Thermal Environment and Aeroheating Mechanism of Protuberances on Mars Entry Capsule

IF 0.5 4区 工程技术 Q4 ENGINEERING, AEROSPACE
Mi Wenbo, Li Qi, Liang Junhong, Zhou Jingyun, Cheng Xiaoli
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引用次数: 4

Abstract

Mars has only thin atmosphere composed mainly of carbon dioxide that differs significantly from the atmosphere of Earth in terms of characteristics of reentry flows. To connect with the orbiter, the Mars entry capsule is provided with titanium pipes and other units installed on the heat-shield. These units will create significant local interaction flow on the surface of the capsule and cause additional heating on the surface of the shield during the entry of the capsule. With a view to interaction thermal environment issues for the surface of the shield, in this paper, the characteristics of protrusion interaction flow on different location of the shield were studied by means of numerical simulation. Heating mechanisms of protuberances on different location were derived by analyzing characteristic parameters such as local flow velocity, pressure, and Mach number. The results show that the interaction thermal environment of protuberances in the windward area is smaller than that of protuberances in the leeward area, mainly because subsonic flow dominates in the windward area, and the interaction is weak, while in the leeward area, the direction of flow intersects with protuberances to form a boundary layer shear flow, which results in a stronger interaction before the protuberances.
火星返回舱上凸起物的热环境与气动加热机理
火星只有稀薄的大气,主要由二氧化碳组成,在再入气流的特征上与地球大气有很大的不同。为了与轨道飞行器连接,火星进入舱配备了钛管和其他安装在隔热板上的装置。这些单元将在胶囊表面产生显著的局部相互作用流,并在进入胶囊期间在屏蔽表面造成额外的加热。针对盾构表面的相互作用热环境问题,采用数值模拟的方法研究了盾构不同位置上的突出相互作用流特性。通过分析局部流速、压力、马赫数等特征参数,推导出不同位置凸起的加热机理。结果表明:迎风区凸起的相互作用热环境小于背风区凸起,主要原因是迎风区以亚音速流为主,相互作用较弱,而在背风区,气流方向与凸起相交形成边界层剪切流,导致凸起前的相互作用较强。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
中国空间科学技术
中国空间科学技术 ENGINEERING, AEROSPACE-
CiteScore
1.80
自引率
66.70%
发文量
3141
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