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。     

实践十号卫星蒸发对流箱地面科学实验结果分析

实践十号卫星蒸发对流实验旨在研究置于加热底板的蒸发液滴在相变过程中,表面蒸发与表面张力驱动对流的耦合机理及其不稳定性.为与空间实验结果进行对比,利用蒸发对流箱完成在轨工况的科学匹配实验,获得相应工况的地面科学数据、工程参数及实验图像.通过对地面科学匹配实验结果进行分析,得到不同工况下液滴形貌（体积、表面积、接触角、液滴高度、液滴直径）变化规律,以及液滴蒸发过程中温度、热流量、蒸发速率和蒸发流量的变化规律.依据实验结果分析研究了具有质量交换的复杂流体相变界面的热质传输规律.     

Experiments in materials science on the ground and in reduced gravity using electrostatic levitators

To counter residual accelerations, dedicated levitators or positioners are necessary to support a host of materials science experiments on the ground and in microgravity. All levitators (e.g., aerodynamic, acoustic, electromagnetic, electrostatic, optical) have their own merits and limitations but the electrostatic scheme offers the combined advantages of processing millimeter-size objects, independent heating, quasi-spherical shape of molten materials, handling of materials under extreme temperatures for hours, virtually convection-free samples, and wide view around the samples for diagnostic. These attributes provide unique research opportunities in materials science on the ground as well as under reduced gravity. In particular, electrostatic levitators are very attractive to measure the physical and structural properties of equilibrium and non-equilibrium liquids, to synthesize multi-function materials, and to understand metastable phase formation, vitrification, and diffusion. In this paper, research and development carried out by the Japan Aerospace Exploration Agency over the years in the field of electrostatic levitation are summarized and the main results obtained in materials science are presented.     

Polar ionosphere and geomagnetic response for the flux transfer events: A case study

On April 15th 2003, Cluster crossed the dayside magnetopause boundary and observed a series flux transfer events (FTEs) during the interval from 0630 to 0730 UT. During this period, the interplanetary magnetic field (IMF) showed a negative z component and a positive y component. Simultaneous corresponding transient plasma flows were identified in the near-conjugate polar ionosphere by the CUTLASS Finland HF radar, and the geomagnetic field disturbances were observed by the IMAGE ground-based magnetometers. By combing these data and applying the Cooling model, we show that the transient plasma flows and the geomagnetic field disturbances are closely related to the dayside FTEs.     

Atmospheric response to a Hot SST Event in November 2006 as observed by the AIRS instrument

Using Atmospheric Infrared Sounder (AIRS) products of atmospheric temperature and geopotential height, we investigate the atmospheric response to HE0611, which was found and investigated by [Qin, H., Kawamura, H., Sakaida, F., Ando, K. A case study of the tropical Hot Event in November 2006 (HE0611) using a geostationary meteorological satellite and the TAO/TRITON mooring array. J. Geophys. Res. 113, C08045, doi: 10.1029/2007JC004640, 2008]. HE0611 was formed by connecting two very high SST areas, HE0611-East and HE0611-West. The period-mean atmosphere temperatures at levels of 925 and 850 hPa in HE0611-West are higher, by about 0.5 K, than those in WE0611-East while the atmospheric temperatures at middle to high levels (700–300 hPa) are higher in HE0611-East. The period-mean geopotential heights HE0611-East are much lower than those in HE0611-West for the levels from the surface to 400 hPa. The mean geopotential heights from 400 hPa to 200 hPa are higher in HE0611-East. In the middle and high layers over HE0611-West, the atmosphere temperatures gradually decrease from 7th to 17th, and then increase significantly. The increase in HE0611-East starts from 15th November, which is earlier than that of HE0611-West. The geopotential heights in the high layer of both the areas also show corresponding behaviors. The lagged atmospheric response in the western part is confirmed by the correlation analysis. It emerges that the atmospheric response to HE0611 is well organized and associated with deep convention in HE0611-East and subsidence in HE0611-West. These are also consistent with the HE0611 features and evolution revealed by earlier HE studies.     

A 2-D comparison of ionospheric convection derived from SuperDARN and DMSP measurements

Ion drift vectors measured by the DMSP satellites are compared with plasma convection vectors obtained by the SuperDARN HF radars through the standard Map Potential algorithm of Ruohoniemi and Baker [Ruohoniemi, M., Baker, K.B. Large-scale imaging of high-latitude convection with super dual auroral radar network HF radar observations. J. Geophys. Res. 103, 20797–20811, 1998]. Despite significant data spread, the agreement can be qualified as reasonable for a data set comprising of 149 satellite passes over the Northern Hemisphere at high latitudes. The slope of the best-fit line relating SuperDARN and DMSP velocity magnitudes is of the order of 0.3 with a tendency for the SuperDARN velocities to be smaller. The agreement between the azimuths of the ion drift and convection is better with the slope of the best-fit line being close to 1. It is shown that consistency between the radar and satellite measurements is much better if the SuperDARN line-of-sight velocities are compared with the DMSP cross-track ion drifts for events showing slow spatial and temporal variations of the convection. If areas of strong convection changes are included into comparison, the degree of agreement deteriorates drastically. This result implies that differences in the spatial and temporal resolutions of DMSP and SuperDARN measurements are crucial factors contributing to the observed discrepancies. In addition, some differences are introduced when the SuperDARN line-of-sight velocities are filtered and reprocessed into vectors with the application of a background convection model.     

