涵道风扇部件耦合设计方法及初步应用

涵道风扇是未来绿色航空动力的重要发展方向,快速、准确的涵道风扇设计方法成为工程领域的迫切需求。在传统的涵道风扇设计方法中,部件间的耦合效应需要建立在完善的三维数值计算或试验数据的基础之上。而本文发展了考虑涵道风扇关键部件耦合效应的设计方法,形成了涵道风扇一体化设计手段,并以此为基础开展了涵道风扇的一体化设计及验证工作。结果表明：相比于简单叠加设计方法,耦合设计使叶片推力设计误差由15%减小到3.5%;采用部件耦合方法设计的带有扩张喷管涵道风扇和等直径喷管涵道风扇的转静叶片推力设计误差满足工程需求,确认了部件耦合的设计方法正确传递了部件间的影响关系;通过试验对设计结果进行了推力校验,试验结果与设计点的总推力误差为1.25%,证明了本文发展的耦合设计方法的准确性。     

基于“高分四号”卫星数据的水体提取效果评价

"高分四号"卫星具有静止轨道卫星高时间分辨率和中高空间分辨率的特点,可以实现对水体面积及变化的大范围实时监测,有效支撑洪涝灾害应急救助工作。为了验证其对水体面积及其变化的监测能力,文章分别利用区域生长法和水体指数法,在开展全国水体面积变化监测基础上,针对与同期"高分一号"卫星16m分辨率多光谱相机及美国Terra卫星的中分辨率成像光谱仪数据等卫星的监测结果展开对比,结果显示,与其他极轨卫星监测结果相比,"高分四号"卫星可以有效开展水体面积及变化监测。但是,鉴于"高分四号"卫星50m像元分辨率,相比更高分辨率遥感影像的水体提取结果,"高分四号"卫星数据提取的水体外部轮廓较为粗糙。在针对规模较小洪涝灾害监测方面可能存在一定误差,仍然需要再进一步开展评价。     

人造地球卫星为何能按预定轨道运行

1无人驾驶的秘密
　　要想使人造地球卫星在预定的轨道运行,首先要用运载火箭把人造地球卫星尽可能精确地送入预定的轨道,使它有较高的速度,然后靠惯性飞行。其关键是要掌握好卫星和火箭分离并开始进入轨道那一瞬时的速度和方向。
　　由于人造地球卫星是一种无人航天器,所以无法像载人飞船那样由航天员操纵来控制其飞行轨道,它主要靠跟踪遥控或自动控制的方式来使卫星按预定的轨道运行。     

基于线性最小均方差估计的星敏感器故障诊断

针对使用两个星敏感器进行姿态测量的三轴稳定控制系统,利用星敏感器输出值与陀螺输出值的解析冗余关系,通过设计两个滤波器实现对不同星敏感器的故障隔离.考虑到陀螺测量噪声以乘性噪声的形式出现在姿态运动学方程中,利用陀螺输出测量值和目标星敏感器的测量值,采用线性最小均方差估计器得到包含目标星敏感器故障信息的残差; 以无故障情况下残差的统计方差为基础得到阈值,通过检验残差评价值是否超过相应的阈值,实现对目标星敏感器故障的检测; 分别将两个星敏感器作为目标星敏感器,综合两个故障检测结果隔离故障.对星敏感器出现测量偏差和精度逐渐下降两种故障的仿真验证了该方法的有效性.     

基于Tersoff-Brenner势的航天器群图形编队研究

从分子动力学模拟角度提出了一种分布式航天器群导航控制方法,可使行星中心开普勒轨道上的航天器群在有限的感知信息条件下自发实现图形编队.该法基于人工势场技术,主要分为两个部分：改造自C-W方程的外围全局汇聚势场和基于Tersoff-Brenner势的局部塑形势场.前者将各航天器导引至预设汇聚点附近,后者进一步使各航天器自我调整彼此相对位置,最终编成期望构型.此外,引入一速度依赖型耗散项以确保任意初始分布条件下图形编队均收敛.通过地球同步轨道上航天器群正四面体构型（含中心,即金刚石结构单元）编队仿真,验证了所提方法的有效性和优越性.将编队脚本简单修改,该法还可方便用于其它类碳元素同素异形体构型的塑造,如石墨晶体结构单元正六边形等.     

