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Model infrared spectra of passively heated proto-planetary disks surrounding intermediate-mass pre-main-sequence stars

机译:围绕中等质量主序前恒星的被动加热原行星盘的红外光谱模型

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Aims. We study theoretical spectra at mid-infrared (5-40)wavelengths of proto-planetary disks surrounding intermediate-mass pre-main-sequence stars. Observations show a wide range of spectral shapes and a rich variety in strength and shape of dust resonances. These strong variations in spectral shape reflect differences in the nature and spatial distribution of dust particles in the disk. The aim of this study is to establish what model parameters influence the mid-IRspectra of planet-forming disks. Methods. A grid of models of passively heated proto-planetary disks is used to calculate the infrared spectrum. We use hydrostatic equilibrium disk models and radiative transfer to calculate the emerging spectrum. We focus on the effects that different disk geometries (flaring, self-shadowed) and dust mineralogy have on the emerging 5-40spectrum. We adopt four scenarios for the radial and vertical distribution of crystalline silicate dust. Results. In our model, the 23.5forsterite band is more sensitive to emission from regions <30AU, while the 33.5forsterite band probes regions up to 50AU. The 23.5band strength does not depend on the degree of flaring of the disk, while the 33.5band does. Only models with a substantial abundance (>5percent) of crystalline silicates at a long distance from the star (>20-50AU) show detectable emission in the 33.5forsterite band. The carbon-dust abundance affects the strength of the dust resonances in the 10spectral region, but not in the 30region. Key words: stars: planetary systems: protoplanetary disks - stars: pre-main sequence - stars: circumstellar matter
机译:目的我们研究围绕中等质量主序前恒星的原行星盘在中红外(5-40)波长处的理论光谱。观测结果表明,光谱形状范围很广,尘埃共振的强度和形状也多种多样。光谱形状的这些强烈变化反映了磁盘中灰尘颗粒的性质和空间分布的差异。这项研究的目的是确定哪些模型参数会影响行星形成盘的中红外光谱。方法。被动加热的原行星盘模型网格用于计算红外光谱。我们使用静水力平衡盘模型和辐射传递来计算新兴光谱。我们关注不同的磁盘几何形状(扩口,自阴影)和粉尘矿物学对新兴的5-40光谱的影响。对于结晶硅酸盐粉尘的径向和垂直分布,我们采用了四种方案。结果。在我们的模型中,23.5镁橄榄石带对<30AU区域的发射更敏感,而33.5镁橄榄石带探测高达50AU的区域。 23.5band的强度不取决于磁盘的张开程度,而33.5band则取决于。只有在距恒星(> 20-50AU)很远的地方具有大量(大于5%)结晶硅酸盐的模型才会在33.5镁橄榄石带中显示可检测到的发射。碳尘含量会影响10个光谱区域的尘埃共振强度,但不会影响30个光谱区域的尘埃共振强度。关键词:恒星:行星系统:原行星盘-恒星:主前序-恒星:绕星物质

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