环形液池热毛细对流的线性稳定性研究

对外壁加热的环形液池热毛细对流进行了线性稳定性分析.采用Chebyshev配点法对Pr=6.8、内外径之比为0.5、深宽比A范围为0.25～1.4的数值结果进行分析,发现流动的临界状态均为振荡形式,并且随着A的增大,临界雷诺数减小,相应的临界波数与振荡频率也呈减小趋势.能量分析结果表明,小扰动与基本流相互作用项较小,表面张力在径向做功与周向做功对小扰动的动能变化起主导作用.观察三者与液池深宽比的关系,发现A=0.8时表面张力在径向做功项达到极小值,周向做功项以及小扰动与基本流相互作用项达到极大值.     

矩形微槽内FC-72的单相流动和换热实验研究

微槽换热器是解决航空电子设备元器件热控制问题的一条有效途径.以新型电子设备冷却液FC-72为工质,利用4种不同结构尺寸的矩形微槽,进行了微槽内单相流动和强迫对流换热性能实验研究;分析了工质流速、过冷度以及微槽结构等对换热性能的影响,给出了适用于层流和紊流的单相流动阻力特性实验关联式和单相强迫对流换热实验关联式,并对实验结果进行了不确定度分析.结果表明,在矩形微槽换热器中,FC-72的单相强迫对流换热能力能够满足中高强度的电子设备散热要求.      

层板内冷通道辐射换热影响

分析了层板换热过程,使用了\"去除复杂表面\"和\"无限大平板\" 等假设,给出了该假设下层板内腔辐射换热计算公式.又以一特定几何结构的层板模型为例,使用了3维流体力学计算程序求解了流-固耦合情况下的层板内部换热过程,研究了其在4种航空发动机典型工作状态下,内冷通道中的对流和辐射换热情况,得到了辐射与对流换热强度之比θ随冷气入口Re数和燃气加热功率的变化曲线,并对该曲线进行了指数拟合.建立了一套快速简捷计算层板内腔辐射状况的方法,为层板内腔换热研究是否应该忽略辐射,以及对层板冷却效果的修正,提供了一定的判断和计算依据.      

Dynamic particle accumulation structure (PAS) in half-zone liquid bridge – Reconstruction of particle motion by 3-D PTV

Three-dimensional (3-D) velocity field reconstruction of oscillatory thermocapillary convections in a half-zone liquid bridge with a radius of O (1 mm) was carried out by applying 3-D particle tracking velocimetry (PTV). Simultaneous observation of the particles suspended in the bridge by two CCD cameras was carried out by placing a small cubic beam splitter above a transparent top rod. The reconstruction of the 3-D trajectories and the velocity fields of the particles in the several types of oscillatory-flow regimes were conducted successfully for sufficiently long period without losing particle tracking. With this application the present authors conducted a series of experiments focusing upon the collapse and re-formation process of the PAS by mechanically disturbing fully developed PAS.     

热毛细对流模式转换及温度振荡特征

研究了矩形液池中由于两端温差引起的热毛细对流的温度振荡临界条件.在实验室中,设计了一个高分辨率的温度测量系统,用于实时观测并记录流体的温度.该系统主要由热电偶温度传感器、纳伏表和数据采集电脑3部分组成.得到了各种实验条件下温度振荡的临界条件,并且讨论了它与Prandtl数和Bond数之间的关系.利用flow3d软件数值模拟了微重力条件下的热毛细对流,发现了一种由于自由面变形和液层流场相互作用导致的晃荡的现象.     

Statistical survey on sawtooth events,SMCs and isolated substorms

Solar wind driving can cause a variety of different responses in the magnetosphere. Strong and steady driving during geomagnetic storms may result in sawtooth events. Strong to moderate driving may be followed by either sawtooth events or steady magnetospheric convection (SMC) events. Lower solar wind energy input typically leads to the formation of isolated non-storm substorms. This study uses superposed epoch analysis to reveal the typical properties of these three event groups as well as their similarities and differences. We use IMF and solar wind parameters, as well as ground-based indices (AL, SYM-H, ASY-H, PCN) to examine the level of solar wind driving and its response in the magnetosphere. Our results show that sawtooth events are associated with the strongest ionospheric activity. The subgroups of events during constant solar wind _EY$E_Y$ show that the key difference between the events is the average solar wind speed. Particularly, the high activity during sawtooth events is driven by high solar wind speed, while the lowest average speed during the SMCs may explain the lack of substorm activity during the steady convection periods.     

振动表面自然对流强化换热特性

基于振动影响流动换热边界层发展的思路,通过实验方法对振动条件下的自然对流换热特性进行研究.实验采用电铃谐振器作为加热膜的激振源,并利用红外测温技术对表面温度场进行了测量.结果表明:振动对自然对流的强化可提高90.7%.在等热流密度条件下,振动能量越大,换热越好;在等振动能量条件下,热流密度越小,换热越强.研究结果为强化表面自然对流换热提供了一种新思路.      

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.