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首页> 外文期刊>The Astrophysical journal >EVIDENCE FOR CLOUD-CLOUD COLLISION AND PARSEC-SCALE STELLAR FEEDBACK WITHIN THE L1641-N REGION
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EVIDENCE FOR CLOUD-CLOUD COLLISION AND PARSEC-SCALE STELLAR FEEDBACK WITHIN THE L1641-N REGION

机译:L1641-N区域内的云冲突和准大规模星空反馈的证据

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We present high spatial resolution 12CO (J = 1-0) images taken by the Nobeyama 45 m telescope toward a 48' × 48' area, including the L1641-N cluster. The effective spatial resolution of the maps is 21'', corresponding to 0.04?pc at a distance of 400?pc. A recent 1.1?mm dust continuum map reveals that the dense gas is concentrated in several thin filaments. We find that a few dust filaments are located at the parts where 12CO (J = 1-0) emission drops sharply. Furthermore, the filaments have two components with different velocities. The velocity difference between the two components is about 3?km?s–1, corresponding to a Mach number of 10, significantly larger than the local turbulent velocity in the cloud. These facts imply that the collision of the two components (hereafter, the cloud-cloud collision) possibly contributed to the formation of these filaments. Since the two components appear to overlap toward the filaments on the plane of the sky, the collision may have occurred almost along the line of sight. Star formation in the L1641-N cluster was probably triggered by such a collision. We also find several parsec-scale CO shells whose centers are close to either the L1641-N cluster or the V 380 Ori cluster. We propose that these shells were created by multiple winds and/or outflows from cluster young stellar objects, i.e., "protocluster winds." One exceptional dust filament located at the western cloud edge lies along a shell; it is presumably part of the expanding shell. Both the cloud-cloud collision and protocluster winds are likely to influence the cloud structure and kinematics in this region.
机译:我们展示了Nobeyama 45 m望远镜向48'×48'区域(包括L1641-N团簇)拍摄的高分辨率12CO(J = 1-0)图像。地图的有效空间分辨率为21英寸,对应于400英寸距离处的0.04英寸距离。最近的1.1毫米尘埃连续体图显示,致密气体集中在几根细丝中。我们发现一些尘埃丝位于12CO(J = 1-0)排放急剧下降的部分。此外,细丝具有两个具有不同速度的成分。这两个分量之间的速度差大约为3?km?s-1,对应的马赫数为10,大大大于云中的局部湍流速度。这些事实暗示两个成分的碰撞(以下称为云-云碰撞)可能有助于这些细丝的形成。由于这两个分量似乎在天空平面上朝向细丝重叠,因此碰撞可能几乎发生在视线范围内。 L1641-N星团中的恒星形成可能是由这种碰撞引起的。我们还发现了几个等分尺度的CO壳,其中心靠近L1641-N群集或V 380 Ori群集。我们建议这些壳是由多个风和/或簇状年轻恒星物体(即“原团团风”)的流出所产生的。位于西云边缘的一根特殊的尘埃细丝沿着贝壳排列着。它大概是扩展壳的一部分。云与云的碰撞和原团簇风都可能影响该地区的云结构和运动学。

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