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.     

SLFM网络及其学习算法的改进

介绍了一种新型的人工神经网络--有监督线性特征映射(SLFM)网络,它综合了BP网络的可监督性和SOM网络算法简单的优点,具有学习速度快、精度高、扩展能力较强的优点.文中讨论了SLFM网络的拓扑结构和学习机制,并对网络的学习算法进行了改进,对比实验表明,改进后的SLFM网络其性能得到了进一步的提高.     

卫星电源系统的母线性能分析

建立以母线为核心的分流器,蓄电池充电调节器（ＢＣＲ）,蓄电池放电调节器（ＢＤＲ）和太阳阵的交流小信号模型;导出母线动态阻抗、稳定性、瞬态响应和纹波的分析法,并利用该方法举例分析了革一电源系统的性能。此外,还利用Ｐｏｗｅｒ Ｓｉｍｕｌａｔｉｏｎ（ＰＳＩＭ）电源系统仿真软件对该电源系统进行了仿真,验证了理论分析方法的正确性。     

跨声速双级轴流压气机对周向进气总压畸变的响应特性分析

基于所建立的总压畸变矩阵传递模型,对周向总压畸变下某型跨声速双级轴流压气机容畸变特性进行了详细的数值分析,揭示出了多级环境下轴流压气机对进气畸变的衰减/增益变化规律,这对理解增强多级轴流压气机抗压力畸变能力机理,提高多级轴流压气机性能和扩大其稳定工作范围意义明显。      

某型加力涡扇发动机变几何扩稳优化模拟

本文基于级特性和级叠积模型,发展了涡扇发动机风扇压气机导叶、静叶调节扩大发动机稳定裕度的计算模型,并将其与某型加力涡扇发动机共同工作计算模型相结合,建立了低函道比加力涡扇发动机风扇和压气机变几何调节扩稳的模拟方法及相应的计算模拟程序,并对发动机变几何的调节方案进行了初步的优化分析,结果表明合理的发动机变几何调节可使发动机性能和稳定裕度获得最佳匹配。      

自旋稳定卫星姿态参数的容错Kalman滤波

Kalman滤波是一组用递推关系给出的动态 测量系统状态向量的最优线性无偏滤波 ,它在航天测控领域中有广泛应用。以自旋稳定型卫星姿态确定为研究对象 ,探讨Kalman滤波算法的实现途径 ,并对Kalman滤波算法本身进行适当改进 ,建立一组对测量数据野值点具有容错能力的修正型滤波算法 ;此外 ,还对滤波初值选取和测量数据误差协方差阵的估计等技术给出了有价值的建议     

快速Max-Min公平带宽分配算法稳定性分析

高QoS的网络传输要以一个稳定的连接作为保证,这就要求资源分配算法要有良好的动态稳定性,但公平分配算法的稳定性还没有得到人们的普遍重视。鉴于Max-Min公平带宽分配方案的实现算法─渐次填充算法的收敛速度太慢,本文提出了快速Max-Min公平分配算法,该算法用多次平均值来快速逼近公平资源值,巧妙的回避了渐次填充算法步长和收敛速度间的矛盾,大大提高了收敛速度。最后,本文对该算法进行了摄动分析,并证明了该算法的稳定性。     

数据传输卡插拔互换性技术探讨

介绍了数据传输卡(DTC)插拔互换性技术有关的几个问题。在产品有使用延续性要求的限制下,在不提高原零部件制造精度和不改变原装配方式的条件下,提出了按照模拟量传递原则而建立的标准体系——装配检验对合平台,并以此在生产中实施,满足了产品使用互换性要求。同时提出了一种新型弹顶组件的设计,使弹顶位置更合理,弹顶更可靠,从而进一步提高了产品插拔可靠性。     

JMASS环境下的飞行仿真组件集成研究

简要介绍了联合建模与仿真系统(JMASS)的基本概念,分析了JMASS的结构和组成。进一步以一个飞行仿真组件的集成为实例,阐述了如何进行基于JMASS仿真环境的仿真子系统开发,特别研究了如何给已有仿真组件增加设计专门针对JMASS环境而的接口的技术,使现有组件能够顺利集成到JMASS环境下,并使之正确运行。