C/E 复合材料“以磨代钻冶制孔工艺

为了提高C/E复合材料构件制孔加工质量,以C/E复合材料为研究对象,提出"以磨代钻"制孔新工艺,并研制了电镀金刚石刀具.与传统硬质合金刀具钻孔工艺进行对比试验,结果表明:金刚石刀具钻削轴向力降低30%-50%、刀具耐用度提高3-5倍、缺陷显著减少,更适合C/E复合材料钻孔加工.     

基于遗传算法的圆柱阵列旁瓣电平优化方法

由于共形阵列所具有的特性,使其正得到日益广泛的应用,但其方向图具有相对主瓣较高的旁瓣电平。为此,文章针对基本的共形阵列——圆柱阵列的天线阵元,应用经典遗传算法进行唯幅度的方向图综合,来优化旁瓣电平。仿真结果表明：该方法可有效降低圆柱阵列的旁瓣电平,为解决此类问题提供了有益的参考。     

基于实测数据的宽带雷达回波半实物仿真方法

自动目标识别技术的发展对雷达回波仿真的要求越来越高。分析了散射点回波叠加法和电磁散射建模回波生成法各自的优缺点,结合两种方法提出了基于实测数据的雷达回波半实物仿真方法。首先通过电磁散射建模预估目标的RCS信息,再从实测回波数据中提取目标的运动特征,从而仿真出雷达回波。该方法灵活性好、精度高、易于工程实现,仿真出的回波成像后具有较清晰的轮廓和明显的运动特征。     

一类三阶非线性系统的全局渐近稳定性

运用"类比法"对两类三阶非线性系统构造了较好的Lyapunov函数,并建立了该系统平凡解全局渐近稳定的条件.     

一次中等磁暴期间全球电离层TEC及ROTI指数变化分析

地磁暴发生时,电离层会有偏离平均水平的强烈扰动.基于全球电离层TEC及其时间变化率ROTI(Rate of TEC Index)数据,对2014年8月一次中等强度磁暴期间的全球电离层影响进行了分析,探讨了磁暴所引发电离层暴的可能机制.研究发现,本次磁暴伴随有明显的电离层暴效应.磁暴期间:南半球电离层以正相暴为主,北半球电离层暴则整体表现为短暂正相暴后长时间强的负相暴;电离层在北半球的下降比南半球强,并且这种下降持续了约一周时间;低纬区域电离层变化幅度明显小于中纬区域,高纬区域则主要表现为负暴效应;赤道北驼峰出现了明显的南移现象,直至磁赤道两侧双驼峰结构消失.对磁暴期间三个不同扇区的电离层ROTI变化的分析表明:欧洲-非洲扇区磁暴前有电离层闪烁发生,磁暴发生后消失,而东亚-澳大利亚及美洲扇区则无此现象出现.研究结果表明,此次磁暴期间的电离层变化存在明显的时间和空间差异.     

空间站的混合自适应控制

本文推导出两板空间站的连续传递矩阵左分解模型;在此基础上,建立了该空间站的一种极点配置混合自适应控制算法,通过计算机仿真验证了该算法的有效性和鲁棒性。     

The present and the future of random signal radars

The 30+ year development of random signal radar (RSR) is described in this paper. Conventional methods of implementing RSRs are summarized: correlation, spectrum analysis, and anti-correlation. Some typical RSR systems are introduced; for example: noise frequency modulation continuous wave radar; and random binary phase-coded continuous wave radar, and their merits and demerits are also pointed out. Finally, the development trends of RSR is analyzed     

标准电池滞后效应的研究

根据电极过程动力学的基本原理,推导出在不同条件下标准电池电动势的表达式。对标准电池电动势——温度滞后及充放电后电池电压的滞后效应作了较深入的研究,对引起滞后的原因给出了理论解释。从而指出滞后效应与电池内在因素(杂质、晶体盐尺寸、电池结构、活性物质等)之间的依赖关系。因此,滞后效应的大小可作为判断电池性能优劣的主要依据。     

Ultrastructural and geochemical characterization of Archean-Paleoproterozoic graphite particles: implications for recognizing traces of life in highly metamorphosed rocks

Abundant graphite particles occur in amphibolite-grade quartzite of the Archean-Paleoproterozoic Wutai Metamorphic Complex in the Wutaishan area of North China. Petrographic thin section observations suggest that the graphite particles occur within and between quartzite clasts and are heterogeneous in origin. Using HF maceration techniques, the Wutai graphite particles were extracted for further investigation. Laser Raman spectroscopic analysis of a population of extracted graphite discs indicated that they experienced a maximum metamorphic temperature of 513 +/- 50 degrees C, which is consistent with the metamorphic grade of the host rock and supports their indigenicity. Scanning and transmission electron microscopy revealed that the particles bear morphological features (such as hexagonal sheets of graphite crystals) related to metamorphism and crystal growth, but a small fraction of them (graphite discs) are characterized by a circular morphology, distinct marginal concentric folds, surficial wrinkles, and complex nanostructures. Ion microprobe analysis of individual graphite discs showed that their carbon isotope compositions range from -7.4 per thousand to -35.9 per thousand V-PDB (Vienna Pee Dee Belemnite), with an average of -20.3 per thousand, which is comparable to bulk analysis of extracted carbonaceous material. The range of their size, ultrastructures, and isotopic signatures suggests that the morphology and geochemistry of the Wutai graphite discs were overprinted by metamorphism and their ultimate carbon source probably had diverse origins that included abiotic processes. We considered both biotic and abiotic origins of the carbon source and graphite disc morphologies and cannot falsify the possibility that some circular graphite discs characterized by marginal folds and surficial wrinkles represent deflated, compressed, and subsequently graphitized organic-walled vesicles. Together with reports by other authors of acanthomorphic acritarchs from greenschist-amphibolite-grade metamorphic rocks, this study suggests that it is worthwhile to examine carbonaceous materials preserved in highly metamorphosed rocks for possible evidence of ancient life.     

伞—弹系统三体运动分析

理论上分析了末敏弹系统伞、伞盘、弹三刚体间的力学关系,考虑了系统的连接方式和约束、分析了伞绳弹性,建立了三体运动的数学模型,算例表明所描述的运动与实测运动规律和扫描特性相符,因此该模型可用于末敏弹总体和扫描装置的分析和设计。