粒子图像技术测量带尾缘吹气静子尾迹特征

采用粒子图像测试技术(PIV Particle Image Velocimetry)和热线相结合的方法,对静子尾缘有无吹气条件下尾迹区流场进行测量,得到了不同尾部吹气量下的静子尾迹区的流场,通过测量得到了尾迹区的流动显示、速度矢量图和涡量图,并根据无动量亏损厚度确定了纯尾迹、弱尾迹、无动量亏损尾迹和射流四种尾迹流动特征。同时对PIV测试结果和热线测试结果进行了对比,两个实验结果比较吻合,验证了PIV实验的准确性,实验结果认为无动量亏损尾迹区与纯尾迹流动相比具有速度周向变化小和脉动小等特点。     

Effective non-vertical and apparent cutoff rigidities for a cosmic ray latitude survey from Antarctica to Italy in minimum of solar activity

In this paper we will report the results of the computation of cutoff rigidities of vertical and non-vertical incident cosmic ray particles. Non-vertical effective cutoff rigidities have been computed by tracing particle trajectories through the “real” geomagnetic magnetic field comprising the International Geomagnetic Reference Field model (IGRF95, IAGA Division 5 Working Group 8, 1996: Sabaka, T.J., Langel, R.A., Baldwin, R.T., Conrad, J.A. The geomagnetic field, 1900–1995, including the large scale fields from magnetospheric sources and NASA candidate models for the 1995 IGRF revision. J. Geomag. Geoelect. 49, 157–206, 1997.) and the Tsyganenko [Tsyganenko, N.A. A magnetospheric magnetic field model with a warped tail current sheet. Planet. Space Sci. 37, 5–20, 1989.] magnetosphere model. The computation have been done for the backward route (from Antarctica to Italy) of the Italian Antarctic ship survey 1996–1997, for geographic points corresponding to the daily average coordinates of the ship; for zenith angles 15°, 30°, 45° and 60°, and azimuth angles from 0° to 360° in steps of 45°. By means of the obtained non-vertical cutoffs the apparent cutoff rigidities have been calculated. The information on integral multiplicities of secondary neutrons detected by the neutron monitor in dependence of the zenith angle of incoming primary cosmic ray particles have also been used. This information is based on the theoretical calculations of meson-nuclear cascades of primary protons with different rigidities arriving to the Earth’s atmosphere at the zenith angles of 0°, 15°, 30°, 45°, 60° and 75°. The difference between the computed apparent and vertical cutoff rigidities reaches ∼1 GV at rigidities >7–8 GV. At rigidities of 10–16 GV, the difference between the apparent and vertical cutoff rigidities is larger than that obtained earlier by Clem et al. [Clem, J.M., Bieber, J.W., Duldig, M., Evenson, P., Hall, D., Humble, J.E. Contribution of obliquely incident particles to neutron monitor counting rate. J. Geophys. Res. 102, 26919–26926, 1997.] and Dorman et al. [Dorman, L.I., Villoresi, G., Iucci, N., Parisi, M., Tyasto, M.I., Danilova, O.A., Ptitsyna, N.G. Cosmic ray survey to Antarctica and coupling functions for neutron component near solar minimum (1996–1997), 3. Geomagnetic effects and coupling functions. J. Geophys. Res. 105, 21047–21056, 2000.].     

Multi-rover navigation on the lunar surface

The paper presents a method of determination an accurate position of a target (rover, immobile sensor, astronaut) on surface of the Moon or other celestial body devoid of navigation infrastructure (like Global Positioning System), by using a group of self-calibrating rovers, which serves as mobile reference points. The rovers are equipped with low-precision clocks synchronized by external broadcasting signal, to measure the moments of receiving radio signals sent by localized target. Based on the registered times, distances between transmitter and receivers installed on beacons are calculated. Each rover determines and corrects its own absolute position and orientation by using odometry navigation and measurements of relative distances and angles to other mobile reference points. Accuracy of navigation has been improved by the use of a calibration algorithm based on the extended Kalman filter, which uses internal encoder readings as inputs and relative measurements of distances and orientations between beacons as feedback information. The key idea in obtaining reliable values of absolute position and orientation of beacons is to first calibrate one of the rovers, using the remaining ones as reference points and then allow the whole group to move together and calibrate all the rovers in-motion. We consider a number of cases, in which basic modeling parameters such as terrain roughness, formation size and shape as well as availability of distance and angle measurements are varied.     

