3,882 research outputs found
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Infrared spectroscopy of chondrites and their components: a link between meteoritics and astronomy?
Mantle formation, coagulation and the origin of cloud/core-shine: II. Comparison with observations
Many dense interstellar clouds are observable in emission in the near-IR,
commonly referred to as "Cloudshine", and in the mid-IR, the so-called
"Coreshine". These C-shine observations have usually been explained with grain
growth but no model has yet been able to self-consistently explain the dust
spectral energy distribution from the near-IR to the submm. We want to
demonstrate the ability of our new core/mantle evolutionary dust model THEMIS
(The Heterogeneous dust Evolution Model at the IaS), which has been shown to be
valid in the far-IR and submm, to reproduce the C-shine observations. Our
starting point is a physically motivated core/mantle dust model. It consists of
3 dust populations: small aromatic-rich carbon grains; bigger core/mantle
grains with mantles of aromatic-rich carbon and cores either made of amorphous
aliphatic-rich carbon or amorphous silicate. We assume an evolutionary path
where these grains, when entering denser regions, may first form a second
aliphatic-rich carbon mantle (coagulation of small grains, accretion of carbon
from the gas phase), second coagulate together to form large aggregates, and
third accrete gas phase molecules coating them with an ice mantle. To compute
the corresponding dust emission and scattering, we use a 3D Monte-Carlo
radiative transfer code. We show that our global evolutionary dust modelling
approach THEMIS allows us to reproduce C-shine observations towards dense
starless clouds. Dust scattering and emission is most sensitive to the cloud
central density and to the steepness of the cloud density profile. Varying
these two parameters leads to changes, which are stronger in the near-IR, in
both the C-shine intensity and profile. With a combination of aliphatic-rich
mantle formation and low-level coagulation into aggregates, we can
self-consistently explain the observed C-shine and far-IR/submm emission
towards dense starless clouds.Comment: Paper accepted for publication in A&A with companion paper "Mantle
formation, coagulation and the origin of cloud/core-shine: I. Dust scattering
and absorption in the IR", A.P Jones, M. Koehler, N. Ysard, E. Dartois, M.
Godard, L. Gavila
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Mid-infrared spectroscopy of CAI and AOA from the Allende CV3.2 chondrite
Mid-infrared spectra of bulk CAI from the CV3.2 chondrite Allende are presented and compared with astronomical spectra of cometary dust, zodiacal light,the circumstellar disk of beta Pictoris and dust around the red supergiant PR Per
Complex itinerant ferromagnetism in noncentrosymmetric Cr11Ge19
The noncentrosymmetric ferromagnet Cr11Ge19 has been investigated by
electrical transport, AC and DC magnetization, heat capacity, x-ray
diffraction, resonant ultrasound spectroscopy, and first principles electronic
structure calculations. Complex itinerant ferromagnetism in this material is
indicated by nonlinearity in conventional Arrott plots, unusual behavior of AC
susceptibility, and a weak heat capacity anomaly near the Curie temperature (88
K). The inclusion of spin wave excitations was found to be important in
modeling the low temperature heat capacity. The temperature dependence of the
elastic moduli and lattice constants, including negative thermal expansion
along the c axis at low temperatures, indicate strong magneto-elastic coupling
in this system. Calculations show strong evidence for itinerant ferromagnetism
and suggest a noncollinear ground state may be expected
Shear Modulus of an Elastic Solid under External Pressure as a function of Temperature: The case of Helium
The energy of a dislocation loop in a continuum elastic solid under pressure
is considered within the framework of classical mechanics. For a circular loop,
this is a function with a maximum at pressures that are well within reach of
experimental conditions for solid helium suggesting, in this case, that
dislocation loops can be generated by a pressure-assisted thermally activated
process. It is also pointed out that pinned dislocations segments can alter the
shear response of solid helium, by an amount consistent with current
measurements, without any unpinning.Comment: 5 pages, 3 figure
Rights Myopia in Child Welfare
For decades, legal scholars have debated the proper balance of parents\u27 rights and children\u27s rights in the child welfare system. This Article argues that the debate mistakenly privileges rights. Neither parents\u27 rights nor children\u27s rights serve families well because, as implemented, a solely rights-based model of child welfare does not protect the interests of parents or children. Additionally, even if well-implemented, the model still would not serve parents or children because it obscures the important role of poverty in child abuse and neglect and fosters conflict rather than collaboration between the state and families. In lieu of a solely rights-based model, this Article proposes a problem-solving model for child welfare and explores one embodiment of such a model, family group conferencing. This Article concludes that a problem-solving model holds significant potential to address many of the profound theoretical and practical shortcomings of the current child welfare system
Mantle formation, coagulation and the origin of cloud/core shine: I. Modelling dust scattering and absorption in the infra-red
Context. The observed cloudshine and coreshine (C-shine) have been explained
in terms of grain growth leading to enhanced scatter- ing from clouds in the J,
H and K photometric bands and the Spitzer IRAC 3.6 and 4.5 {\mu}m bands. Aims.
