论文标题
螃蟹星云的索非亚/HAWC+观测:偏光发射的灰尘特性
SOFIA/HAWC+ observations of the Crab Nebula: dust properties from polarised emission
论文作者
论文摘要
超新星残留物(SNR)是众所周知的粉尘生产者,但是由于谷物性质的不确定性,它们的净灰尘生产率仍然难以捉摸,这些特性不确定性地传播到观察到的尘埃质量不确定性,并确定这些谷物的有效性如何通过反向冲击来处理。在本文中,我们介绍了螃蟹脉冲星云中的极化粉尘发射的检测,第二个具有确认的SNR。在CassiopeiaA。CassiopeiaA后,我们用新的Sofia/Hawc+极化数据限制了Band C 89 UM和Band d 154 UM中粉尘的大量组成。校正同步加速器极化后,我们报告了尘埃偏振量的范围为3.7-9.6%和2.7-7.6%,分别为89和154 um的三个单独的尘土飞扬的细丝。检测到的极化信号表明蟹状星云中存在大(> 0.05-0.1 um)。随着观察到的极化以及极化和总通量,我们限制了碳质和硅酸盐晶粒的温度和质量。我们发现,富含碳的晶粒质量分数在12%至70%之间变化,这表明该SNR中的碳质和硅酸盐谷物共存。碳质和硅酸盐晶粒的温度分别为40 K至70 K,从30 K到50 K。在三个单个区域中,尘埃质量从10^{-4} MSOL到碳粒晶粒的10^{ - 2} MSOL,再到10^{ - 1} MSOL,用于三个单个区域的硅酸盐晶粒。
Supernova remnants (SNRs) are well-recognised dust producers, but their net dust production rate remains elusive due to uncertainties in grain properties that propagate into observed dust mass uncertainties, and determine how efficiently these grains are processed by reverse shocks. In this paper, we present a detection of polarised dust emission in the Crab pulsar wind nebula, the second SNR with confirmed polarised dust emission after Cassiopeia A. We constrain the bulk composition of the dust with new SOFIA/HAWC+ polarimetric data in band C 89 um and band D 154 um. After correcting for synchrotron polarisation, we report dust polarisation fractions ranging between 3.7-9.6 per cent and 2.7-7.6 per cent in three individual dusty filaments at 89 and 154 um, respectively. The detected polarised signal suggests the presence of large (> 0.05-0.1 um) grains in the Crab Nebula. With the observed polarisation, and polarised and total fluxes, we constrain the temperatures and masses of carbonaceous and silicate grains. We find that the carbon-rich grain mass fraction varies between 12 and 70 per cent, demonstrating that carbonaceous and silicate grains co-exist in this SNR. Temperatures range from 40 K to 70 K and from 30 K to 50 K for carbonaceous and silicate grains, respectively. Dust masses range from 10^{-4} Msol to 10^{-2} Msol for carbonaceous grains and to 10^{-1} Msol for silicate grains, in three individual regions.