601 research outputs found
Critical core mass for enriched envelopes: the role of H2O condensation
Context. Within the core accretion scenario of planetary formation, most
simulations performed so far always assume the accreting envelope to have a
solar composition. From the study of meteorite showers on Earth and numerical
simulations, we know that planetesimals must undergo thermal ablation and
disruption when crossing a protoplanetary envelope. Once the protoplanet has
acquired an atmosphere, the primordial envelope gets enriched in volatiles and
silicates from the planetesimals. This change of envelope composition during
the formation can have a significant effect in the final atmospheric
composition and on the formation timescale of giant planets.
Aims. To investigate the physical implications of considering the envelope
enrichment of protoplanets due to the disruption of icy planetesimals during
their way to the core. Particular focus is placed on the effect on the critical
core mass for envelopes where condensation of water can occur.
Methods. Internal structure models are numerically solved with the
implementation of updated opacities for all ranges of metallicities and the
software CEA to compute the equation of state. CEA computes the chemical
equilibrium for an arbitrary mixture of gases and allows the condensation of
some species, including water. This means that the latent heat of phase
transitions is consistently incorporated in the total energy budget.
Results. The critical core mass is found to decrease significantly when an
enriched envelope composition is considered in the internal structure
equations. A particular strong reduction of the critical core mass is obtained
for planets whose envelope metallicity is larger than Z=0.45 when the outer
boundary conditions are suitable for condensation of water to occur in the top
layers of the atmosphere. We show that this effect is qualitatively preserved
when the atmosphere is out of chemical equilibrium.Comment: Accepted for publication in A&
Did Fomalhaut, HR 8799, and HL Tauri Form Planets via the Gravitational Instability? Placing Limits on the Required Disk Masses
Disk fragmentation resulting from the gravitational instability has been
proposed as an efficient mechanism for forming giant planets. We use the planet
Fomalhaut b, the triple-planetary system HR 8799, and the potential protoplanet
associated with HL Tau to test the viability of this mechanism. We choose the
above systems since they harbor planets with masses and orbital characteristics
favored by the fragmentation mechanism. We do not claim that these planets must
have formed as the result of fragmentation, rather the reverse: if planets can
form from disk fragmentation, then these systems are consistent with what we
should expect to see. We use the orbital characteristics of these recently
discovered planets, along with a new technique to more accurately determine the
disk cooling times, to place both lower and upper limits on the disk surface
density--and thus mass--required to form these objects by disk fragmentation.
Our cooling times are over an order of magnitude shorter than those of Rafikov
(2005),which makes disk fragmentation more feasible for these objects. We find
that the required mass interior to the planet's orbital radius is ~0.1 Msun for
Fomalhaut b, the protoplanet orbiting HL Tau, and the outermost planet of HR
8799. The two inner planets of HR 8799 probably could not have formed in situ
by disk fragmentation.Comment: 5 pages, 1 figure, accepted for publication in ApJ
TRPV1-expressing primary afferents generate behavioral responses to pruritogens via multiple mechanisms
The mechanisms that generate itch are poorly understood at both the molecular and cellular levels despite its clinical importance. To explore the peripheral neuronal mechanisms underlying itch, we assessed the behavioral responses (scratching) produced by s.c. injection of various pruritogens in PLCβ3- or TRPV1-deficient mice. We provide evidence that at least 3 different molecular pathways contribute to the transduction of itch responses to different pruritogens: 1) histamine requires the function of both PLCβ3 and the TRPV1 channel; 2) serotonin, or a selective agonist, α-methyl-serotonin (α-Me-5-HT), requires the presence of PLCβ3 but not TRPV1, and 3) endothelin-1 (ET-1) does not require either PLCβ3 or TRPV1. To determine whether the activity of these molecules is represented in a particular subpopulation of sensory neurons, we examined the behavioral consequences of selectively eliminating 2 nonoverlapping subsets of nociceptors. The genetic ablation of MrgprD^+ neurons that represent ≈90% of cutaneous nonpeptidergic neurons did not affect the scratching responses to a number of pruritogens. In contrast, chemical ablation of the central branch of TRPV1+ nociceptors led to a significant behavioral deficit for pruritogens, including α-Me-5-HT and ET-1, that is, the TRPV1-expressing nociceptor was required, whether or not TRPV1 itself was essential. Thus, TRPV1 neurons are equipped with multiple signaling mechanisms that respond to different pruritogens. Some of these require TRPV1 function; others use alternate signal transduction pathways
Near-infrared transit photometry of the exoplanet HD 149026b
The transiting exoplanet HD 149026b is an important case for theories of
planet formation and planetary structure, because the planet's relatively small
size has been interpreted as evidence for a highly metal-enriched composition.
