导弹热分离环境下发动机壳体温度分布研究

用数值模拟的方法对多级导弹间分离时发动机壳体前后封头的温度分布进行了预示。流场计算采用Ｇｏｄｕｎｏｖ格式求争非常定轴对称Ｅｕｌｅｒ方程组；针对物理域比较复杂，采用了区域重叠的分区算法；热流计算考虑了燃气射流中Ａｌ２Ｏ３粒子含量在驻点区引起的热增量，结果表明：对于前封头，由于含有Ａｌ２Ｏ３粒子而经起的驻点区热增量因子４－６，计算得到的最大热流与实测热流接近；对于后封头，不需采用驻点区热增量模型进行     

再入航天飞机表面热流密度辨识

本文给出了求解表面热流密度辨识这一热传导逆问题的顺序函数法。然后以某模型航天飞机迎风中心线上的某特征点为例，将航天飞机再入时的表面热流密度辨识问题简化为一维模型问题，用顺序函数法来对该特征点上的对流加热流密度进行了仿真辨识，得到了较理想的辨识结果。该方法在航天研究领域有着良好的工程应用前景。     

N2O4／UDMH火球特性的实验与理论研究

本文对液体推进剂四氧化二氮／偏二甲肼（Ｎ２Ｏ４／ＵＤＭＨ）爆炸热过程特性进行了实验与理论研究。研究结果显示出了火球尺寸变化、火球持续时间、火球内部温度、火球辐射热流传递过程等热过程特性参数随推进剂重量、时间和空间位置的变化规律。理论预测结果与实验测量结果相比符合较好，表明理论预测模型的正确性。本文还讨论了火球升离地面的临界条件、高空环境对火球直径的影响和火球随风漂移等三方面的问题。     

大型固体发动机旋转试车头部热防护工程分析

介绍了与ＬＭ－２Ｆ运载火箭配套的固体近地点变轨发动机的结构参数和在地面旋转试车时出现的头部烧穿故障。     

带环向槽环路热管主芯中流动和传热的数学模型和数值模拟

蒸发器是环路热管中最重要的部件,蒸发器主芯中的流场是设计中关注的焦点。建立了一个轴对称二维数学模型来模拟流体工质在圆柱形蒸发器主芯中的流动、传热和蒸发现象。模型充分考虑了流场和蒸发界面间相互作用对于蒸发界面的位置和孔隙中弯曲液面曲率半径的影响。模拟了瞬态和稳态流场,并研究了热负荷的影响。模拟结果在一定工况下是合理的。     

具有吸附性的平板型轨道分子屏离轴区域真空特性的研究

轨道分子屏真空系统,是利用分子屏轨道飞行速度远大于轨道环境大气的平均热运动速度,使空间环境对分子屏产生理想的抽速,在尾部形成气体分子的稀化区,达到极高真空.对平板型轨道分子屏,现有的文献中,仅仅计算了沿对称轴线的压力分布,然而,由于实际的分子屏试验,试件是具有一定尺寸的三维物体。仅仅获得对称轴线上的真空信息是不够的,需要对偏离对称轴线的空间点,进行分析计算.文章针对具有吸附性的平板型轨道分子屏,对偏离对称轴线的压力分布计算,提出了一套计算方法,对500km 的轨道高度,计算结果表明:当考察点与分子屏表面的距离(=|Z0|)小于1.0m,偏离对称轴线的距离小于1.6m 时,真空度维持在优于10~(-10)Pa 的数量级。建议在这一尺度范围进行材料试验。     

星载电子设备的热设计

介绍了星载电子设备的温升控制的各种方法，除了采用导热、热辐射设计外，还采用了热管的高效传热的方法。     

热管辐射器设计,试验及其在通信广播卫星上的应用

首先介绍了热管辐射器的计算及优化设计的理论。制作了两个铝蜂窝板热管辐射器单元试件，一个是热管预埋的，一个是热管外贴的。通过试验比较了这两种形式辐射器，并验证了理论计算。还介绍了用于广播通信卫星行波管散热用热管辐射器的设计及太阳模拟热平衡试验结果。     

Mercury: can any ice exist at subpolar regions?

The heat transfer in a regolith subsurface layer of thickness 20 m has been theoretically simulated for the areas near Mercury's north pole aiming at the clarification of the possible existence of subsurface ice formations of different form. The paper considers different models of the icy regolith structure and composition: pure uniform amorphous ice; a porous dispersive system with ice-filled pores and voids; permafrost. For comparison the heat transfer in dry iceless regolith has been considered as well. It has been shown that the line of maximum distribution of subsurface icy formations depends on the icy regolith model, but for any one in the “hot” regions it does not go below 70°. For the “cool” regions this line has been shown to go from 5° to 10° southward than that for the “hot” ones. The possible thickness of icy regolith near the pole has been estimated for different models assuming an interior heat flow of 15 mW m⁻². It has been shown that the maximum thickness of this layer takes place at the pole and is equal to 10 km for any model.     

Analysis on capabilities of density-based solvers within OpenFOAM to distinguish aerothermal variables in difusion boundary layer

Open source feld operation and manipulation（OpenFOAM）is one of the most prevalent open source computational fluid dynamics（CFD）software.It is very convenient for researchers to develop their own codes based on the class library toolbox within OpenFOAM.In recent years,several density-based solvers within OpenFOAM for supersonic/hypersonic compressible flow are coming up.Although the capabilities of these solvers to capture shock wave have already been verifed by some researchers,these solvers still need to be validated comprehensively as commercial CFD software.In boundary layer where diffusion is the dominant transportation manner,the convective discrete schemes＇capability to capture aerothermal variables,such as temperature and heat flux,is different from each other due to their own numerical dissipative characteristics and from viewpoint of this capability,these compressible solvers within OpenFOAM can be validated further.In this paper,frstly,the organizational architecture of density-based solvers within OpenFOAM is analyzed.Then,from the viewpoint of the capability to capture aerothermal variables,the numerical results of several typical geometrical felds predicted by these solvers are compared with both the outcome obtained from the commercial software Fastran and the experimental data.During the computing process,the Roe,AUSM＋（Advection Upstream Splitting Method）,and HLLC（Harten-Lax-van Leer-Contact）convective discrete schemes of which the spatial accuracy is 1st and 2nd order are utilized,respectively.The compared results show that the aerothermal variables are in agreement with results generated by Fastran and the experimental data even if the1st order spatial precision is implemented.Overall,the accuracy of these density-based solvers can meet the requirement of engineering and scientifc problems to capture aerothermal variables in diffusion boundary layer.