76°/40°双三角翼前缘涡破裂及其控制实验研究

流动显示结果表明,喷流能有效地推迟双三角翼前缘涡的破裂,且随着攻角的增大,前缘涡破裂位置逐渐推后,喷流极大地改善了大攻角情况下前缘涡的非对称破裂特性,能有效地克服可能出现的机翼的"摇滚"现象.另外,后缘喷流可以减弱乃至消除前缘涡混掺现象的发生,进而有利于飞行器的操纵.     

滑流区中三角翼大攻角气动力特性的实验研究

一种以后掠75.7°薄三角翼为主要特征的典型航空航天飞行器模型,在激波管风洞马赫数为11.9和15.4两种条件下,攻角范围20°～50°,用模型自由飞方法测量了它们的轴向力系数、法向力系数和俯仰力矩特性。相应的实验雷诺数分别为3.19×10~4和1.64×10~4,这两种流动条件均属于稀薄气流的滑流区。 实验结果表明在M_∞=11.9和15.4两种条件下,两种剖面外形模型的升力系数和阻力系数均随攻角加大而递增,其变化规律有很好的一致性,且对马赫数并不敏感;但从体轴系来看,不仅两种模型的轴向力系数不同,而且因粘性干扰的缘故,同一模型A在M_∞=15.4时比M_∞=11.9时有相对较大的轴向力系数,但两者随攻角变化的规律一致,且当α>45°时接近牛顿值。此外,实验表明两种模型的压心系数随攻角均没有明显变化。     

卫星姿态控制的一种鲁棒控制方法

针对含有不确定性的Delta算子离散系统,研究了其鲁棒控制问题。鲁棒控制律的存在条件及设计由线性矩阵不等式描述,便于求解。将所得结果应用于卫星姿态控制系统的设计,以解决对模型进行线性化处理时产生的误差。针对所得控制律进行了仿真研究,结果证明了方法的有效性。     

阵列式表面电弧等离子体气动激励控制三角翼流动分离的实验

为探索多路阵列式微秒脉冲表面电弧放电(μs-SAD,Microsecond pulse surface arc discharge)对尖前缘小后掠三角翼流动分离的控制效果和作用机理,首先通过放电测试和纹影测试对多路阵列式μs-SAD的激励特性进行研究,揭示其对流场的作用原理,进一步将多路阵列式μs-SAD用于三角翼流动控制,开展了小后掠三角翼流动分离控制低速风洞实验,研究了来流速度、激励电压和激励频率等参数对控制效果的影响规律。结果表明:多路阵列式μs-SAD能够快速放热,单路瞬间放电能量可达68mJ,在流场局部可诱导产生冲击波;机翼前缘多路阵列式μs-SAD能有效改善三角翼大迎角气动特性,当来流速度为30m/s时,使最大升力系数提高27.2%,失速迎角推迟4°;来流速度增大到40m/s时,流动控制效果减弱,使最大升力系数提高15.5%;存在最佳激励频率使无量纲频率F+=1时,控制效果最好;激励电压存在阈值,其随来流速度的增加而增大,当激励电压超过阈值电压继续增大时,流动控制效果不再增强。     

对流层顶变化对上对流层/下平流层臭氧分布的影响

上对流层和下平流层(UT／LS)，位于8-25km高度之间，是大气中一个很特殊的区域．大部分的臭氧分布在下平流层，在下平流层臭氧的含量发生一个很小的变化，就会对气候和地面的紫外辐射产生很大的影响．而作为气象参数的对流层顶，是充分混合、缺乏臭氧的上对流层和层结稳定、臭氧丰富的下平流层之间的边界或过渡层，其变化对臭氧总量和分布有直接和明显的影响．本文使用二维模式模拟研究对流层顶变化对臭氧在UT／LS分布的影响．模拟结果表明对流层顶的季节变化对UT/LS的臭氧分布有明显的影响，臭氧的局地变化可以超过10％在冬季北半球中纬度对流层顶高度升高1km时，模式结果表明对臭氧分布的影响比较显著，局地变化可超过6％，但是对臭氧总量的影响较小，变化不超过5DU，小于观测资料统计分析的结果。     

相对差分单向测距（△DOR）技术在探月工程中的应用研究

相对差分单向测距（△DOR）是一种高精度测角技术,在深空探测任务的高精度测定轨方案中得到广泛应用．介绍了△DOR测量的基本原理及CCSDS（国际空间数据系统委员会）关于△测量的相关标准．针对中国探月工程月面软着陆任务提出的高精度测定轨要求,分析了△DOR测量的信号形式、工作模式以及测量精度,推导了解模糊过程．研究表明,△DOR测角精度达到25nrad,对应到月球上的距离约为10m．     

