基于序贯回归的小样本测试性验证试验方案

针对现有测试性验证试验方案难以实现较小样本量下满足置信水平要求的测试性评估问题,提出了基于序贯回归的小样本测试性验证试验方案。提出并证明了成败型试验序贯样本回归可行性假设;对序贯样本进行回归分析,实现了小样本下的测试性评估;建立了评估优化方案,实现了满足置信水平要求的测试性评估。实例验证表明:该方法可同时适用于有双方风险要求和置信水平要求的场合,且完所需样本量明显减少,在案例中平均减少了22.3%,最大减少了85%。      

基于通用充分性准则的测试性试验方案研究

建立了故障模式与被测单元(UUT)特性之间的关系模型,根据关系模型建立了样本集的通用充分性准则。在通用充分性准则的基础上,研究了确定试验方案的新方法,包括确定样本量和建立样本集的方法,以及相应的合格判断方法。通过实例应用说明了方法的可行性。与现有方法相比,新方法更适用于现有的指标要求情况和多参数综合试验的需求,而且建立的样本集可以覆盖UUT的重要特性。     

我国空间站安全与任务保证工作若干问题探讨

从我国空间站运营阶段对安全性、可靠性、维修性及质量保证(SRMQA)工作的需求出发,在系统分析国外载人航天安全与任务保证(SMA)工作体系的基础上,总结国际空间站安全性可靠性工作的先进经验,并针对我国空间站对航天员安全、寿命与可靠性要求更高的需求,从管理和技术应用两个方面,系统论述了我国空间站安全与任务保证应重点开展的安全性、寿命与可靠性等工作。     

Charged particles on the Earth–Jupiter–Europa spacecraft trajectory

Charged particle fluxes on the trajectory of future Russian space research mission to Jupiter and its satellite Europa are investigated. The existing experimental data and models of Jupiter’s main magnetic field and radiation belts are summarized. Preliminary results of computations of energetic particle fluxes and radiation doses for each stage of the flight are given. Special attention is paid to estimation of radiation conditions in Europa’s orbit and on its surface; influence of the satellite on spatial distribution of the fluxes of charged particles of various energies is studied.     

火星卫星的冻结轨道研究

冻结轨道是一种稳定的轨道,地球、火星、月球的卫星因引力场的南北不对称,都存在冻结轨道.由于主星体引力场的不同,它们卫星的冻结轨道也有不同的特性.地球卫星的冻结执道的偏心率非常小,对卫星遥感非常有利,国内外已有相当多的近地遥感卫星采用这种轨道.月球卫星的冻结轨道偏心率随轨道倾角的不同有很大的变化,对月球卫星冻结轨道的研究...     

基于FPGA技术的多功能接口控制卡设计

随着测试技术的不断发展,为了满足信号种类、数量繁多的测试需求,考虑实现多路接口信号的复用、处理,提出了基于FPGA技术的开关阵列,及信号采集和激励的设计方案.实现了信号的多路复用、交叉互连、采集和激励,也充分考虑到系统扩展性和性能增长能力,以及实施方案的先进性、可行性,将实用有效地满足自动化测试需求.     

论当前大学图书馆的使命

论述了在当前形势下,中国大学图书馆应重新诠释其使命，即从支持教学改革，支持科学研究，参加大学信息基础建设，保障学生信息平等方面支持高等教育的发展，以及应在支持个人的学习方面发挥自己不可替代的作用。     

飞机活动半径与飞行等时点

飞机活动半径与飞行等时点是在特殊或者紧急飞行情况下,根据飞机实际油量选定最有利的紧急备降机场,保证飞机在安全距离或者最短时间内在备降机场降落的一种紧急情况处置方法。本文通过理论分析和实例验证,提出在曲折航线飞行中,用实际飞行资料精确计算飞机活动半径和飞行等时点位置的新的计算方法。     

Broyden算法在测量沙质样品介电常数实验中的应用

针对波导取样法测量沙质样品介电常数实验中复超越方程求解问题,提出用Broyden秩1迭代算法解决.     

Ocean Tides in GRACE Monthly Averaged Gravity Fields

The GRACE mission will map the Earth's gravity fields and its variations with unprecedented accuracy during its 5-year lifetime. Unless ocean tide signals and their load upon the solid earth are removed from the GRACE data, their long period aliases obscure more subtle climate signals which GRACE aims at. In this analysis the results of Knudsen and Andersen (2002) have been verified using actual post-launch orbit parameter of the GRACE mission. The current ocean tide models are not accurate enough to correct GRACE data at harmonic degrees lower than 47. The accumulated tidal errors may affect the GRACE data up to harmonic degree 60. A study of the revised alias frequencies confirm that the ocean tide errors will not cancel in the GRACE monthly averaged temporal gravity fields. The S₂ and the K₂ terms have alias frequencies much longer than 30 days, so they remain almost unreduced in the monthly averages. Those results have been verified using a simulated 30 days GRACE orbit. The results show that the magnitudes of the monthly averaged values are slightly higher than the previous values. This may be caused by insufficient sampling to fully resolve and reduce the tidal signals at short wavelengths and close to the poles. This revised version was published online in August 2006 with corrections to the Cover Date.