Using our global dust modelling approach THEMIS (The Heterogeneous dust
Evolution Model at the IaS) we explore the effects of dust evolution in dense
clouds, through aliphatic-rich carbonaceous mantle formation and grain-grain
coagulation. Methods. We model the effects of wide band gap a-C:H mantle
formation and the low-level aggregation of diffuse interstellar medium dust in
the moderately-extinguished outer regions of molecular clouds. Results. The
formation of wide band gap a-C:H mantles on amorphous silicate and amorphous
carbon (a-C) grains leads to a decrease in their absorption cross-sections but
no change in their scattering cross-sections at near-IR wavelengths, resulting
in higher albedos. Conclusions. The evolution of dust, with increasing density
and extinction in the diffuse to dense molecular cloud transition, through
mantle formation and grain aggregation, appears to be a likely explanation for
the observed C-shine.Comment: 12 pages, 15 figures, accepted for publication in A&A along with the
companion paper entitled, Mantle formation, coagulation and the origin of
cloud/core shine: II Comparison with observations, by Ysard et al. (also
accepted for publication in A&A
Neutron-skin thickness of Pb, and symmetry-energy constraints from the study of the anti-analog giant dipole resonance
The Pb(,) Pb reaction at a beam energy of
30 MeV has been used to excite the anti-analog of the giant dipole resonance
(AGDR) and to measure its -decay to the isobaric analog state in
coincidence with proton decay of IAS. The energy of the transition has also
been calculated with the self-consistent relativistic random-phase
approximation (RRPA), and found to be linearly correlated to the predicted
value of the neutron-skin thickness (). By comparing the
theoretical results with the measured transition energy, the value of 0.190
0.028 fm has been determined for of Pb, in
agreement with previous experimental results. The AGDR excitation energy has
also been used to calculate the symmetry energy at saturation (
MeV) and the slope of the symmetry energy ( MeV), resulting in
more stringent constraints than most of the previous studies.Comment: 6 pages, 5 figures. arXiv admin note: text overlap with
arXiv:1205.232
The evolution of amorphous hydrocarbons in the ISM: dust modelling from a new vantage point
Context. The evolution of amorphous hydrocarbon materials, a-C(:H),
principally resulting from ultraviolet (UV) photon absorption- induced
processing, are likely at the heart of the variations in the observed
properties of dust in the interstellar medium. Aims. The consequences of the
size-dependent and compositional variations in a-C(:H), from aliphatic-rich
a-C:H to aromatic-rich a-C, are studied within the context of the interstellar
dust extinction and emission. Methods. Newly-derived optical property data for
a-C(:H) materials, combined with that for an amorphous forsterite-type silicate
with iron nano-particle inclusions, a-SilFe, are used to explore dust evolution
in the interstellar medium. Results. We present a new dust model that consists
of a power-law distribution of small a-C grains and log-normal distributions of
large a-SilFe and a-C(:H) grains. The model, which is firmly anchored by
laboratory-data, is shown to quite naturally explain the variations in the
infrared (IR) to far-ultraviolet (FUV) extinction, the 217 nm UV bump, the IR
absorption and emission bands and the IR-mm dust emission. Conclusions. The
major strengths of the new model are its inherent simplicity and built-in
capacity to follow dust evolution in interstellar media. We show that mantle
accretion in molecular clouds and UV photo-processing in photo-dominated
regions are likely the major drivers of dust evolution.Comment: 22 pages, 20 figure
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