are observed: direct collapse and fragmentation into a multiple protostar system (models with Boi = 0), periodic contraction and expansion without collapse (models with tad/tff = 106), or periodic contraction and expansion leading eventually to collapse on a timescale of ~6tff-12tff (all other models). Because the computational grid is a finite-volume sphere, the expanding clouds bounce off the spherical boundary and recollapse toward the center of the spherical grid, leading to the periodic formation of shocked regions where the infalling gas collides with itself, forming dense layers susceptible to sustained collapse and eventual fragmentation. The models develop weakly supersonic velocity fields as a result of rebounding prior to collapse. The models show that magnetically supported clouds subject to magnetic braking can undergo dynamic collapse leading to protostellar fragmentation on scales of 10-100 AU, consistent with typical binary star separations.

Gravitational instability in binary protoplanetary disks

Abstract: We review the models and results of simulations of self-gravitating, gaseous protoplanetary disks in binary star systems. These models have been calculated by three different groups with three different computational methods, two particle-based and one grid-based. We show that interactions with the companion star can affect the temperature distribution and structural evolution of disks, and discuss the implications for giant planet formation by gravitational instability as well as by core accretion. Complete consensus has not been reached yet on whether the formation of giant planets is promoted or suppressed by tidal interactions with a companion star. While systems with binary separations of order 100 AU or larger appear to behave more or less as in isolation, systems with smaller separations exhibit an increased or decreased susceptibility to fragmentation, depending on the details of thermodynamics, in particular on the inclusion or absence of artificial viscosity, and on the initial conditions. While code comparisons on identical problems need to be carried out (some of which are already in progress) to decide which computer models are more realistic, it is already clear that relatively close binary systems, with separations of order 60 AU or less, should provide strong constraints on how giant planets form in these systems.

An m sin i = 24 Earth Mass Planetary Companion To The Nearby M Dwarf GJ 176

Abstract: We report the detection of a planetary companion with a minimum mass of m sin i = 0.0771 M_Jup = 24.5 M_Earth to the nearby (d = 9.4 pc) M2.5V star GJ 176. The star was observed as part of our M dwarf planet search at the Hobby-Eberly Telescope (HET). The detection is based on 5 years of high-precision differential radial velocity (RV) measurements using the High-Resolution-Spectrograph (HRS). The orbital period of the planet is 10.24 d. GJ 176 thus joins the small (but increasing) sample of M dwarfs hosting short-periodic planets with minimum masses in the Neptune-mass range. Low mass planets could be relatively common around M dwarfs and the current detections might represent the tip of a rocky planet population.

Observational tests of planet formation models

Abstract: We summarize the results of two experiments to address important issues related to the correlation between planet frequencies and properties and the metallicity of the hosts. Our results can usefully inform formation, structural, and evolutionary models of gas giant planets.

Observational Tests of Planet Formation Models

Abstract: We summarize the results of two experiments to address important issues related to the correlation between planet frequencies and properties and the metallicity of the hosts. Our results can usefully inform formation, structural, and evolutionary models of gas giant planets.

Collapse and Fragmentation of Molecular Cloud Cores. IX. Magnetic Braking of Initially Filamentary Clouds

Abstract: The collapse and fragmentation of initially filamentary, magnetic molecular clouds is calculated in three dimensions with a gravitational, radiative hydrodynamics code. The code includes magnetic field effects in an approximate manner: magnetic pressure, tension, braking, and ambipolar diffusion are all modelled. Three types of outcomes are observed: direct collapse and fragmentation into a multiple protostar system, periodic contraction and expansion without collapse, or periodic contraction and expansion leading eventually to collapse. While the models begin their evolution at rest except for the assumed solid-body rotation, they develop weakly supersonic velocity fields as a result of the rebounding prior to collapse. The models show that magnetically-supported clouds subject to magnetic braking can undergo dynamic collapse leading to protostellar fragmentation on scales of 10 AU to 100 AU, consistent with typical binary star separations.