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首页> 外文期刊>The Astrophysical journal >PHOTOELECTRIC HEATING AND [C Ⅱ] COOLING OF HIGH GALACTIC LATITUDE TRANSLUCENT CLOUDS
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PHOTOELECTRIC HEATING AND [C Ⅱ] COOLING OF HIGH GALACTIC LATITUDE TRANSLUCENT CLOUDS

机译:高银河半透明云团的光电加热和[CⅡ]冷却

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摘要

The (~2P_(3/2) → ~2P_(1/2)) transition of singly ionized carbon, [C Ⅱ], is the primary coolant of diffuse interstellar gas. We describe observations of [C Ⅱ] emission toward nine high Galactic latitude translucent molecular clouds, made with the long-wavelength spectrometer on board the Infrared Space Observatory. To understand the role of dust grains in processing the interstellar radiation field (ISRF) and heating the gas, we compare the [C Ⅱ] integrated intensity with the far-infrared (far-IR) integrated surface brightness for the 101 sampled lines of sight. We find that [C Ⅱ] is linearly correlated with far-IR, and the average ratio is equal to that measured with the COBE satellite for all high-latitude Milky Way gas. There is a significant decrease that was not detected with COBE in [C Ⅱ] emissivity at high values of far-IR. Our sample splits naturally into two populations depending on the 60 μm/100 μm surface brightness ratio, or color: "warm" positions with 60/100 > 0.16 and "cold "positions with 60/100 < 0.16. A transition from sources with warm to those with cold 60/100 colors coincides approximately with the transition from constant to decreasing [C Ⅱ] emissivity. We model the [C Ⅱ] and far-IR emission under conditions of thermal equilibrium, using the simplifying assumptions that, in all regions heated by the ISRF, the most important source of gas heating is the photoelectric effect on grains and the most important source of gas cooling is [C Ⅱ] emission. The model matches the data well, provided the ISRF incident flux is χ_0 ≈ 1.6 (in units of the nominal value near the Sun), and the photoelectric heating efficiency is ε ≈ 4.3%. There are no statistically significant differences in the derived values of χ_0 and ε for warm and cold sources. The observed variations in the [C Ⅱ] emissivity and the 60/100 colors can be understood entirely in terms of the attenuation and softening of the ISRF by translucent clouds, not changes in dust properties.
机译:单离子化碳的[〜2P_(3/2)→〜2P_(1/2))跃迁[CⅡ]是星际弥散气体的主要冷却剂。我们描述了用长波光谱仪在红外空间天文台上向九个高银河纬度半透明分子云发射[CⅡ]的观测结果。为了了解尘粒在处理星际辐射场(ISRF)和加热气体中的作用,我们比较了101条采样视线的[CⅡ]积分强度与远红外(far-IR)积分表面亮度。我们发现,[CⅡ]与远红外线性相关,并且平均比率等于用COBE卫星测得的所有高纬度银河系气体的平均比率。在远红外值较高时,[CⅡ]的发射率存在COBE未检测到的显着降低。我们的样本根据60μm/ 100μm表面亮度比率或颜色自然分为两个种群:60/100> 0.16的“温暖”位置和60/100 <0.16的“冷”位置。从暖色源到冷色60/100色源的过渡近似与从恒定[CⅡ]发射率过渡到降低。我们使用简化的假设,即在ISRF加热的所有区域中,最重要的气体加热源是对谷物的光电效应,也是最重要的源,对热平衡条件下的[CⅡ]和远红外发射进行建模。气体冷却是[CⅡ]排放。只要ISRF入射通量为χ_0≈1.6(以太阳附近的名义值为单位),并且光电加热效率为ε≈4.3%,该模型就可以很好地匹配数据。对于冷热源,χ_0和ε的推导值没有统计学上的显着差异。观察到的[CⅡ]发射率和60/100颜色的变化可以完全理解为半透明云对ISRF的衰减和软化,而不是尘埃特性的变化。

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