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Measurement of atomic oxygen in the middle atmosphere using solid electrolyte sensors and catalytic probes

机译:使用固体电解质传感器和催化探针测量中层大气中的原子氧

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The middle- and upper-atmospheric energy budget is largely dominated byreactions involving atomic oxygen (O). Modeling of these processesrequires detailed knowledge about the distribution of this oxygen species.Understanding the mutual contributions of atomic oxygen and wave motions tothe atmospheric heating is the main goal of the rocket project WADIS (WAvepropagation and DISsipation in the middle atmosphere). It includes, amongstothers, our instruments for the measurement of atomic oxygen that have bothbeen developed with the aim of resolving density variations on small verticalscales along the trajectory. In this paper the instrument based on catalyticeffects (PHLUX: Pyrometric Heat FluxExperiment) is introduced briefly. The experiment employing solidelectrolyte sensors (FIPEX: Flux φ(Phi) Probe Experiment) is presented in detail. These sensors werelaboratory calibrated using a microwave plasma as a source of atomic oxygenin combination with mass spectrometer reference measurements. Thespectrometer was in turn calibrated for O with a method based onmethane. In order to get insight into the horizontal variability, the rocketpayload had instrument decks at both ends. Each housed several sensor headsmeasuring during both the up- and downleg of the trajectory. The WADISproject comprises two rocket flights during different geophysical conditions.Results from WADIS-1 are presented, which was successfully launched in June2013 from the And?ya Space Center, Norway. FIPEX data were sampled at100 Hz and yield atomic oxygen density profiles with a verticalresolution better than 9 m. This allows density variations to bestudied on very small spatial scales. Numerical simulations of the flow field aroundthe rocket were done at several points of the trajectory to assess theinfluence of aerodynamic effects on the measurement results. Density profilespeak at 3 × 1010 cm?3 ataltitudes of 93.6 and 96 km for the up- and downleg,respectively.
机译:中高大气能量收支主要由涉及原子氧(O)的反应决定。对这些过程进行建模需要详细了解这种氧的分布。了解原子氧和波动对大气加热的相互影响是火箭项目WADIS(在中层大气中的WA传播和耗散)的主要目标。除其他外,它还包括我们开发的用于测量原子氧的仪器,目的都是为了解决沿轨迹的小垂直尺度上的密度变化。本文简要介绍了基于催化作用的仪器(PHLUX:高温热通量实验)。详细介绍了使用固体电解质传感器的实验(FIPEX:FluxΦ(Phi)探针实验)。这些传感器在实验室中使用微波等离子体作为原子氧源并结合质谱仪参考测量进行了校准。依次用基于甲烷的方法对光谱仪进行O校准。为了深入了解水平可变性,火箭有效载荷的两端都装有仪表台。在轨迹的上下运动期间,每个传感器都装有几个传感器头。 WADIS项目包括在不同地球物理条件下的两次火箭飞行,并介绍了WADIS-1的结果,该结果已于2013年6月从挪威安迪亚航天中心成功发射。 FIPEX数据以100 Hz采样,并产生垂直分辨率优于9 m的原子氧密度分布图。这样可以在很小的空间尺度上估算出密度变化。在轨迹的几个点对火箭周围的流场进行了数值模拟,以评估空气动力学效应对测量结果的影响。上,下腿的密度剖面分别在93.6和96 km的3×10 10 cm ?3 海拔高度上讲话。

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