航空发动机减速器轴系零件的强度可靠性计算方法

以古德曼（Ｇｏｏｄｍａｎ）应力线图和第四强度理论为基础,提出了等效高、低周复合循环应力的方法。采用蒙特卡罗（ＭｏｎｔｅＣａｒｌｏ）法对应力和强度进行了统计模拟,同时拟合了应力和强度的分布规律。运用应力－强度干涉模型,提出了评估轴在单一工作状态和多工作状态下,屈服、破坏和疲劳强度的可靠度计算方法,并编制了计算机程序。计算实例表明,该方法是令人满意的。     

旋翼表面非定常压力脉动计算的三维自由尾迹非定常面元法

利用最新发展的高分辨率三维自由尾迹非定常面元方法计算多叶片直升机旋翼的三维非定常气动力，将风洞实验数据与旋翼在悬停和出现严重桨涡干扰的低速前飞下滑状态下的计算结果进行了比较，在悬停时，还与欧拉方法的结果进行了比较，本方法与欧拉方法的结果以及风洞实验结果都吻合很好。     

复杂外形飞机绕流数值模拟研究

飞机复杂外形的绕流数值模拟在飞机型号研制中有重要的作用 ,也是数值模拟中比较复杂的问题之一。本文采用基于Octree技术的方法生成非结构四面体网格 ,用耦合隐式离散的方法进行有限体积离散 ,利用此方法对某型飞机的绕流特性进行了数值模拟 ,收到较好效果。     

一种新型航空鱼雷模拟训练装置

介绍了一种用于攻潜实践教学的模拟训练装置 ,以及该装置的硬件构成、软件流程、抗干扰的措施和能进行训练的内容     

带箍环掠型叶片整体叶盘强度分析方法研究

针对带复合材料箍环掠型叶片整体叶盘结构，开发了对叶片快速施加气动载荷的方法，发现了整体叶盘的应力应变分析和寿命预测方法，成功地完成了模型叶盘的应变测量和低循环疲劳试验。通过模型叶盘数值分析与试验测量数据的比较可见，二吻合较好，从而验证了上述方法的有效性。     

含钾盐的NC/TMETN基钝感双基推进剂火焰结构研究

利用单幅放大摄影法研究了含钾盐消焰剂的NC／TMETN（三羟甲基乙烷三硝酸酯）基钝感推进剂的火焰结构。结果表明，不同的钾盐导致该类推进剂的火焰结构各不相同，含有机钾盐KD的推进剂的火焰结构保持了平台双基推进剂火焰结构的特征，而含K3AlF6的推进剂却有着安全不同的火焰结构。由此可发现K3AlF6使得推进剂平台燃烧效应消失的原因。     

飞机穿越下冲暴流安全起飞运动方程的研究

推导了存在风切变时在气流坐标系（相对风轴系）中飞机质心空间三维运动方程和在体轴系中飞机的旋转运动方程，指出了按航迹坐标系，（绝对风轴系）建立移动运动方程时某些不便之外。为了进行比较，给出了分别应用上述两组运动方程计算的波音－７２７飞机起飞行轨迹的不同结果。     

充有弹性介质多层复合材料圆筒壳稳定性

本文分析了充有弹性介质的多层复合材料圆筒壳在轴压、侧压与水压作用下的稳定性。所采用的方法是用Galerkin—差分法求介改型的Donnell方程,再根据稳定准则确定临界值。若干算例已在文中列出。计算结果表明:内部介质材料性能和壳体的边界条件对临界载荷有较大影响。本文采用的分析方法和结论可供固体火箭发动机壳体设计工作者参考。     

微波带通滤波器的时域分析法研究

文章介绍了一种利用微波带通滤波器的时域反射损耗(即S11)曲线分析和调试滤波器的方法,运用此法在调试滤波器时可以快速地分析出具体是哪一个谐振电路或耦合器需要调试,以便对其进行专门的修正和调试,从而节省调试时间,简化调试过程。同时也介绍了3种方法作为把频域数据转换为时域数据的理论基础,即傅里叶级数法、快速傅里叶变换法和Chirp-z变换法,并对这3种方法作了相应的评价。     

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.