旋成体表面沟槽减阻试验研究

在旋成体模型表面粘贴铝基沟槽蒙皮,研究沟槽表面对模型阻力的影响.给出基于来流单位雷诺数的沟槽尺寸无量纲公式,用于设计沟槽齿高和齿宽,依据试验风洞的单位雷诺数范围,选定3种尺寸的沟槽进行减阻试验.结果表明,在旋成体表面湍流流动区域顺流向布置沟槽,当沟槽齿高和齿宽的无量纲值h+、s+均小于25时,在小迎角下具有减阻作用,当s+约为15时减阻效果最明显,可减小约3%~4%的阻力.     

Abiotic nitrogen fixation on terrestrial planets: reduction of NO to ammonia by FeS

Understanding the abiotic fixation of nitrogen and how such fixation can be a supply of prebiotic nitrogen is critical for understanding both the planetary evolution of, and the potential origin of life on, terrestrial planets. As nitrogen is a biochemically essential element, sources of biochemically accessible nitrogen, especially reduced nitrogen, are critical to prebiotic chemistry and the origin of life. Loss of atmospheric nitrogen can result in loss of the ability to sustain liquid water on a planetary surface, which would impact planetary habitability and hydrological processes that shape the surface. It is known that NO can be photochemically converted through a chain of reactions to form nitrate and nitrite, which can be subsequently reduced to ammonia. Here, we show that NO can also be directly reduced, by FeS, to ammonia. In addition to removing nitrogen from the atmosphere, this reaction is particularly important as a source of reduced nitrogen on an early terrestrial planet. By converting NO directly to ammonia in a single step, ammonia is formed with a higher product yield (~50%) than would be possible through the formation of nitrate/nitrite and subsequent conversion to ammonia. In conjunction with the reduction of NO, there is also a catalytic disproportionation at the mineral surface that converts NO to NO? and N?O. The NO? is then converted to ammonia, while the N?O is released back in the gas phase, which provides an abiotic source of nitrous oxide.     

Calcification and silicification: fossilization potential of cyanobacteria from stromatolites of Niuafo'ou's Caldera Lakes (Tonga) and implications for the early fossil record

Calcification and silicification processes of cyanobacterial mats that form stromatolites in two caldera lakes of Niuafo'ou Island (Vai Lahi and Vai Si'i) were evaluated, and their importance as analogues for interpreting the early fossil record are discussed. It has been shown that the potential for morphological preservation of Niuafo'ou cyanobacteria is highly dependent on the timing and type of mineral phase involved in the fossilization process. Four main modes of mineralization of cyanobacteria organic parts have been recognized: (i) primary early postmortem calcification by aragonite nanograins that transform quickly into larger needle-like crystals and almost totally destroy the cellular structures, (ii) primary early postmortem silicification of almost intact cyanobacterial cells that leave a record of spectacularly well-preserved cellular structures, (iii) replacement by silica of primary aragonite that has already recrystallized and obliterated the cellular structures, (iv) occasional replacement of primary aragonite precipitated in the mucopolysaccharide sheaths and extracellular polymeric substances by Al-Mg-Fe silicates. These observations suggest that the extremely scarce earliest fossil record may, in part, be the result of (a) secondary replacement by silica of primary carbonate minerals (aragonite, calcite, siderite), which, due to recrystallization, had already annihilated the cellular morphology of the mineralized microbiota or (b) relatively late primary silicification of already highly degraded and no longer morphologically identifiable microbial remains.     

环境减灾-1B卫星遥感数据在干旱监测中的应用

以2010-2011年发生在山东省的秋、冬、春三季连旱为例,介绍了环境减灾-1B（HJ-1B）卫星遥感数据在干旱监测中的应用。获取了山东省干旱发展顶峰时段的HJ-1B卫星采集的多光谱和热红外遥感影像,利用ENVI 4.7遥感数据处理平台对山东全省的归一化植被指数和地面温度进行了反演,在此基础上计算了山东全省的植被供水指数,并据此将山东省的干旱情况划分为5级,对该干旱监测结果进行了分析。为了验证结论的可靠性,将干旱监测结果与全国降水距平百分率进行了对比,对比结果表明两者一致性较好。文章提供了HJ-1B卫星遥感数据在干旱监测方面的一个实例,其监测结果为相关减灾部门的救灾工作提供了重要的参考,同时也为HJ-1B卫星遥感数据在干旱监测方面的业务化运营提供了一个通用的方法。     

某型号大推力火箭发动机试验推力测量不确定度评定

根据某型号大推力火箭发动机试验推力测量系统的工作原理和组成、计量标准量值传递关系和系统低温调试结果,确定推力测量系统的不确定度来源,通过进一步的误差分析并应用误差计算理论对系统不确定度进行评定,得出该系统测量不确定度作为推力测量准确性依据。