Morris Patrick W, Gull Theodore R, Hillier D John, Barlow M J, Royer Pierre, Nielsen Krister, Black John, Swinyard Bruce
California Institute of Technology, IPAC, M/C 100-22, Pasadena, CA 91125.
NASA Goddard Space Flight Center, Code 667, Greenbelt, MD 20771.
Astrophys J. 2017 Jun 20;842(2). doi: 10.3847/1538-4357/aa71b3. Epub 2017 Jun 15.
Infrared observations of the dusty, massive Homunculus Nebula around the luminous blue variable Carinae are crucial to characterize the mass-loss history and help constrain the mechanisms leading to the Great Eruption. We present the 2.4 - 670 m spectral energy distribution, constructed from legacy ISO observations and new spectroscopy obtained with the Using radiative transfer modeling, we find that the two best-fit dust models yield compositions which are consistent with CNO-processed material, with iron, pyroxene and other metal-rich silicates, corundum, and magnesium-iron sulfide in common. Spherical corundum grains are supported by the good match to a narrow 20.2 m feature. Our preferred model contains nitrides AlN and SiN in low abundances. Dust masses range from 0.25 to 0.44 but ≥ 45 in both cases due to an expected high Fe gas-to-dust ratio. The bulk of dust is within a 5″ × 7″ central region. An additional compact feature is detected at 390 m. We obtain = 2.96 × 10 , a 25% decline from an average of mid-IR photometric levels observed in 1971-1977. This indicates a reduction in circumstellar extinction in conjunction with an increase in visual brightness, allowing 25-40% of optical and UV radiation to escape from the central source. We also present an analysis of CO and CO = 5 - 4 through 9 - 8 lines, showing that the abundances are consistent with expectations for CNO-processed material. The [C II] line is detected in absorption, which we suspect originates in foreground material at very low excitation temperatures.
对明亮蓝变星船底座周围尘埃密布的大质量侏儒星云进行红外观测,对于描绘其质量损失历史并有助于限制导致大爆发的机制至关重要。我们展示了从遗留的红外空间天文台(ISO)观测数据和利用昴星团望远镜获得的新光谱构建的2.4 - 670微米光谱能量分布。通过辐射传输建模,我们发现两个最佳拟合尘埃模型产生的成分与经碳氮氧(CNO)处理的物质一致,常见的有铁、辉石和其他富含金属的硅酸盐、刚玉以及镁铁硫化物。与一条狭窄的20.2微米特征的良好匹配支持了球形刚玉颗粒的存在。我们的首选模型包含低丰度的氮化物氮化铝(AlN)和氮化硅(SiN)。尘埃质量范围为0.25至0.44 ,但由于预期的高铁气尘比,两种情况下 ≥ 45 。大部分尘埃位于一个5″×7″的中心区域内。在390微米处检测到一个额外的致密特征。我们得到 = 2.96 × 10 ,比1971 - 1977年观测到的中红外光度水平平均值下降了25%。这表明星周消光减少,同时目视亮度增加,使得25 - 40%的光学和紫外线辐射能够从中央源逃逸。我们还对一氧化碳(CO)从5 - 4到9 - 8的谱线以及二氧化碳(CO₂)进行了分析,结果表明其丰度与对经CNO处理物质的预期一致。检测到[C II]线处于吸收状态,我们怀疑它起源于极低激发温度下的前景物质。