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INTERPRETING THE ROLE OF THE MAGNETIC FIELD FROM DUST POLARIZATION MAPS

机译:从粉尘极化图解释磁场的作用

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Dust polarization observations from the Submillimeter Array (SMA) and the Caltech Submillimeter Observatory (CSO) are analyzed with the goal of providing a general tool to interpret the role of the magnetic field in molecular clouds. Magnetic field and dust emission gradient orientations are observed to show distinct patterns and features. The angle δ between these two orientations can be interpreted as a magnetic field alignment deviation, assuming the emission gradient orientation to coincide with the density gradient orientation in the magnetohydrodynamics force equation. In SMA high-resolution (collapsing) cores, additional symmetry properties in δ can reveal accretion and outflow zones. All these observational findings suggest the angle δ to be a relevant quantity that can assess the role of the magnetic field. Indeed, when comparing this angle with the (projection-free) magnetic field significance Σ B (introduced by Koch and coworkers in 2012), it is demonstrated that |δ| yields an approximation to the change in Σ B . Thus, changes in the magnetic field alignment deviation δ trace changes in the role of the magnetic field. The angle δ is observationally straightforward to determine, providing a tool to distinguish between zones of minor or significant magnetic field impact. This is exemplified by the CSO M+0.25 + 0.01, Mon?R2, CO+0.02 – 0.02, M–0.02 – 0.07 sources and by the SMA high-resolution data from W51 e2, W51 North, Orion BN/KL and g5.89. Additional CSO sources are analyzed, providing further support of this result. Finally, based on the different features found in our sample of 31 sources in total, covering sizes from large-scale complexes to collapsing cores, a schematic evolutionary scenario is proposed. Here, the significance of the magnetic field evolves both with position and scale, and can be assessed with the angle δ.
机译:分析了亚毫米波阵列(SMA)和加州理工学院亚毫米波观测站(CSO)产生的粉尘极化现象,目的是提供一种通用的工具来解释磁场在分子云中的作用。观察到磁场和粉尘发射梯度方向显示出不同的图案和特征。假设发射梯度方向与磁流体动力方程中的密度梯度方向一致,则这两个方向之间的角度δ可以解释为磁场对准偏差。在SMA高分辨率(塌陷)岩心中,δ的其他对称性可以显示积聚和流出区域。所有这些观察结果表明,角度δ是可以评估磁场作用的相关量。的确,当将该角度与(无投影的)磁场显着度ΣB(由Koch和他的同事在2012年引入)进行比较时,证明|δ|等于0。得出ΣB变化的近似值。因此,磁场对准偏差δtrace的变化对磁场的作用也发生变化。角度δ在观察上很容易确定,为区分较小或较大磁场影响的区域提供了一种工具。 CSO M + 0.25 + 0.01,Mon?R2,CO + 0.02 – 0.02,M–0.02 – 0.07源以及W51 e2,W51 North,Orion BN / KL和g5的SMA高分辨率数据举例说明了这一点。 89。分析了其他CSO来源,为该结果提供了进一步的支持。最后,根据我们在总共31种来源的样本中发现的不同特征(涵盖从大型复合物到塌陷核的大小),提出了一种示意性的进化方案。在此,磁场的重要性随位置和比例而变化,并且可以通过角度δ进行评估。

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