半球功率输入和高纬电离层电导

综述和介绍了由TIROS—NOAA系列卫星资料制定高纬沉降粒子能流和电离层积分电导经验模式的方法,绘制了不同粒子沉降活动的Pedersen和Hall电导在磁纬-磁地方时坐标内的等值线分布图．同时给出了不同季节内受太阳电磁辐射控制的电导等值线分布．具体地分析了电导经验模式与磁层-电离层耦合过程的内在联系。     

某控制组合电磁发射超标分析及解决方案

本文针对电磁兼容测试中,传导发射和辐射发射超过标准限值要求问题,首先介绍了发射超标主要原因,继而梳理超标定位方法和常用电磁兼容加固措施。并以某控制组合为例,应用上述方法制定排查方案,完成电磁发射测试超标问题的干扰定位;并针对干扰源,使用线缆添加屏蔽层、电源端口添加滤波器等加固措施,经验证,措施有效,发射明显降低。同时,本文所述排查方法和加固措施,可为后续电子产品电磁兼容性设计和通过测试提供参考。     

存在初始引导场情况下的无碰撞磁场重联

采用二维三分量的全粒子模拟方法研究了不同初始引导场情况下的无碰撞磁场重联及初态为一维的Harris电流片.结果表明,Bz0＞0.5B0的强引导场不仅会显著改变粒子的运动轨迹,而且会改变重联区附近的电场和流场结构,从而影响重联率和电子加速.运用广义欧姆定律解释了不同引导场下电场的结构特征.另外,通过对扩散区附近束流电子的跟踪研究发现,在二维模型中,不论引导场强弱,位于扩散区中心垂直模拟平面的感应电场对电子加速起主要作用,而扩散区外平面电场的贡献很小.      

大功率高频无线电波对赤道E区双流不稳定性的影响--PIC静电粒子模拟研究

地面入射的大功率高频无线电波(泵波)和电离层等离子体之间的参数相互作用，能够引起静电波的激发，在一定条件下，产生不稳定性．本文用PIC静电粒子模拟方法，研究泵波与赤道电离层E区等离子体的相互作用．研究结果表明，泵波能够控制双流不稳定性的发生，在不同条件下，泵波对双流不稳定性起着稳定与不稳作用，模拟结果定性地与理论研究结果相符合，这为我们对不规则体产生的地面人工控制提供了依据．     

空间机动目标的跟踪和定位

轨道机动控制过程中，推力加速度的不确定性是机动目标运动的主项摄动。通过对推力加速度和机动目标运动建模，在地心惯性系建立了增广系统状态动力学模型，在地平测量坐标系建立了离散量测模型，同时讨论了机动目标增广状态非线性动力学模型的线性化问题。给出了扩展卡尔曼滤波实时估计增广状态向量的算法，仿真分析证明所述算法稳定、收敛，对机动目标具有较高的定位精度。     

基于激光反射层析法的换能器声场测量技术及仿真研究

换能器的辐射声场分布能够直接反映出换能器声学性能的好坏,若不能精确测量出换能器的辐射声场,则会对换能器的诊断和评估造成严重影响。从理论仿真的角度出发,推导了运用激光反射层析法重建换能器辐射声场的理论公式,着重利用推导出的理论公式对激光反射层析法进行了仿真计算。结果表明激光反射层析法能够精确地重建出换能器的辐射声场分布及声场中的声压量值,这为换能器的声场重建及声压测量提供了一种可行的方法。     

某控制组合电磁发射超标分析及解决方案

本文针对电磁兼容测试中,传导发射和辐射发射超过标准限值要求问题,首先介绍了发射超标主要原因,继而梳理超标定位方法和常用电磁兼容加固措施。并以某控制组合为例,应用上述方法制定排查方案,完成电磁发射测试超标问题的干扰定位;并针对干扰源,使用线缆添加屏蔽层、电源端口添加滤波器等加固措施,经验证,措施有效,发射明显降低。同时,本文所述排查方法和加固措施,可为后续电子产品电磁兼容性设计和通过测试提供参考。