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Mission Sizing and Trade Studies for Low Ballistic Coefficient Entry Systems to Venus

机译:低弹道系数进入金星的任务规模和贸易研究

摘要

The U.S and the U.S.S.R. have sent seventeen successful atmospheric entry missions to Venus. Past missions to Venus have utilized rigid aeroshell systems for entry. This rigid aeroshell paradigm sets performance limitations since the size of the entry vehicle is constrained by the fairing diameter of the launch vehicle. This has limited ballistic coefficients (beta) to well above 100 kg/m2 for the entry vehicles. In order to maximize the science payload and minimize the Thermal Protection System (TPS) mass, these missions have entered at very steep entry flight path angles (gamma). Due to Venus thick atmosphere and the steep-gamma, high- conditions, these entry vehicles have been exposed to very high heat flux, very high pressures and extreme decelerations (upwards of 100 g's). Deployable aeroshells avoid the launch vehicle fairing diameter constraint by expanding to a larger diameter after the launch. Due to the potentially larger wetted area, deployable aeroshells achieve lower ballistic coefficients (well below 100 kg/m2), and if they are flown at shallower flight path angles, the entry vehicle can access trajectories with far lower decelerations (~50-60 g's), peak heat fluxes (~400 W/cm2) and peak pressures. The structural and TPS mass of the shallow-gamma, low-beta deployables are lower than their steep-gamma, high-beta rigid aeroshell counterparts at larger diameters, contributing to lower areal densities and potentially higher payload mass fractions. For example, at large diameters, deployables may attain aeroshell areal densities of 10 kg/m2 as opposed to 50 kg/m2 for rigid aeroshells. However, the low-beta, shallow-gamma paradigm also raises issues, such as the possibility of skip-out during entry. The shallow-gamma could also increase the landing footprint of the vehicle. Furthermore, the deployable entry systems may be flexible, so there could be fluid-structure interaction, especially in the high altitude, low-density regimes. The need for precision in guidance, navigation and control during entry also has to be better understood. This paper investigates some of the challenges facing the design of a shallow-gamma, low-beta entry system.
机译:美国和苏联已成功向维纳斯发送了17次大气进入任务。过去对维纳斯的访问已经利用刚性航空器系统进入。由于进入飞行器的尺寸受到发射飞行器的整流罩直径的限制,因此这种刚性的机壳范例设置了性能限制。对于入门车来说,这将弹道系数(β)限制在100 kg / m2以上。为了最大化科学有效载荷并最小化热保护系统(TPS)的质量,这些任务以非常陡峭的进场飞行角(γ)进入。由于金星的大气层浓密和伽玛射线较高的高温条件,这些进入的车辆暴露于非常高的热通量,非常高的压力和极高的减速度下(超过100克)。可展开的机体通过在发射后扩大到更大的直径,从而避免了发射飞行器整流罩直径的限制。由于潜在的更大的湿润区域,可展开的机壳会获得较低的弹道系数(远低于100 kg / m2),并且如果它们以较浅的飞行角度飞行,则进入的车辆可以以较低的减速(〜50-60 g's ),峰值热通量(〜400 W / cm2)和峰值压力。浅伽玛,低β部署物的结构和TPS质量要比直径较大的陡伽玛,高β刚性航空器外壳低,从而导致较低的面密度和潜在的更高的有效载荷质量分数。例如,在大直径情况下,可展开物可达到10 kg / m2的航空器面密度,而刚性航空器的密度为50 kg / m2。但是,低beta浅伽玛范式也会引发一些问题,例如在进入过程中可能会被跳过。浅伽玛值还会增加车辆的着陆足迹。此外,可部署的进入系统可能是灵活的,因此可能存在流体-结构相互作用,尤其是在高海拔,低密度区域。还必须更好地理解进入期间对制导,导航和控制的精确性的需求。本文研究了浅伽玛,低贝塔进入系统设计所面临的一些挑战。

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