俄罗斯Fregat上面级

介绍了俄罗斯Fregat上面级的基本功能、组成和主要技术指标。给出了其几何布置、贮箱可承力、独立性与自主性、液-固耦合及大幅晃动和多次起动等特点与关键技术等。给出了2003年欧空局火星探测项目、2005年欧空局金星探测项目和中俄联合火星探测项目等典型应用。     

Satellite and ground detection of very dense smoke clouds produced on the islands of the Paraná river delta that affected a large region in Central Argentina

Intense fires were produced on the Paraná river delta islands, Argentina, during most part of 2008, by a combination of an exceptionally dry period and the farmers’ use of a fire land-cleaning technique. In April 2008, those fires significantly affected the nearby regions and their inhabitants, from Rosario city to Buenos Aires mega-city. In this work we present satellite as well as ground Aerosol Optical Depth (AOD) at 550 nm data obtained during the propagation of pollution clouds to the central zone of Argentina. The highest value (1.18) was registered at Buenos Aires by atmospheric remote sensing, using the satellite instrument MODIS/Terra on April 18th 2008 at 10:35 local time (= UT − 3 h). On the same day, ground air quality detectors also measured in this city the highest Total Suspended Particle (TSP) value of the month, 2.02 mg/m³. The AOD(550) daily variation at Rosario Astronomical Observatory, which is located near the Paraná riverside, was derived by combining solar ultraviolet erythemal irradiance data (measured with a YES biometre) with model calculations. On April 25th 2008, from 12:00 to 15:30 local time, a rather high and constant AOD(550) value was registered, with a mean value of (0.90 ± 0.21). Cities located on the side of the Rosario–Buenos Aires highway (San Nicolás, Baradero and San Pedro) were also affected, showing a mean AOD(550) between the Rosario and Buenos Aires values. The particulate matter was collected with gridded samplers placed on the Paraná river islands as well as at the Rosario Observatory. They were analysed with a Scanning Electron Microscope (SEM) and mainly showed a biological origin. Even if normally large particles travel small distances from the source, organic aerosol in the range of 40–100 μm and complex asymmetric structures were registered several kilometres away from the aerosol sources on the islands. Another event of intense UV index attenuation (98.6%) occurred on September 18th 2008, due to very dense smoke clouds that extended over the Rosario area for several hours. The clouds were driven away from the fires by East–northeast and East–southeast winds. The minimum value of this index measured around noon allows to derive a maximum AOD(550)_max = (3.65 ± 0.90) at 12:45 local time. Soot clouds extended over the Paraná river, transporting Burned Biomass Debris (BBD) that deposited on Rosario. In particular, burned leaves and small branches with dimensions of 1–20 cm were collected. The mean (BBD) particles deposited on the ground from 7:00 to 19:00 local time were (0.92 ± 0.20) BBD/(m² h).     

中国深空网首次△DOR联合测轨试验分析

通过分析中国深空网首次△DOR（Delta Differential One way Ranging,双差分单向测距）联合测轨试验的干涉测量事后数据,重点从观测量随机精度、闭合时延等方面讨论了国内深空网与国内VLBI（Very Long Baseline Interferometry,甚长基线干涉测量）观测网、国内深空网与国际深空网的联合干涉处理情况,并与ESOC（European Space Operation Center,欧洲空间操作中心）数据处理结果进行了比对.试验结果表明：我国深空网已具备独立或联合开展深空探测器导航测轨的系统支持能力;深空站系统具备高速率数据接收、采集、记录、传输能力,采集数据处理精度优于1 ns;深空网干涉测量信号处理中心具备多体制信号的干涉处理分析能力,其分析精度与ESOC处理精度差异在0.1 ns量级.     

Experimental investigation of boundary layer transition over a delta wing at Mach number 6

An experimental study on the boundary layer transition over a delta wing was carried out at Mach number 6 in a quiet wind tunnel. The Nano-tracer-based Planar Laser Scattering (NPLS) and Temperature-Sensitive Paints (TSP) techniques were used to measure the fine flow field structure and the wall Stanton number of the delta wing. The influence of factors such as the angle of attack and the Reynolds number was studied. The following results were obtained. The boundary layer transition between the leading edge and the centerline was dominated by the crossflow instability. At the location of the initial appearance of the traveling crossflow waves, the Stanton number began to rise. The Stanton number reached a maximum when the crossflow waves were broken up to turbulence. Increasing the angle of attack increased the spanwise pressure gradient at the windward side of the delta wing, thereby increasing the crossflow instability and advancing the boundary layer transition front. However, increasing the angle of attack caused the transition front to move backward at the leeward side. In addition, the sensitivity of the boundary layer transition to the Reynolds number varied with the angle of attack and the region.