压力畸变对涡扇发动机稳定性影响的试验

为了评定涡扇发动机在稳态工作时的抗压力畸变能力，采用可调畸变速度的发动机进口压力畸变模拟器，在发动机地面静止试车台上进行了不同进气畸变度下的整机抗畸变试验，试验中获得了发动机重要参数随不同畸变度的变化数据，并得到了发动机能稳定工作的最大进气畸变度范围。     

不同部件对机翼摇滚特性影响的风洞试验研究

简要介绍了机翼摇滚低速风洞试验技术研究，对试验装置、试验方法、数据采集等进行了描述。重点讨论了不同部件对机翼摇滚特性影响的风洞试验研究结果，结果表明：机翼摇滚是不依赖于初始滚转角的滚摆现象，出现机翼摇滚现象的超始迎角在滚转阻尼导数反号处；飞机不同布局以及不同部件对机翼摇滚特性有显著影响。     

二次时效处理对Ti40合金力学性能的影响

研究了四种不同二次时效热处理制度对β型阻燃钛合金Ti40力学性能的影响,并分析合金的微观组织.结果表明,延长550℃时效保温时间,合金塑性降低明显;时效温度从550℃提高到700℃,对塑性影响较大,特别是热暴露后的塑性降低较快;对相的分析表明其原因主要是时效时间的延长和温度的提高都会增加Ti5Si3相的析出与长大;但延长时效时间和提高时效温度可以有效提高材料的持久性能.     

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.     

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。     

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.