涡轮叶片气膜冷却的研究

本文针对涡轮叶片离散气膜孔结构及叶片表面具有不同曲率的特点 ,采用传质比拟、数值计算及可视化技术 ,通过比较平板、弯曲壁面及涡轮叶片的气膜冷却流动及传热特性 ,系统地研究了离散孔三维效应、壁面曲率及压力梯度诸因素对叶片气膜冷却的影响。在此基础上 ,提出了估算叶片头部、中弧区及尾缘气膜冷却有效温比的准则公式、实验曲线及计算机程序     

The Plasma Environment of Comet 67P/Churyumov-Gerasimenko Throughout the Rosetta Main Mission

The plasma environment of comet 67P/Churyumov-Gerasimenko, the Rosetta mission target comet, is explored over a range of heliocentric distances throughout the mission: 3.25 AU (Rosetta instruments on), 2.7 AU (Lander down), 2.0 AU, and 1.3 AU (perihelion). Because of the large range of gas production rates, we have used both a fluid-based magnetohydrodynamic (MHD) model as well as a semi-kinetic hybrid particle model to study the plasma distribution. We describe the variation in plasma environs over the mission as well as the differences between the two modeling approaches under different conditions. In addition, we present results from a field aligned, two-stream transport electron model of the suprathermal electron flux when the comet is near perihelion.     

无任何附加假设的梁的自由振动

本文不采用平面假设来研究梁的弯曲自由振动，也不采用剪切型振动假设研究短粗梁的自由振动，而用弹性力学的位移法导出了梁的自由振动微分方程，并推导了简支梁的自振频率的统一公式，其特殊情况即为有附加假设的自振频率公式。     

高强驻波声场中的湍流

反射端声压级高于140dB以后驻波管中的声流结构会发生明显变化。利用流动显示和LDV（Laser Doppler Velocimetry）技术对该问题进行了实验研究。流动显示结果表明，在160dB左右的高强驻波声场中随着旋涡结构的合并、破裂等现象的出现，声致流动有明显的湍流特性。LDV测量结果显示，随着驻波管中声压级的提高，一些测点的速度频谱明显加宽，出现高频速度脉动，而另一些点的速度频谱则没有显著变化。径向湍流强度测量结果显示，此时管中流动已是复杂的三维结构,而非轴对称的二维结构。     

Ku波段波导扫频双六端口网络分析仪

介绍研制的一种实用Ku波段扫频双六端口网络分析仪。该仪器能同时测量双口网络的4个散射参数及单口网络的复反射系数。     

柱面菲涅耳太阳聚光透镜的光学设计和光学效率

研究了柱面线聚焦菲涅耳太阳聚光透镜的光学设计和光学效率。依据理论分析，对透镜参数进行了优化设计，成功地研制出了柱面线聚焦菲涅耳聚光透镜。还分析了透镜相对孔径（F数）和成型模具等因素对透镜光学效率的影响。     

热沉温度场仿真研究

为了确定热沉温度场控制方法，建立了KM6热沉正常运行状态的数学模型，在MATRIX仿真平台上构造了仿真模型并求解，确定了KM6热沉温度场的动态特性和等价模型，并对热沉的设计提出了若干建议。     

液氢贮箱停放过程中的力热分析

为了寻找到运载火箭长时间停放过程中液氢贮箱的最经济液位，用于制定合理的发射流程以及紧急处置方法，采用计算流体力学(CFD)技术，对某型运载火箭停放期间液氢贮箱的力、热情况进行了仿真计算和分析。计算选用了VOF(Volume-of-fluid)两相流模型以及Lee相变模型，为了提高Lee模型在不同压力情况下对相变过程的模拟精度，采用安托因方程修正了该模型。修正后的模型首先由试验数据校验了其精确性，随后开展的液氢贮箱停放过程仿真结果表明：贮箱的竖直方向与径向均存在温度分层的现象，液相内会形成大的漩涡，该漩涡会使得冷热流体不断进行热交换，并导致贮箱内部的液氢出现气化。贮箱停放期间蒸发率最大值超过2 m 3/h，发生在停放4 h左右；而贮箱液位充填至37 m 3以上或17 m 3以下时蒸发率较低，最小值接近1 m 3/h。     

Evaluation and improvement of coastal GNSS reflectometry sea level variations from existing GNSS stations in Taiwan

Global sea level rise due to an increasingly warmer climate has begun to induce hazards, adversely affecting the lives and properties of people residing in low-lying coastal regions and islands. Therefore, it is important to monitor and understand variations in coastal sea level covering offshore regions. Signal-to-noise ratio (SNR) data of Global Navigation Satellite System (GNSS) have been successfully used to robustly derive sea level heights (SLHs). In Taiwan, there are a number of continuously operating GNSS stations, not originally installed for sea level monitoring. They were established in harbors or near coastal regions for monitoring land motion. This study utilizes existing SNR data from three GNSS stations (Kaohsiung, Suao, and TaiCOAST) in Taiwan to compute SLHs with two methods, namely, Lomb–Scargle Periodogram (LSP)-only, and LSP aided with tidal harmonic analysis developed in this study. The results of both methods are compared with co-located or nearby tide gauge records. Due to the poor quality of SNR data, the worst accuracy of SLHs derived from traditional LSP-only method exceeds 1?m at the TaiCOAST station. With our procedure, the standard deviations (STDs) of difference between GNSS-derived SLHs and tide gauge records in Kaohsiung and Suao stations decreased to 10?cm and the results show excellent agreement with tide gauge derived relative sea level records, with STD of differences of 7?cm and correlation coefficient of 0.96. In addition, the absolute GNSS-R sea level trend in Kaohsiung during 2006–2011 agrees well with that derived from satellite altimetry. We conclude that the coastal GNSS stations in Taiwan have the potential of monitoring absolute coastal sea level change accurately when our proposed methodology is used.     

Ionospheric F2-Layer critical frequency retrieved from COSMIC radio occultation: A statistical comparison with measurements from a meridional ionosonde chain over Southeast Asia

In this paper, we compared the F2-Layer critical frequency (foF2) derived from FORMOSAT-3/COSMIC radio occultation (RO) and ionosondes at Chiang Mai, Chumphon and Kototabang during the years 2008–2015 to evaluate the performance of COSMIC RO over Southeast Asia region. The results show that the time development of foF2 values derived from COSMIC RO generally agrees well with those from ionosonde measurements. However, the differences between the foF2 derived from COSMIC RO and that derived from ionosonde observations display latitudinal dependence. COSMIC RO tends to underestimate foF2 at Chiang Mai and Kototabang, which is near to the north EIA crest and the south one, respectively, while a little overestimate foF2 at Chumphon, which is close to the geomagnetic equator. COSMIC RO agrees best with ionosonde at Chumphon and worst at Chiang Mai. At each ionosonde station, the quality of COSMIC RO data degrades with the increase of solar activity. In addition, at the station Chiang Mai and Kototabang, COSMIC RO performs better in summer than in equinox and winter. Furthermore, the differences in foF2 derived from COSMIC RO and that from ionosonde measurements vary with local time, i.e., the differences in foF2 are generally smaller at night and larger in noontime when equatorial ionization anomaly (EIA) is well developed.