低空目标电波折射修正中地球半径计算方法

在防御体系中雷达对低空目标一般呈俯视状况,因此在电波折射修正中必须把地球视为椭球,而不能视为圆球体,否则会产生很大误差.本文通过雷达测量参数和大地坐标与空间坐标的转换,给出了计算雷达电波射线上任意一点对应地球半径的方法.     

高效砂轮的在线检测

硬质氮化硼磨料在很多加工场合可经济地代替常用的金刚砂，碳化硅等磨料，在加工过程中可显著提高生产率。但如何高效获得周转和平面理想的磨削结果，本文叙述的测量砂轮径跳的方法可达到其目的。     

一种安全的身份认证模型的研究与实现

研究分析了Radius身份认证协议,就其在安全性方面的不足给出了解决办法,同时根据给出的解决方案构建一种身份认证模型,最后对新构建的模型进行安全性分析,通过实例证明该模型是安全的、可靠的、实现简单的、并具有很强的实用价值。     

Simulation software for the spiral trajectory of our Moon

At 4.56 Ga, the accretion of the slowly rotating Solar Nebula led to the formation of Sun and its Planets in the plane of disc of accretion. Moon was formed by accretion from a circumterrestrial disk of debris generated by the glancing angle impact of the young Earth by a Mars size planetary embryo at about 4.5 Ga at a distance of 15,000 km. The Moon since then has migrated to the present position of 384,400 km from the center of the Earth. In course of this outward migration it has slowed down the spin rate of Earth and caused the lengthening of diurnal day length from 5 h initially to 24 h presently. The basic mechanics of Earth–Moon System has been worked out and theoretical determination of lengthening of day curve is carried out. This theoretical lengthening of day curve is compared with the observed lengthening of day curve based on paleobotanical evidences, ancient tidalites and Australian Banded Iron Formation. There is a remarkable correspondence between the two curves except for intermittent deviations due to geographical and geophysical factors. Based on the theoretical curve of lengthening of day, an empirical formula for the lunar orbital radius expansion is determined. Based on this empirical formula, simulation software is developed that gives the correct evolution of the semi-major axis (a) of our Moon for any time span from the inception to the time chosen under study. For mathematical simplicity the system is considered to be a two body rotating system throughout its evolutionary history of 4.5 Gyrs. This simulation draws the Moon’s spiral trajectory from its inception to any subsequent epoch. The terminal epoch is an input to the simulation software to arrive at the spiral trajectory of the Moon from the inception to the given epoch. The basic mechanics of Earth–Moon System and this simulation can be generalized to lay the foundation of simulation software for any Planet–Satellite pair or any Sun-Planet pair in our Solar System or Star-Planet pair in any Extra-Solar System. The basic dynamics has been found to be valid for Star–Planet pair also. So this Simulation Methodology can as well be applied to study the migratory evolution of Gas Giants also.     

精密离心机半径值动态测试系统

精密离心机半径值动态测试系统采用量块法测量其静态半径值，与动态下利用线位移传感器组件测量其微位移量之和的方法相比较，其工作半径值测量的相对误差达３．３×１０￣（－６）。对静态半径测量所采用的量块法及动态下采用线位移传感器组件测量补偿量的原理、方法、数据处理及误差分析进行了详细论述。此法可推广应用到其他类似的大量程动态测试系统中。     

考虑半径补偿的三坐标测量数据精确配准方法

叶片模型的配准定位是叶片形状检测分析的一个核心环节,针对涡轮叶片的三坐标测量数据在基于迭代最近点的配准定位中与CAD模型表面点的配准关系不对应的问题,提出一种考虑半径补偿的精确配准方法。在求取配准点集的过程当中考虑到半径补偿,使得测量点集与待配准点集之间的关系相对应,进而获取更高的配准精度。进行基于仿真数据的配准试验及对比,给出了基于实测数据的应用与分析,验证了该方法的精确性与实用性。结果表明,考虑半径补偿的三坐标测量数据精确配准方法是可行的。     

转台离心机动态半径测试方法的研究

精确测量离心机动态半径长度是离心机研制工作的关键和难点。根据动态测试理论要求与离心机的实际情况,提出了一种对线加速度模拟转台离心机动态半径进行测量的新方法。该方法选择了两个电容传感器,一个测量径向变化,一个测量轴向变化,组成双通道测量系统。介绍了该系统的数据采集与传输方法,论证了动态测试原理及其实验过程。实验结果证明,该系统对于动态测量范围可达到200μm,动态重复测量误差达到±0.5μm。此法可推广应用到其它类似的动态测试系统中。