五元素风帆的试验研究

用正交试验与系列试验相结合的方法,研究了五元素风帆的气动特性及其各参数之间的最佳配合问題。设计的4个五元素风帆,均是由3个固定小翼、2个活动小翼及上下两块制流板所组成,但小翼的形状及分布曲线不同。 通过风洞试验,得到了各个风帆攻角与两个活动小翼转角之间的最佳配合,并对各帆的气动特性作了比较。试验结果表明,在最佳配合状态下,4个帆的升力系数可分别达到2.64、2.87、2.69和2.08,均比常规帆有较大的增长;而且,只要打开活动小翼,就能释放大部分风能,从而保证船舶在大风中的安全,这些帆的结构并不复杂,是具有广泛应用前景的高效帆具。     

串置双五分量天平的研制

本文介绍风洞应变天平中首次研制成功的一台串置双五分量天平。串置双天平由一块钢材制成。O_1天平固定在 O_2天平的受力端。O_2天平既能测量左平尾载荷,又能传递由 O_1天平测量的右平尾载荷。正确分析两台天平的受力传力路线和弹性变形的综合位移量,用严谨的数学公式描述两台天平测量的力和传递的力。对这两种力进行数学分解,形成数学模型,写出天平静校公式的数学表达式,并据此研制天平静校设备,分析天平在各分力作用下的弹性位移,写出弹性角公式。上述各点是串置双天平的核心问题。最后经风洞引导性实验证明,串置双天平的原理、方案、受力分析、静校公式等都是正确的。在国内外,串置双天平第一次用于风洞实验,获得了初步成功。     

土壤槽三分量天平

本文通过实例表明,常规风洞测力天平移植于对沙漠的研究是成功的。设计排除了土壤的自重影响,天平有较高的灵敏度,整机可根据不同土壤槽而升沉,是研究沙粒迁移的较好工具。     

俯仰振荡三角翼在非定常自由流中运动的实验

在南京航空航天大学已建成的国内首座非定常风洞内,研制了一套单自由度俯仰振荡实验装置,设计开发了一套对模型姿态和来流风速进行联合控制的软件。对一60°后掠三角翼模型进行了单独俯仰振荡运动和俯仰振荡与自由来流耦合运动的实验。实验结果表明:模型做单独俯仰振荡时,振动频率和振动幅值的影响只有在迟滞环出现后才起作用,而迟滞环的出现是由于翼面上的不同流态对外界扰动的反应时间不同造成的。非定常自由流对做俯仰振荡的三角翼气动特性有很大的影响,模型上仰过程中来流的减速,进一步提高了最大升力系数,推迟了失速迎角;模型下俯过程中来流的加速,则更进一步推迟了升力系数恢复到静态时的值。当翼面上产生破碎涡流时,非定常自由流的作用表现得更为明显。     

跨声速柔壁自适应风洞及试验技术研究

简述西北工业大学自适应壁风洞研究课题组在“八五”期间开展跨声速柔壁自适应壁风洞试验技术研究的主要研究工作成果。简介该校的高速柔壁自适应壁风洞的设计及主要参数，以及在该风洞中开展的低超声速消除波反射的研究、近声速的自适应壁风洞试验技术研究和跨声速自适应壁试验段优化设计的研究。     

CARDC 2.4m引射式跨声速风洞设计与运行调试

中国空气动力研究与发展中心研制了可更换喷嘴的中压气体引射器 ,利用现有中压气源驱动 ,建成一座增压回流引射式跨声速风洞。试验段截面尺寸 2 .4m×2 .4m ,M =0 .3～ 1 .2。稳定段最高工作压力为 0 .45MPa ,最高模型试验雷诺数Rec=1 5× 1 0 6(M =0 .90 ,C =0 .2 4m) ,稳定吹风时间≥ 1 5s。风洞气动回路上分别配置有多喷管引射器、栅指扩散段、跨声速试验段驻室抽气系统及特殊的主排气系统等装置。采用智能自适应解耦控制技术 ,实现总压和M数独立、快速、精确地控制。该气动布局与部段配置及其功能设计 ,在国内跨声速风洞中均是首次采用。     

用电离层特性参量提取等效风场信息

导出了利用中低纬电离层特性参量获取电离层F层峰区高度上等效风场（包含电场和风场信息在内）的基本方程，并尝试用该方法从电离层特性参量（峰高和临频）提取等效风场信息，利用武汉站DGS-256电离层数字测高仪数据及由美国Massachusetts Lowell大学最新版的剖面反演程序换算得到F层峰高，获得了武汉地区夏季至日点附近，冬季至日点附近，冬季地磁特别宁静的九天和冬季平均等效风场的初步特征，并利用Fejer经验电场模式计算冬季电场引起的垂直漂移，估计电场和风场对武汉地区的垂直等效风场的贡献大小，结果表明：等效风场呈现出白天与夜晚幅度和方向的差异。至日点附近冬季与夏季白天的幅度差异以及明显的凌晨凹陷现象；平均情况下，垂直等效风场幅度和方向的变化主要是由中性风引起，受电场的影响不大。     

The characteristics of sharp (small-scale) boundaries of solar wind plasma and magnetic field structures

We investigate properties of large (>20%) and sharp (<10 min) solar wind ion flux changes using INTERBALL-1 and WIND plasma and magnetic field measurements from 1996 to 1999. These ion flux changes are the boundaries of small-scale and middle-scale solar wind structures. We describe the behavior of the solar wind velocity, temperature and interplanetary magnetic field (IMF) during these sudden flux changes. Many of the largest ion flux changes occur during periods when the solar wind velocity is nearly constant, so these are mainly plasma density changes. The IMF magnitude and direction changes at these events can be either large or small. For about 55% of the ion flux changes, the sum of the thermal and magnetic pressure are in balance across the boundary. In many of the other cases, the thermal pressure change is significantly more than the magnetic pressure change. We also attempted to classify the types of discontinuities observed.     

Acceleration of interplanetary pick-up ions and anomalous cosmic rays

It may not be doubted anymore that anomalous cosmic rays (ACRs) are produced in the heliosphere from interplanetary pick-up ions through their acceleration at the solar wind termination shock. However, there is no general agreement in the community of heliospheric researchers concerning the mechanism of injection of the pick-up ions into the shock acceleration. We discuss here three possible ways for pick-up ions to be involved into the acceleration process at the termination shock: (1) preacceleration of pick-up ions in the whole region from the Sun up to the termination shock by solar wind turbulences and interplanetary shock waves, (2) local preacceleration of pick-up ions in a vicinity of the termination shock by shock surfing, and (3) formation of high-velocity tails in pick-up ion spectra consisting of secondary pick-up ions which are produced in the supersonic solar wind due to ionization of energetic neutral atoms entering from the inner heliosheath.     

Effects of Mach numbers on Magnus induced surface pressure

Experimental and numerical methods were used to investigate the Magnus phenomena over a spinning projectile. The pressure force acting on the surface of a spinning projectile was measured for various cases by employing a relatively novel experimental technique. A set of miniature pressure sensors along with a data acquisition board, battery and storage memory were placed inside a spinning model and the surface pressure were obtained through a remotely controlled system. Circumferential pressures of the model for both rotational and static conditions were obtained at two different free stream Mach numbers of 0.4 and 0.8 and at different angles of attack. The results showed the ability of this new test method to measure the very small Magnus force via surface pressures over the projectile. The results provide a deep insight into the flow structure and illustrate changes in the cross-flow separation locations as a result of rotation. Similar results were obtained by the numerical simulations and were compared with the experimental data.