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Development of a Chemistry Model for DSMC Simulation of the Atmosphere of Io using Molecular Dynamics

机译:利用分子动力学发展DSMC模拟的化学模型

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A significant process in the formation of the unique atmosphere of lo, a Jovian moon, is collision-induced dissociation of sulfur dioxide. The rarefied nature of the Ionian atmosphere makes its simulation by the Direct Simulation Monte Carlo method (DSMC) the method of choice. However, there is a lack of reliable data on collisions, particularly reaction and collision cross sections needed for DSMC, of Ionian species at the conditions seen in its atmosphere. As such, collisions between SO_2 and O are studied through Molecular Dynamics, Quasi-Classical Trajectories using two different methods for determining molecular potential: a polynomial potential defined by Murrell [1] and a complex tunable potential defined by the ReaxFF force field. Five possible reaction paths are considered: atomization of the SO_2 molecule, dissociation to SO, dissociation to O_2, and the formation of SO_3, and an exchange reaction leading to SO and O_2. Relative velocities and initial SO_2 internal energies relevant to Io's atmospheric conditions are used. The results from each chemistry model are analyzed and compared to each other, in particular the reaction cross sections and equivalent variable hard sphere cross sections. In general, higher collision energies are found to cause atomization of the SO_2. In addition, dissociation to SO is a significant process for many of the studied cases, but dissociation to O_2 is mostly a negligible process. Finally, formation of SO_3 occurs only at low impact velocities. The chemistry and collision models developed from the Murrell and ReaxFF methods are then implemented in DSMC 0-D, time-dependant and 2-D axisymmetric simulations under conditions relevant to the Ionian atmosphere. The results of these analyses are examined, and compared to results obtained using the baseline Total Collisional Energy (TCE) model and the previous results of Deng et al [2]. It is found that the new Murrell and ReaxFF based models predict less SO_2 dissociation than previous models, and that simulated Ionian atmospheric structure is sensitive to the total cross section model.
机译:在罗马月亮的独特气氛中形成了一个重要的过程,是二氧化硫的碰撞诱导的二氧化硫解剖。 Ionian大气层的稀土性质通过直接仿真蒙特卡罗方法(DSMC)进行了模拟。然而,在其大气中所见的条件下,缺乏关于DSMC所需的碰撞,特别是对DSMC所需的反应和碰撞横截面的可靠数据。因此,通过分子动力学,使用两种不同的方法来研究SO_2和O之间的碰撞,用于确定分子电位:由Murrell [1]限定的多项式电位和由Reaxff力场限定的复杂可调谐电位。考虑了五种可能的反应路径:SO_2分子的雾化,离解,离解,对O_2的解离,以及形成为SO_3的形成和O_2的交换反应。使用与IO的大气条件相关的相对速度和初始SO_2内部能量。分析并彼此进行分析并比较各种化学模型的结果,特别是反应横截面和等同的可变硬球横截面。通常,发现更高的碰撞能量导致SO_2的雾化。此外,解离对许多研究的病例是一个重要的过程,而是对O_2的解离主要是一个可忽略的过程。最后,SO_3的形成仅在低冲击速度下发生。然后在与爱奥尼亚气氛相关的条件下在DSMC 0-D,时间相关和2-D轴对称模拟中实现从Murrell和Reaxff方法开发的化学和碰撞模型。检查这些分析的结果,并与使用基线总碰撞能量(TCE)模型获得的结果进行比较,以及邓等[2]的先前结果。结果发现,新的Murrell和Reaxff的模型预测了比以前的模型更少的SO_2离解,并且模拟的离子大气结构对总横截面模型敏感。

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