航天器舱内气体对流换热的地面模拟试验方法

对航天器舱内气体对流换热的地面模拟试验方法进行了系统地理论分析,包括热缩比模型法、降压法和浓度比拟法三种。分别给出了各种方法的相似律或相似准则及其应用的约束条件,并从原理上定性比较这三种方法的优缺点。分析表明,热缩比模型法在保持Ｒｅｙｎｏｌｄｓ数不变的前提下可明显减弱自然对流的影响,但这种方法不能用于工程原型;降压法可用工程原型进行模拟试验,但不能用于液体流动问题;然而这两种方法的共同缺点是都不能完全消除自然对流;浓度比拟法理论上可以完全消除自然对流,但约束条件多,工程实现困难。     

微重力环境下蒸发液层热毛细对流的数值模拟

提出了一种新模型来研究由单一物质构成的液层在其纯蒸气中的蒸发.液层置于微重力环境中并且受到水平方向温度梯度的作用,液层的热毛细对流和蒸发耦合在一起,使得气液界面的传热传质规律更加复杂.用理论分析的方法求解了不考虑热毛细效应的纯蒸发模型,得出温度场分布和界面质量流量的解析表达式.对于热毛细对流和蒸发耦合情况,采用有限差分的投影算法同时求解Navier-Stokes方程和能量方程,得到了不同蒸发Biot数和Marangoni数下流场和温度场的稳态数值解.论述了蒸发Biot数和Marangoni数对界面传热传质的影响,提出并解释了蒸发和热毛细对流耦合的三种模式.      

天舟一号货运飞船空间实验装置蒸发相变地面实验

以天舟一号货运飞船为依托,开展空间蒸发相变传热规律的科学实验研究,探索重力对蒸发传热传质过程的影响规律.设计了一套地面蒸发实验平台,以蒸发相变液体FC-72为研究对象,通过红外热像仪测温、热流量计、差分热电偶等手段,观测FC-72液层在不同台面温度、注液量等情况下的相变界面变化、蒸发表面特性、流体物性及Marangoni对流涡胞的变化等,获取其蒸发两相流体的液层温度差、表面温度场、热流量值、蒸发速率和涡胞结构等.实验结果表明:在其他条件不变的情况下,FC-72液层与蒸发台面的温差越高,其蒸发速率越快;注液量越大,蒸发速率也越大;在蒸发过程中出现了浮力对流涡胞和Marangoni对流涡胞.此外,通过地面蒸发实验可以确定空间科学实验选用的实验介质和材料,进而优化确定空间科学实验的工况、参数及流程等,部分地面实验结果也将直接成为天地对比实验的科学成果.      

Two-dimensional Marangoni and buoyancy convection related to crystal growth techniques in space

The natural convection in the horizontal liquid layer driven both by surface tension gradient and buoyancy was investigated experimentally and theoretically.The fluid motion was visualized by mixing fine flakes of aluminum into the liquid. At the same time, the temperature field was visualized by the Mach-Zehnder interferometry and the local temperature gradient distributions were visualized by making use of the refraction of parallel incident light.The numerical analysis using the Galerkin method was also carried out which agreed well with the experimental results.It was found that the velocity and temperature fields of Marangoni convection were varied depending on the aspect ratio of the liquid layer and on the coupled buoyancy convection.     

Two-dimensional convection in liquid layer related to crystal growth techniques in space

In this paper, the Marangoni convection including buoyancy convection in two-dimensional fluid model was investigated experimentally and theoretically. The transparent liquid in the test cell was heated and cooled under various conditions. The fluid flow driven by surface tension and by buoyancy force was visualized and measured. The flow patterns, velocity distributions and temperature field were obtained and they were compared with the results of the numerical solutions. The effect of the configuration and the convection in microgravity on crystal growth was discussed. The temperature field of the crystallizing surface was predicted.     

Hydrothermal instability of thermocapillary convection in large-Prandtl-number liquid bridges under microgravity

Linear stability analysis was performed to study the mechanism of transition of thermocapillary convection in liquid bridges with liquid volume ratios ranging from 0.4 to 1.2, aspect ratio of 0.75 and Prandtl number of 100. 2-D governing equations were solved to obtain the steady axi-symmetric basic flow and temperature distributions. 3-D perturbation equations were discretized at the collocation grid points using the Chebyshev-collocation method. Eigenvalues and eigenfunctions were obtained by using the Q–R method.The predicted critical Marangoni numbers and critical frequencies were compared with data from space experiments. The disturbance of the temperature distribution on the free surface causes the onset of oscillatory convection. It is shown that the origin of instability is related to the hydrothermal origin for convections in large-Prandtl-number liquid bridges.     

