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CO concentration measurements using tunable diode laser absorption spectroscopy behind the shock waves in Martian atmosphere

机译:Co浓度测量使用可调谐二极管激光吸收光谱在火星大气中的冲击波后面

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Shock tube experiments are carried out to study the physical and chemical processes during a vehicle entry into the Marsatmosphere using tunable diode laser absorption spectroscopy (TDLAS) and optical emission spectroscopy (OES). COconcentration distributions are diagnosed behind a shock wave in a CO_2-N_2 mixture with three different conditions ofinitial pressure and velocity. The strong shock wave is established in a shock tube driven by combustion of hydrogen andoxygen. Time-resolved spectra of the Δv = 0 sequence of the B~2Σ~+→X~2Σ~+ electronic transition of CN have been observedthrough OES. A precise analysis of the CN violet spectra is performed and used to determine rotational and vibrationaltemperatures. Two absorption lines in the first overtone band of CO near 2.33 μm, are selected from a HITRANsimulation to calibrate laser wavelength and detect the CO concentration. Combined with these temperature results usingOES, CO concentrations in the thermal equilibrium region are derived, which are 2.91 × 10~(17) cm~(-3), 7.46 × 10~(17) cm~(-3) and1.01 × 10~(18) cm~(-3), corresponding to equilibrium temperatures equal to 7000 ± 400 K, 7400 ± 300 K, 6000 ± 300 K in thelow, medium and high pressure conditions, respectively.
机译:进行了冲击管实验,以研究车辆进入火星时的物理和化学过程使用可调谐二极管激光吸收光谱(TDLA)和光发射光谱(OES)的气氛。 CO.浓度分布被诊断为在CO_2-N_2混合物中的冲击波后面,其三种不同的条件初始压力和速度。在由氢气燃烧驱动的冲击管中建立了强烈的冲击波氧。已经观察到,已经观察到CN的B〜2σ〜→X〜+电子转换的ΔV= 0序列的时间分辨光谱通过OES。进行CN紫光谱的精确分析,并用于确定旋转和振动温度。来自CO近2.33μm的第一个泛孔带中的两个吸收线选自HITRAN模拟以校准激光波长并检测CO浓度。结合这些温度结果衍生热平衡区域中的CO浓度,其为2.91×10〜(17)cm〜(-3),7.46×10〜(17)cm〜(3)1.01×10〜(18)cm〜(3),对应于平衡温度等于7000±400 k,7400±300 k,6000±300 k低,中等和高压条件。

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