首页> 外文期刊>Sadhana: Academy Proceedings in Engineering Science >Effect of micro- and elevated gravity condition on the evolution of stratification and self-pressurization in a cryogenic propellant tank
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Effect of micro- and elevated gravity condition on the evolution of stratification and self-pressurization in a cryogenic propellant tank

机译:重力条件对低温推进剂箱中分层和自加压力演化的影响

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摘要

An efficient way of handling and storing cryogenic propellant is required for future space exploration. In rocketry applications, propellants are stored at subcooled conditions in foam-insulated tanks. Any kind of heat infiltration may lead to stratification and self-pressurization of the tank. The supply of warm propellant beyond the cavitation limit to a turbo-pump is dangerous and hence additional propellant has to be loaded, which affects the payload capacity. The evolution of stratification during lift-off and accelerated conditions and coast phase will be different from those during normal ambient conditions. During lift-off the gravity value can reach up to 6g and microgravity (g) conditions at the coast phase. Hence, accurate prediction of the state of propellant at all stage is required for the successful mission planning. A multiphase axis-symmetric CFD model is developed, which can simultaneously account for heat transfer from the ambient and heat exchanges within the fluids during different gravity conditions. The results show that the self-pressurisation in microgravity condition is due to phase change rather than thermal stratification. The flow velocity will be maximum during lift-off and accelerated condition. Hence, greater self-pressurisation happens during the initial period and reduction in pressure rise rate is noticed later, which is due to turbulence of the fluid.
机译:未来的空间探索需要一种有效的处理和存储低温推进剂。在鲁莽应用中,推进剂在泡沫绝缘罐中储存在过冷条件下。任何种类的热渗透可能导致罐的分层和自加塑。向涡轮泵的空化限制提供温暖推进剂的供应是危险的,因此必须加载额外的推进剂,这影响了有效载荷容量。在剥离和加速条件和海岸阶段期间分层的演变将与正常环境条件下的分层不同。在剥离期间,重力值可以在海岸阶段达到高达6g和微匍匐(g)条件。因此,成功的任务规划需要精确预测所有阶段的推进剂状态。开发了一种多相轴对称CFD模型,其可以同时考虑在不同的重力条件下从流体内的环境和热交换器的热传递。结果表明,微匍匐条件下的自压制性是由于相变而不是热分层。在剥离和加速条件下,流速将是最大的。因此,在初始时段期间发生更大的自我压力,并且稍后会注意到压力上升速率的降低,这是由于流体的湍流。

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