微重力与电磁场对凝固过程的影响

欧洲空间局两项材料领域课题MICAST和CETSOL均涉及微重力科学相关研究.通过等轴晶柱状晶转变（CET）分析了微重力环境对材料凝固过程的影响;介绍了一项在地面施加行波电磁场的标准（Benchmark）凝固实验,其温度场演化及微观凝固组织和浓度偏析均展示了磁控受迫对流对金属材料凝固过程的显著作用.      

蒸发效应与热毛细对流耦合现象的实验研究

实验研究了矩形液池中蒸发薄液居中蒸发效应与热毛细对流的耦合机理. 对于单纯的热毛细对流稳定性从实验和理论上已有深入研究,但目前国际上对带有菇发界面的热毛细对流问题尚缺乏研究. 特别是近来的研究发现,气液界面的蒸发对热毛细对流稳定性有很大的影响. 本实验以温度为主要控制参数,测量了不同工况下蒸发界面不同点的蒸发速率和表层温度,并利用 PIV 方法分析得到了液体内的嘛场分布. 实验结果发现,随着沿界面的温差增加,蒸发液体内的流型从稳定的单涡胞结构变为稳定的多祸胞结构,并最终演变为紊流结构. 综合分析以上测量结果并与理论分析结果进行了比较。      

Manipulation of Colloidal Droplets in Space and the Instability of Thermocapillary Convection in Large Prandtl Number Liquid Bridge in Microgravity

In 2016 and 2017, SJ-10 and TG-2 satellites were launched. In this short paper, we report recent progress on the studies of manipulation of colloidal droplets and instability of thermocapillary convection in large Prandtl number liquid bridge that based on the space experiments boarding SJ-10 and TG-2 satellites, separately. It was shown that the colloidal droplets can be successfully formed and manipulated in microgravity through the patterned substrates. In another aspect, the coffee-ring effect was observed at the first time in space. For the studies of the instability of thermocapillary convection in large Prandtl number liquid bridge in microgravity, our experiments in TG-2 broadened the way of such kind of study and abundant experimental results are emerging.      

过冷核态池沸腾中的Marangoni效应

分析了过冷核态池沸腾过程中气泡横向运动现象,指出其成因在于相邻气泡界面温度差引起的Mara-ngoni对流对周围液体的吸引.通过对该流动的尺度分析,得到了气泡横向运动特征速度及其可观测度的估算公式,其预测结果与实验观测相一致.特别是对极细小的初始核化气泡,该公式预测了强烈的横向Marangoni对流会导致气泡顶端微射流的形成.该效应在加热面水平向下或微重力沸腾等气泡脱落频率较低的情形中尤为重要.      

微重力条件下悬浮区中的Marangoni对流

本文研究微重力条件下悬浮区中的表面张力梯度驱动对流。采用有限元方法数值研究二维、轴对称悬浮区中的定常流动和温度分布,讨论P_r数及自由面上散热条件的影响。计算表明,P_r数(M_α数)增大时,流区大部分自由表面上温度梯度减小,流区流速较小,对流热输运较扩散效应增强。只要能维持自由面上一定的温度梯度,在较大的P_r数(M_α数)时,仍能得到收敛的定常解。     

Onset of Marangoni convection in an infinite layer of an electrically conducting liquid under magnetic field

The onset of Marangoni convection in an electrically conducting liquid is studied theoretically for the case that the liquid is subjected to a vertical temperature gradient and a magnetic field with arbitrary orientation.The effects of the intensity of magnetic field, the angle of inclination of magnetic field and the Biot number at the free surface on both the critical Marangoni number and the flow pattern are made clear.     

纵向非均匀多孔介质Marangoni对流不稳定性

理论研究了纵向非均匀多孔介质中流体表面张力驱动的对流不稳定性.充满液体的多孔介质层从下方加热,上方自由表面冷却,形成可引起多孔介质液层Marangoni-Benaxd对流流动的纵向温度梯度.采用线性化的Brinkman-Forchheimier方程作为控制方程组,对孔隙率分别为线性函数、正弦三角函数分布的非均匀多孔介质液层的Marangoni-Benaxd问题进行了线性稳定性分析.通过采用Chebyshev-Tau谱方法求解广义特征值问题,得到了系统临界Maxangoni数随无量纲波数变化的中性稳定性曲线,分析和比较了孔隙率的变化对液层对流稳定性和流场结构的影响,获得了纵向非均匀多孔介质液层不稳定性现象的新特征.      

