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Reduction of rocket-borne atmospheric density measurements using Monte Carlo simulation.

机译:使用蒙特卡洛模拟减少火箭传播的大气密度测量值。

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摘要

The HEX II atmospheric rocket experiment, conducted near 9:30 U.T. February 14, 2007 from the Poker Flat Rocket Range in Alaska was designed to lead to a better understanding of density and velocity gradients in the lower thermosphere. In a supporting role to this mission, cold cathode ionization gauges recorded composite density along three rocket payload trajectory paths from 90 km to 200 km. Rocket-borne instruments experience near sonic to hypersonic velocities and encounter a range of viscous, slipflow, and collisionless flow conditions at these heights. These variable conditions necessitate the use of tailored analytic expressions appropriate to the flow conditions, requiring increasingly unacceptable levels of approximation beyond their applicable range. In contrast, Direct Monte Carlo-based simulations (DSMC) reproduce the full behaviour of a gas through direct representation of gas molecules and their kinetics by a matrix of state variables, allowing accurate prediction of evolving macroscopic gas characteristics under a wide variety of mean free path conditions.;The HEX II ion density measurements are corrected for atmospheric ram and wake effects using G.A. Bird's DSMC DS3VD software and a simulated payload in a model atmosphere. Density measurements were likewise corrected through the use of analytic expressions appropriate to either viscous or collisionless flow. The ambient atmospheric densities reduced by the DSMC simulation factors are maximum +4.5%/- 5.7% uncertain, instrument error excluded.;However, DSMC reduced ambient densities near 115 km were outside the bounds of estimated model atmosphere variation(+200%/-50%). Other sources of error, such as instrument and calibration uncertainty, must be not only identified but also accounted for to improve these results. DSMC ram reduction factors were typically only +/- 2% different from collisionless analytic factors above 120 km, wake regions excluded. Therefore, less costly analytic ram factors may be used in place of DSMC simulations for a carefully designed instrument chamber within the collisionless region, typically above 120 km.
机译:在美国东部时间9:30附近进行的HEX II大气火箭实验。 2007年2月14日从阿拉斯加的扑克平火箭范围出发,旨在使人们更好地了解低热层的密度和速度梯度。为了完成这项任务,冷阴极电离仪记录了从90 km到200 km的三个火箭有效载荷轨迹的复合密度。火箭仪器的音速接近高音速,并在这些高度遇到各种粘性,滑流和无碰撞流动条件。这些可变条件需要使用适合于流动条件的量身定制的分析表达式,要求超出其适用范围的近似水平越来越无法接受。相比之下,基于直接蒙特卡洛的模拟(DSMC)通过状态变量矩阵直接表示气体分子及其动力学,从而再现了气体的全部行为,从而可以在各种均值自由度下准确预测不断演变的宏观气体特征。 HEX II离子密度测量值使用GA校正了大气撞击和尾流影响Bird的DSMC DS3VD软件和模型环境中的模拟有效载荷。同样,通过使用适合于粘性流或无碰撞流的解析表达式来校正密度测量。 DSMC模拟因子降低的环境大气密度最大不确定性为+4.5%/-5.7%,不包括仪器误差;但是,DSMC降低的115 km附近的环境密度不在模型大气变化估计范围之内(+200%/- 50%)。不仅必须识别其他误差源,例如仪器和校准不确定性,而且还要考虑这些误差源以改善这些结果。 DSMC撞锤降低因子通常与120 km以上的无碰撞分析因子仅有+/- 2%的差异(不包括尾流区域)。因此,对于无碰撞区域(通常在120 km以上)内精心设计的仪表室,可以使用成本更低的分析夯土系数代替DSMC模拟。

著录项

  • 作者

    Gaulden, Travis Michael.;

  • 作者单位

    Clemson University.;

  • 授予单位 Clemson University.;
  • 学科 Applied Mechanics.;Atmospheric Sciences.;Aeronomy.
  • 学位 M.S.
  • 年度 2010
  • 页码 99 p.
  • 总页数 99
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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