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NUMERICAL SIMULATIONS OF RADIATIVE HEAT EFFECTS AT A PLASMA WIND-TUNNEL FLOW UNDER MARS ENTRY CONDITIONS

机译:火星进入条件下等离子风隧道流动辐射热效应的数值模拟

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Mars atmosphere, consisting mainly of CO_2, with a few percent of N_2 and other trace gases, is of interest to future space projects. Entry into its gaseous shell is of current significant research interest. For this application, an arc jet driven plasma wind tunnel is available to simulate relevant entry conditions for the planet. Recent improvements and qualification of the test facility, enables the testing on earth of high enthalpy flows with CO_2 rich composition. In order to complement the experimental analysis, numerical simulations of the test facility running at relevant ambient pressures of some 600 - 1000 Pa, corresponding to low altitudes, have been completed. The simulations used a density-based Navier Stokes solver, and with non-equilibrium chemical and thermal effects which are characteristic of these types of high enthalpy flows. Special interest is given to the radiative heat transfer mechanism. Under these high temperature conditions, radiative effects become more relevant and advanced radiation models must be used. The coupling between the Navier Stokes and radiative transfer equations favours the understanding of plasma wind tunnel flows. The radiative heat is estimated using the k-distribution spectral model, which is appropriate for nonhomogeneous radiating media. The numerical results and measurements are compared in order to improve the analysis methods for Mars entry flows.
机译:MARS气氛主要由CO_2组成,占未来空间项目的百分之几的N_2和其他痕量气体。进入其气体壳是目前的重大研究兴趣。对于本申请,可以为弧形喷射驱动的等离子体风洞进行模拟地球的相关进入条件。最近的测试设施的改进和资格,可以使用CO_2富含组合物的高焓流的地球测试。为了补充实验分析,完成了在600 - 1000Pa的相关环境压力下运行的测试设施的数值模拟,对应于低海拔。该模拟使用了基于密度的Navier Stokes求解器,并具有非平衡化学和热效应,这些化学和热效应是这些类型的高焓流的特征。特别兴趣给辐射传热机制。在这些高温条件下,辐射效果变得更加相关,必须使用先进的辐射模型。 Navier Stokes和辐射传递方程之间的耦合有利于对等离子风洞流动的理解。使用K分布光谱模型估计辐射热,这适用于非均匀辐射介质。比较数值结果和测量,以改善火星条目流动的分析方法。

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