1999
DOI: 10.3936/35
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Cited by 4 publications
(6 citation statements)
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“…For the opacities of the dust we use a mixture of silicates (∼58%), iron sulphide (∼18%), and carbonaceous dust grains (∼24%) with an average density of ρmix = 3.2 g/cm 3 (Min et al 2011) and a porosity of p = 0.625, corresponding to the density ρ = 1.2 g/cm 3 used in the dust evolution simulations. The indices of refraction are obtained from: Dorschner et al (1995); Henning & Stognienko (1996) for the silicates, Begemann et al (1994) for the iron sulphide, and Preibisch et al (1993) for the carbonaceous dust grains. For Figure A1.…”
Section: A2 Radiative Transfer and Synthetic Observationsmentioning
confidence: 99%
“…For the opacities of the dust we use a mixture of silicates (∼58%), iron sulphide (∼18%), and carbonaceous dust grains (∼24%) with an average density of ρmix = 3.2 g/cm 3 (Min et al 2011) and a porosity of p = 0.625, corresponding to the density ρ = 1.2 g/cm 3 used in the dust evolution simulations. The indices of refraction are obtained from: Dorschner et al (1995); Henning & Stognienko (1996) for the silicates, Begemann et al (1994) for the iron sulphide, and Preibisch et al (1993) for the carbonaceous dust grains. For Figure A1.…”
Section: A2 Radiative Transfer and Synthetic Observationsmentioning
confidence: 99%
“…Alternatively, the difference between the average IRS spectrum of quasars and the IRS spectra of our three galaxies could be due to different silicate composition. Dorschner et al (1995) have experimentally demonstrated that the absorption in the UV, optical and near-IR up to λ < 8 µm of amorphous silicate dust decreases with the decrease of the iron content in the dust. As shown in Figure 4 of Dorschner et al (1995), the imaginary part of the index of refraction of MgSiO 3 is smaller than that of Mg 0.4 Fe 0.6 SiO 3 by a factor of > 10.…”
Section: Discussionmentioning
confidence: 99%
“…Dorschner et al (1995) have experimentally demonstrated that the absorption in the UV, optical and near-IR up to λ < 8 µm of amorphous silicate dust decreases with the decrease of the iron content in the dust. As shown in Figure 4 of Dorschner et al (1995), the imaginary part of the index of refraction of MgSiO 3 is smaller than that of Mg 0.4 Fe 0.6 SiO 3 by a factor of > 10. It is possible that the silicate dust in quasars and typical AGNs are iron-rich, while the silicate dust in the three galaxies are iron-poor.…”
Section: Discussionmentioning
confidence: 99%
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“…The ubiquitous and conspicuous 10 and 20-µm features are essential to this choice (see, for instance, the study of forsterite (Olivine group) and enstatite ( Pyroxene group) by Pegourie and Papoular 1985). In the visible, these silicates were found to be fairly transparent (see Nitsan et al 1978, Palik 1985Dorschner et al 1995). This was difficult to reconcile with observations of polarization of InterStellar (IS) visible light which exhibits a wide, prominent, asymmetric bump whose peak wavelength, λmax, varies from 0.3 to 0.8 µm, with a mean value of 0.55 (see Spitzer 1978;Whittet 2003, Fig.…”
Section: Introductionmentioning
confidence: 99%