收敛形进气道数值研究的验证

介绍一种新型的、具有最小喉道面积的三维高超声速进气道 (称之为收敛形进气道 )的数值和实验研究结果。表明使用这种形式的进气道 ,在整个飞行速度范围内可以降低阻力和高超声速发动机表面的热防护要求 ,通过降低外压缩表面的倾斜度和减少进气道及燃烧室壁的面积就可以做到这一点。在采用低维次流动的气体动力设计方法的基础上设计成这种形式的进气道。计算是在无粘气体模型构架内用有限体积法进行的。同时用边界层方程计算出计及粘性的气流特性和进气道特性。数值算法是通过收敛形进气道的有限宽楔形外压缩表面的计算和实验数据来验证的。进行实验研究的马赫数M=2～ 1 0 7,基于模型进气道高度的雷诺数Re=( 1～ 5) × 1 0 6。数值计算与实验结果一致性很好。这些结果也和通常的二维进气道的数据作了比较。     

基因方法在网格结点位置优化中的应用

将基因方法应用于网格结点位置的优化中。文中首先简单介绍了基因优化方法中基于达尔文进化论和Ｍｅｎｄｅｌ基因理论的基本原理,其中包括插索空间表达、三个基因作用器（选择、交配和变异）等要点;然后着重阐述了相关偏微分方程的离散误差和三角形网格几何形状的适应度函数的定义、结点位置的二进制基因表达及基因方法的优化进程。离散误差是在二次非连续彭鼓包（ｂｕｍｐ）函数的空间中近似定义的,并且在点移动过程中相关解的二     

基于Petri网的空中交通管制辅助决策系统

空中交通管制系统是生产实际中的一种典型的离散事件动态系统（Ｄｉｓｃｒｅｔｅ ｅｖｅｎｔ ｄｙｎａｍｉｃｓｙｓｔｅｍ,ＤＥＤＳ）,而Ｐｅｔｒｉ网理论是研究ＤＥＤＳ的有力工具之一。为了描述空中交通管制系统受到外部控制的交互机制及层次结构,文中引入Ｐｅｔｒｉ网概念的一类扩充－－开放Ｐｅｔｒｉ网的概念,并用开放Ｐｅｔｒｉ网工中交通管制辅助决策系统进行建模与分析,阐述了空中交通管制辅助决策系统的开放Ｐｅｔｒ     

低速高湍流度90°弯管流动数值模拟

分析了曲率对弯曲管道流动的影响 ,给出了曲率修正的双层 k-ε湍流模型 ,并数值模拟了非均匀来流低速高湍流度 90°弯管内流动。文中比较了曲率修正双层 k- ε湍流模型的计算结果与实验结果 ,以及双层 k- ε湍流模型和逆压力梯度修正双层 k- ε湍流模型的计算结果。通过比较 ,发现经过曲率修正后的双层 k- ε湍流模型更好地模拟了非均匀来流低速高湍流度 90°弯管内流动。同时比较了壁面参数的插值方法 ,发现在弯曲管道流动模拟中对壁面参数进行一阶插值比零阶插值能更好地模拟真实流场     

更多测试 更多安全

<正>Agilent U1250系列数字手持式数字万用表的强大功能特性和性能指标超过了客户的预期,能满足客户最苛刻的测量要求和应用需要。     

Implications of X-ray Observations for Electron Acceleration and Propagation in Solar Flares

High-energy X-rays and ??-rays from solar flares were discovered just over fifty years ago. Since that time, the standard for the interpretation of spatially integrated flare X-ray spectra at energies above several tens of keV has been the collisional thick-target model. After the launch of the Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI) in early 2002, X-ray spectra and images have been of sufficient quality to allow a greater focus on the energetic electrons responsible for the X-ray emission, including their origin and their interactions with the flare plasma and magnetic field. The result has been new insights into the flaring process, as well as more quantitative models for both electron acceleration and propagation, and for the flare environment with which the electrons interact. In this article we review our current understanding of electron acceleration, energy loss, and propagation in flares. Implications of these new results for the collisional thick-target model, for general flare models, and for future flare studies are discussed.     

长征运载火箭飞行过程中二级游机提前或推迟关机问题的探讨

论述了具有小推力飞行段的长征运载火箭在飞行过程中二级游机提前或推迟关机的机理,明确给出了游机可能提前或推迟关机的时间范围,为以后的火箭飞行参数判定提供理论依据。     

Characterization and Calibration of the CheMin Mineralogical Instrument on Mars Science Laboratory

A principal goal of the Mars Science Laboratory (MSL) rover Curiosity is to identify and characterize past habitable environments on Mars. Determination of the mineralogical and chemical composition of Martian rocks and soils constrains their formation and alteration pathways, providing information on climate and habitability through time. The CheMin X-ray diffraction (XRD) and X-ray fluorescence (XRF) instrument on MSL will return accurate mineralogical identifications and quantitative phase abundances for scooped soil samples and drilled rock powders collected at Gale Crater during Curiosity’s 1-Mars-year nominal mission. The instrument has a Co X-ray source and a cooled charge-coupled device (CCD) detector arranged in transmission geometry with the sample. CheMin’s angular range of 5^° to 50^° 2θ with <0.35^° 2θ resolution is sufficient to identify and quantify virtually all minerals. CheMin’s XRF requirement was descoped for technical and budgetary reasons. However, X-ray energy discrimination is still required to separate Co?Kα from Co?Kβ and Fe?Kα photons. The X-ray energy-dispersive histograms (EDH) returned along with XRD for instrument evaluation should be useful in identifying elements Z>13 that are contained in the sample. The CheMin XRD is equipped with internal chemical and mineralogical standards and 27 reusable sample cells with either Mylar^? or Kapton^? windows to accommodate acidic-to-basic environmental conditions. The CheMin flight model (FM) instrument will be calibrated utilizing analyses of common samples against a demonstration-model (DM) instrument and CheMin-like laboratory instruments. The samples include phyllosilicate and sulfate minerals that are expected at Gale crater on the basis of remote sensing observations.