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The abundance of HNCO and its use as a diagnostic of environment

机译:HNCO的丰富性及其在环境诊断中的用途

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Aims. We aim to investigate the chemistry and gasphase abundance of HNCO and the variation of the HNCO/CS abundanceratio as a diagnostic of the physics and chemistry in regions ofmassive star formation. Methods. A numerical-chemical model has beendeveloped which self-consistently follows the chemical evolution of ahot core. The model comprises of two distinct stages. The first stagefollows the isothermal, modified free-fall collapse of a molecular darkcloud. This is immediately followed by an increase in temperature whichrepresents the switch on of a central massive star and the subsequentevolution of the chemistry in a hot, dense gas cloud (the hot core).During the collapse phase, gas species are allowed to accrete on tograin surfaces where they can participate in further reactions. Duringthe hot core phase surface species thermally desorb back in to theambient gas and further chemical evolution takes place. For comparison,the chemical network was also used to model a simple dark cloud andphotodissociation regions. Results. Our investigation reveals that HNCO isinefficiently formed when only gas-phase formation pathways areconsidered in the chemical network with reaction rates consistent withexisting laboratory data. This is particularly true at low temperaturesbut also in regions with temperatures up to 200K. Using currently measured gasphase reaction rates, obtaining the observed HNCO abundances requiresits formation on grain surfaces - similar to other ``hot core'' speciessuch as CH3OH. However our model shows that thegas phase HNCO in hot cores is not a simple direct product of theevaporation of grain mantles. We also show that the HNCO/CS abundanceratio varies as a function of time in hot cores and can match the rangeof values observed. This ratio is not unambiguously related to theambient UV field as been suggested - our results are inconsistent withthe hypothesis of Martín etal. (2008, ApJ, 678, 245). Inaddition, our results show that this ratio is extremely sensitive tothe initial sulphur abundance. We find that the ratio growsmonotonically with time with an absolute value which scalesapproximately linearly with the S abundance at early times. Key words: astrochemistry - stars:formation
机译:目的我们旨在研究HNCO的化学和气相丰度以及HNCO / CS的丰度比变化,以诊断大质量恒星形成区域的物理和化学。方法。已经建立了一个数值化学模型,该模型自发地跟随着热核的化学演化。该模型包括两个不同的阶段。第一阶段遵循分子暗云的等温,改进的自由落体塌陷。紧接着是温度升高,这代表着中央大质量恒星的开启以及随后化学物质在热的致密气体云(热核)中的演化。在坍缩阶段,气体物质被允许在粒状颗粒上积聚。他们可以参与进一步反应的表面。在热芯相阶段,表面物质热解吸回周围的气体中,并进一步发生化学反应。为了进行比较,还使用化学网络对简单的暗云和光解离区域进行建模。结果。我们的研究表明,仅在化学网络中考虑气相形成途径且反应速率与现有实验室数据一致时,HNCO的形成效率较低。在低温下尤其如此,在温度高达200K的区域中也是如此。使用当前测量的气相反应速率,要获得观测到的HNCO丰度,需要在谷物表面形成-类似于其他``热核''物种,例如CH3OH。然而,我们的模型表明,热核中的气相HNCO并不是颗粒幔蒸发的简单直接产物。我们还表明,HNCO / CS丰度比在热芯中随时间变化,并且可以与观察到的值范围相匹配。正如所建议的,该比率与环境紫外线场没有明确关系-我们的结果与Martín等人的假设不一致。 (2008,ApJ,678,245)。另外,我们的结果表明该比例对初始硫丰度极为敏感。我们发现该比率随时间单调增长,其绝对值在早期与S丰度成线性比例关系。关键词:天化学-恒星:形成

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