气体在矿物油中扩散现象的可视化研究

介绍了利用马赫-泽德干涉仪法实现气体-矿物油扩散过程的可视化测量的原理、作用与意义。由于运用马赫-泽德干涉仪法获得的图像干涉条纹数及其图像的形状变化与折射率n直接与液体介质折射率相关,用马赫-泽德干涉仪法可获得十分清晰的影像。在N2,O2-矿物油扩散过程中,干涉条纹式样并未发生显著的紊乱变化,表明N2与O2气体在矿物油中发生扩散后,所引起的矿物油折射率变化过程较为缓慢。在CO2-矿物油扩散过程中,由于溶解的作用,矿物油近表面层中的气体溶解度增加,导致自然对流的出现。通过可视化测量,成功地观测到这一重要实验现象。同时,利用可视化技术,还可很好地判明对流出现的时间,从而确保扩散研究的有效性。     

微重力效应的物理解释及其应用

讨论了微重力效应及其分子物理学解释，万有引力的单极性决定了它的累积性和宏观性，重力对自由分子的影响是微科其微的，然而在流钵，特别是在液体内部的具体条件下，重力对流体内部分子集团产生明显影响，以宏观的静压强形式表现出来。而当重力变小，变微，流体内部的静压强也就趋于消失，由静压强产生的二级现象，如异相沉降或浮泛。同相的浮泛对流，液体自约束成球形，也就消失，这些就是微重力的一，二级物理效应，本文认为，Bossinesq近似对于流体而言实质上是线性热力学假设或近平衡态假设，可以用初始平衡态的物性参量表征临界点时的无量纳数，提出一种重力消失诱发非平衡态向平衡态蜕变的猜想，从文中导出的瑞利数Rα的表达式可以看出，重力加速度的消失，可以使瑞利数的值从远离平衡态的湍流蜕变到稳定流动的瑞利－贝纳对流胞，甚至是没有宏观流动的平衡态，最后，将本文给出的理论解释模型应用到空间材料加工所需微重力水平的估算、窨材料加工工艺的微重力利用准则和空间装置中气体自然对流传热状态模拟的低真空和微重力的互换性方面。     

地球磁尾的电场模式

地球磁层中的电场是磁层等离子体运动的主要驱动力。目前常用的磁层电场为均匀晨昏电场和投影电场。本文假定磁力线为电场的等位线，地球电离层电场看做磁层电场沿磁力线在电离层的投影。利用Tsyganenko磁场模式（T89），沿磁力线反电离层电场投影到磁尾，得到了一个新的磁层电场模式。文中对偶极磁场和T89磁场模式下的投影场作了比较，说明本模式突破了偶极磁场的局限，在磁层有更大的适用范围。     

Physical parameters affecting living cells in space

The question is posed: Why does a living cell react to the absence of gravity? What sensors may it have? Does it note pressure, sedimentation, convection, or other parameters?

If somewhere in a liquid volume sodium ions are replaced by potassium ions, the density of the liquid changes locally: the heavier regions sink, the lighter regions rise. This may contribute to species transport, to the metabolism. Under microgravity this mechanism is strongly reduced. On the other hand, other reasons for convection like thermal and solutal interface convection are left. Do they affect species transport?

Another important effect of gravity is the hydrostatic pressure. On the macroscopic side, the pressure between our head and feet changes by 0.35 atmospheres. On the microscopic level the hydrostatic pressure on the upper half of a cell membrane is lower than on the lower half. This, by affecting the ion transport through the membrane, may change the surrounding electric potential. It has been suggested to be one of the reasons for graviperception.

Following the discussion of these and other effects possibly important in life sciences in space, an order of magnitude analysis of the residual accelerations tolerable during experiments in materials sciences is outlined. In the field of life sciences only rough estimates are available at present.     

Diurnal variations of convective cloudiness in tropical Africa observed with Meteosat ISCCP B2 data

Monthly composite images have been constructed from 8 times of the day from the ISCCP B2 Meteosat data set. Average and standard deviation images in IR and WV channels have been constructed at first. These images allow to describe the mean diurnal cycle of convection over Africa, and show that this cycle is strongly influenced by the orography. Comparisons between two very different rainy seasons in West Africa, 1983 and 1985, show some differences in the diurnal cycles.     

Marangoni convection in a liquid layer under the simultaneous action of a transverse magnetic field and rotation

Asymptotic stability characteristics with respect to the onset of Marangoni convection in a liquid layer under the simultaneous action of a large transverse magnetic field and a large rate of rotation are investigated. In certain parameter ranges there is a decrease in critical Marangoni number for increasing magnetic field and rotation depending on the coupling between interfacial perturbations and rotation.