首页> 外文期刊>The Astrophysical journal >A STUDY OF THE MUTUAL INTERACTION BETWEEN THE MONOCEROS R2 OUTFLOW AND ITS SURROUNDING CORE
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A STUDY OF THE MUTUAL INTERACTION BETWEEN THE MONOCEROS R2 OUTFLOW AND ITS SURROUNDING CORE

机译:MONOCEROS R2出流与其周围核互作用的研究

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We present high-resolution (12″-24″) ~(12)CO(J = 2-1), ~(13)CO(2-1), CS(2-1), CS(3-2), and CS(5-4) maps of the central 4′ x 4′ of Mon R2 and study the bipolar outflow, the dense core, and their mutual interaction. The high-velocity ~(12)CO and ~(13)CO emissions that trace the bipolar outflow show that the outflow lobes are limb-brightened shells of accelerated gas that have the Mon R2 IR cluster near their apex and extend approximately toward the north and south. These shells of gas are clumpy, and their emission at the highest velocities arises from discrete condensations that move with the flow but each has a slightly different speed. The CS data, on the other hand, trace the ambient core at low velocities, but also trace the accelerated gas of the outflow at higher speeds. The ambient CS emission shows that the core has a cavity along the path of the outflow, and that the walls of this cavity coincide in position and orientation with the shells of the bipolar flow. The accelerated CS emission concentrates along the cavity walls and arises from the same clumpy shells of gas that form the outflow lobes in ~(12)CO and ~(13)CO. This outflow material, therefore, is rather dense, and a solution of the CS radiative transfer shows that it is as dense as the gas in the core (≈4x 10~5 cm~(-3)), suggesting that what we see as outflow is in fact gas from the dense core that has been set into motion. With the same radiative transfer analysis of the CS lines, we estimate that from a total of 1000 solar mass of dense gas in the core, more than 170 solar mass have been accelerated and incorporated into the bipolar flow. In addition, the CS spectra show a systematic enhancement of the line width toward the IR cluster that suggests the outflow has increased the gas turbulence in its vicinity. The amount of kinetic energy contained in both the bipolar and turbulent motions is comparable to the total binding energy of the dense gas, and this shows that the action of the outflow on the core can be strong enough to affect the distribution of dense gas in the core. We therefore propose that the cavity in the dense gas is the result of the evacuation of a channel by the outflow, and that the material initially filling its volume has been accelerated and incorporated into the flow. The Mon R2 system, therefore, illustrates how bipolar molecular outflows form through the acceleration of ambient molecular gas and that the process of molecular outflow formation is accompanied by a partial destruction of the dense gas environment of the newly formed star.
机译:我们提出了高分辨率(12″ -24″)〜(12)CO(J = 2-1),〜(13)CO(2-1),CS(2-1),CS(3-2),以及Mon R2中心4'x 4'的CS(5-4)图,研究了双极流出,密实核及其相互相互作用。追踪双极流出的〜(12)CO和〜(13)CO高速排放表明,流出瓣为肢体发亮的加速气体壳,其Mon R2 IR团簇靠近其顶点并大致向北延伸和南方。这些气体壳是块状的,它们以最高速度排放是由于离散的冷凝物引起的,这些冷凝物随流动而移动,但每个冷凝器的速度略有不同。另一方面,CS数据以较低的速度跟踪环境堆芯,但也以较高的速度跟踪流出的加速气体。环境CS发射表明,岩心在流出路径上有一个空腔,该空腔的壁在位置和方向上与双极流的壳层重合。加速的CS发射沿空腔壁集中,并由形成〜(12)CO和〜(13)CO中的流出瓣的相同块状气体壳产生。因此,这种流出的物质非常稠密,CS辐射传递的解决方案表明它与堆芯中的气体一样稠密(≈4x10〜5 cm〜(-3)),这表明我们看到的是实际上,流出的气体是来自致密芯的已开始运动的气体。通过对CS线进行相同的辐射传递分析,我们估计从核心中总共1000个太阳质量的稠密气体中,已有170多个太阳质量被加速并纳入了双极流。另外,CS光谱显示了朝向IR簇的线宽的系统增强,这表明流出增加了其附近的气体湍流。双极运动和湍流运动中包含的动能数量均与稠密气体的总结合能相当,这表明流出液对岩心的作用可能足以影响稠密气体在岩心中的分布。核心。因此,我们提出,致密气体中的空腔是流出通道疏散的结果,并且最初填充其体积的材料已被加速并整合到流中。因此,Mon R2系统说明了如何通过环境分子气体的加速形成双极分子外流,以及分子外流形成的过程伴随着新形成恒星的致密气体环境的部分破坏。

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