会议筹备的多目标规划

针对会议筹备的三个问题即预订宾馆、会议室安排、租车问题建立优化模型。对于预订宾馆问题、建立目标函数和约束条件、利用Lingo求解,将会议室安排和租车问题的各方面因素综合考虑建立模型并求解。     

地球低纬区边缘大气密度的预测

基于NRLMSISE-00大气模型讨论日地空间环境对地球低纬度地区边缘大气密度的影响,提出预测地球低纬地区边缘大气日平均密度的简化模型法和经验法。简化模型法利用地磁活动和太阳活动的11年准周期特性,通过预测地磁活动和太阳活动的变化规律以预测地球边缘大气密度。经验法则直接利用第23个太阳活动周期的日平均密度变化曲线经过傅里叶变换处理得到日平均密度变化规律曲线,然后将曲线拟合得到不同高度下的密度昼夜波动规律,再利用预测得到的日平均密度即可计算出具体当地时间对应的密度情况。误差分析说明经验预测法比简化模型法精度更高。两种方法均具有较高的精度并且使用方便,可用于地球边缘大气密度的工程化预测计算。     

谈谈环境工程剪裁和环境试验剪裁

文章简要阐述环境工程剪裁和环境试验剪裁产生的历史背景,环境工程剪裁和环境试验剪裁的定义及其内涵;指出了环境工程剪裁的目的和任务;以表的形式列出了MIL-STD-810F和GJB 150A中相应部分的剪裁要求并进行了对比分析,指出了两标准在剪裁阐述上的不足之处;最后分析了810F前言中有关剪裁的内容和各试验方法的可剪裁程度。     

考虑燃料均衡的卫星编队队形重构技术

在卫星编队队形重构过程中,如何在实现编队整体燃料消耗较少的同时使得各子卫星燃料消耗均衡,能够有效地提高卫星编队整体的寿命。提出了一种基于虚拟中心位置可变的卫星编队队形重构新方法。该方法以虚拟中心位置为寻优变量,以首末脉冲时刻可优化的双脉冲规划作为单星轨道机动策略,将编队队形重构问题转化为混合0-1数学规划问题。仿真结果表明,该优化算法在实现整体燃料次优的同时,兼顾了各星当前的燃料剩余水平,实现了各子卫星的燃料均衡。     

基于改进Johnson-Cook模型的5083P-0铝合金动态本构关系研究

为研究5083P-0铝合金在高应变率下的力学行为及本构模型,通过RPL100材料试验机和分离式霍普金森压杆(SHPB),对5083P-0铝合金进行了准静态及应变率范围950～3000 s-1的冲击动态压缩实验.结果 显示随着应变率的增加,5083P-0铝合金的屈服强度、流动应力增加,应变硬化率减小,具有应变硬化效应,正...     

体表电位标测系统中关键技术——心电信号数据高速采集

心电信号的数据采集是体表标测系统中关键技术之一。文中提出了128通道高性能体表标测系统中心电信号数据采集的VxD算法，在Wind9x系统下利用VxD技术、锁定内存和临界资源互斥访问算法相结合，实现了心电数据高速实时采集。该软件充分利用了硬件的等待时间，具有实时性高，运行速度快占内存少的特点。该软件在VtoolsD开发平台上用VisualC＋＋开发。     

日食对低纬地区f0F2和ICF的影响

研究了１９９５年１０月２４日日食过程中,我国低纬地区广州和海口的Ｆ２层临界频率ｆ０Ｆ２的高干扰重心频率ＩＣＦ变化过程,鉴于多次日 处低纬的两地ｆ０Ｆ２的日食变化形态不完全一样,以及多次日食期间同一地方ｆ０Ｆ２变化形态不完全一样,ＩＣＦ也并不像预想的那样降低,因而对于低纬电离层,动力学过程可能要比直接与太阳辐射有关的光化学过程起更为重要的作用。     

玉树地震前的电离层异常现象分析

分析了玉树地震前地基电离层探测临界频率、GPS TEC和卫星探测原位等离子体参量等多个参数的扰动变化信息, 研究了不同高度异常变化的时空关联性. 分析发现, 在地震前一天的4月13日, 多个电离层参量出现同步扰动异常, 电离层临界频率f₀F₂异常相对滑动中值增大40%, 异常空间上存在从震中东南向西南漂移的特性; GPS TEC异常增强15TECU (1TECU=1016m-2)左右, 分布于震中南部经度15°范围内, 且有明显的磁共轭效应; DEMETER观测的原位氧离子密度N_i(O+) 4月13日为1-4月中最强的一天, 异常分布偏向赤道区, 但仅局限在30°-50°左右的经度范围内. 综合三个参量的异常特征发现, 无论是空间的局地性还是时间上的密切关联均反映这次电离层扰动可能与玉树地震孕育有关. 结合其他观测信息, 进一步探讨了这次地震孕育过程的地震电离层耦合机理.      

Observations of non-migrating tides and ionospheric perturbations of O(D) airglow by ISUAL instrument

In this paper, we present the spatial variations of O(¹D) airglow observed by the ISUAL (Imager of Sprites and Upper Atmospheric Lightning) instrument on board the FORMOSAT-2 satellite. With a CCD camera and a 630 nm filter, ISUAL can measure global atmospheric emissions lying between the heights of 80 and 300 km. In days of 3–6 September 2008 and 25–27 February 2009, ISUAL has measured the emissions of O(¹D) airglow with results showing strong longitudinal peak-3 and peak-4 structures. The Lomb-Scargle analyses for these two cases show periods of longitudes of 120° and 90° supporting the DE2 and DE3 non-migrating tides. The 630 nm emissions are enhanced in equatorial regions and are lying along the equator. Over Africa its intensity can sometimes increase up to 80% relative to other longitudes. The perturbation is so strong that non-migrating tides are erased. A case of bimodal distribution with strong emissions at latitudes in equator and mid-latitude in geographic coordinates was observed.     

Low latitude nighttime ionospheric vertical E × B drifts at African region

The nighttime vertical E × B drifts velocities of the F2-region were inferred from the hourly hmF2 values obtained from ionosonde data over an African equatorial station, Ilorin (8.50^oN, 4.68^oE; dip lat. 2.95^o) during period of low solar activity. For each season, the plasma drift Vz is characterized by an evening upward enhancement, then by a downward reversal at 1900 LT till around 0000 LT, except for June solstice. This was explained using the Rayleigh–Taylor (R-T) instability mechanism. The occasional drift differences in Vz obtained by inferred and direct measurement over Ilorin and Jicamarca, respectively are reflective of the importance of chemistry and divergent transport system due to both the E region electric and magnetic fields instead of simple motions. The pre-reversal enhancement (PRE) magnitude is higher during the equinoctial months than the solsticial months over Jicamarca, highest during December solstice and the equinoctial months over Ilorin, suggesting the dominance of higher E × B fountain during equinoxes at both stations. The lowest PRE magnitude was in June solstice. The appearance of post-noon peak in NmF2 around 1700 LT is highest during the equinoctial months and lowest during the solsticial period. A general sharp drop in NmF2 around 1800 LT is distinct immediately after sunset, lowest during June solstice and highest in March equinox. Our result suggests that between 0930 and 2100 LT, the general theory that vertical drifts obtained by digisonde measurements only match the E × B drift if the F layer is higher than 300 km is reliable, but does not hold for the nighttime period of 2200–0600 LT under condition of solar minima. Hence, the condition may not be sufficient for the representation of vertical plasma drift at nighttime during solar minima. This assertion may still be tentative, as more equatorial stations needed to be studied for better confirmation.