We present observations of 4 transits with the Near Infrared Camera and
Multi-Object Spectrometer on the Hubble Space Telescope, within a wavelength
range of 1.1--2.0 m. Analysis of the light curve gives the most precise
estimate yet of the stellar mean density, g cm. By requiring agreement between the
observed stellar properties (including ) and stellar evolutionary
models, we refine the estimate of the stellar radius: R_\sun. We also find a deeper transit than has been
measured at optical and mid-infrared wavelengths. Taken together, these
findings imply a planetary radius of , which is larger than earlier estimates. Models of the planetary interior
still require a metal-enriched composition, although the required degree of
metal enrichment is reduced. It is also possible that the deeper NICMOS transit
is caused by wavelength-dependent absorption by constituents in the planet's
atmosphere, although simple model atmospheres do not predict this effect to be
strong enough to account for the discrepancy. We use the 4 newly-measured
transit times to compute a refined transit ephemeris.Comment: 18 pages, 13 figures, accepted for publication in Ap
The Heavy Element Composition of Disk Instability Planets Can Range From Sub- to Super-Nebular
Transit surveys combined with Doppler data have revealed a class of gas giant
planets that are massive and highly enriched in heavy elements (e.g.,
HD149026b, GJ436b, and HAT-P-20b). It is tempting to consider these planets as
validation of core accretion plus gas capture because it is often assumed that
disk instability planets should be of nebular composition. We show in this
paper, to the contrary, that gas giants that form by disk instability can have
a variety of heavy element compositions, ranging from sub- to super-nebular
values. High levels of enrichment can be achieved through one or multiple
mechanisms, including enrichment at birth, planetesimal capture, and
differentiation plus tidal stripping. As a result, the metallicity of an
individual gas giant cannot be used to discriminate between gas giant formation
modes.Comment: Accepted by Ap
On the Origin of HD149026b
The high density of the close-in extrasolar planet HD149026b suggests the
presence of a huge core in the planet, which challenges planet formation
theory. We first derive constraints on the amount of heavy elements and
hydrogen/helium present in the planet: We find that preferred values of the
core mass are between 50 and 80 M_E. We then investigate the possibility of
subcritical core accretion as envisioned for Uranus and Neptune and find that
the subcritical accretion scenario is unlikely in the case of HD149026b for at
least two reasons: (i) Subcritical planets are such that the ratio of their
core mass to their total mass is above ~0.7, in contradiction with constraints
for all but the most extreme interior models of HD149026b; (ii) High accretion
rates and large isolation mass required for the formation of a subcritical core
of 30 M_E are possible only at specific orbital distances in a disk with a
surface density of dust equal to at least 10 times that of the minimum mass
solar nebula. This value climbs to 30 when considering a 50 M_E core. These
facts point toward two main routes for the formation of this planet: (i) Gas
accretion that is limited by a slow viscous inflow of gas in an evaporating
disk; (ii) A significant modification of the composition of the planet after as
accretion has stopped. These two routes are not mutually exclusive.
Illustrating the second route, we show that for a wide range of impact
parameters, giant impacts lead to a loss of the gas component of the planet and
thus may lead to planets that are highly enriched in heavy elements. In the
giant impact scenario, we expect an outer giant planet to be present.
Observational studies by imaging, astrometry and long term interferometry of
this system are needed to better narrow down the ensemble of possibilities.Comment: 29 pages, 8 figures, to appear in the 10 October 2006 issue of Ap
ESPRESSO Mass determination of TOI-263b: An extreme inhabitant of the brown dwarf desert
The TESS mission has reported a wealth of new planetary systems around bright
and nearby stars amenable for detailed characterization of the planet
properties and their atmospheres. However, not all interesting TESS planets
orbit around bright host stars. TOI-263b is a validated ultra-short period
substellar object in a 0.56-day orbit around a faint (V=18.97) M3.5 dwarf star.
The substellar nature of TOI-263b was explored using multi-color photometry,
which determined a true radius of 0.87+-0.21 Rj, establishing TOI-263b's nature
ranging from an inflated Neptune to a brown dwarf. The orbital period-radius
parameter space occupied by TOI-263b is quite unique, which prompted a further
characterization of its true nature. Here, we report radial velocity
measurements of TOI-263 obtained with 3 VLT units and the ESPRESSO spectrograph
to retrieve the mass of TOI-263b. We find that TOI-263b is a brown dwarf with a
mass of 61.6+-4.0 Mj. Additionally, the orbital period of the brown dwarf is
found to be synchronized with the rotation period of the host star, and the
system is found to be relatively active, possibly revealing a star--brown dwarf
interaction. All these findings suggest that the system's formation history
might be explained via disc fragmentation and later migration to close-in
orbits. If the system is found to be unstable, TOI-263 is an excellent target
to test the migration mechanisms before the brown dwarf becomes engulfed by its
parent star.Comment: Accepted for Publication in Astronomy and Astrophysic
Have proto-planetary discs formed planets?
It has recently been noted that many discs around T Tauri stars appear to
comprise only a few Jupiter-masses of gas and dust. Using millimetre surveys of
discs within six local star-formation regions, we confirm this result, and find
that only a few percent of young stars have enough circumstellar material to
build gas giant planets, in standard core accretion models. Since the frequency
of observed exo-planets is greater than this, there is a `missing mass'
problem. As alternatives to simply adjusting the conversion of dust-flux to
disc mass, we investigate three other classes of solution. Migration of planets
could hypothetically sweep up the disc mass reservoir more efficiently, but
trends in multi-planet systems do not support such a model, and theoretical
models suggest that the gas accretion timescale is too short for migration to
sweep the disc. Enhanced inner-disc mass reservoirs are possible, agreeing with
predictions of disc evolution through self-gravity, but not adding to
millimetre dust-flux as the inner disc is optically thick. Finally, the
incidence of massive discs is shown to be higher at the {\it proto}stellar
stages, Classes 0 and I, where discs substantial enough to form planets via
core accretion are abundant enough to match the frequency of exo-planets.
Gravitational instability may also operate in the Class 0 epoch, where half the
objects have potentially unstable discs of \ga30 % of the stellar mass.
However, recent calculations indicate that forming gas giants inside 50 AU by
instability is unlikely, even in such massive discs. Overall, the results
presented suggest that the canonically 'proto-planetary' discs of Class II T
Tauri stars {\bf have globally low masses in dust observable at millimetre
wavelengths, and conversion to larger bodies (anywhere from small rocks up to
planetary cores) must already have occurred.}Comment: Accepted for publication in MNRAS (main journal
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