平面激波绕30°出峰后的绕射与反射

本文针对一平面激波S绕过坡角为30°的山峰后与地面作用所产生的波系图案等问题,通过激波管光测模型实验手段进行了分析和研究。实验是在入射激波马赫数Μ_i=1.18,1.32,1.74,2.00和2.29等五种条件下进行的。实验结果表明,在入射激波S和反射激波R之间出现了一接触面C,并与Skews关于平面激波绕凸角壁面时所得到的结果做了比较。与此同时,从我们所拍摄的纹影流场照片上可以看出,平面激波S绕过30°山峰后与地面作用所产生的反射波均属于马赫反射的范围。     

二维跨音速流动计算的显式多步有限面积方法

本文按Jameson等的思路,采用新的人工粘性项系数,建立显式多步有限面积方法,给出绕NACA0012翼型和RAE2822翼型跨音速流动的计算结果。     

平板上钝缘舵在超声速绕流中的三维分离特性研究

对于平板上的直立钝缘舵在M_∞=1.79、2.04和2.50的条件下,研究了该平板干扰区中的三维分离特性。着重讨论了钝缘直径、舵面迎角和来流马赫数对主分离线位置和形状的影响。分析了该类三维分离在性态上更强地依赖于无粘流动特性。此外,还对分离区内的二次分离发展过程和形态进行了初步讨论。     

强海杂波背景下目标检测方法综述

高频地波雷达被广泛应用于海面目标的检测,而由于海杂波的分布散射具有很强的动态特性,通常情况下成为了海面目标检测的主要干扰成分.因此,在强海杂波背景下进行目标检测的关键在于如何有效抑制海杂波.从循环对消、子空间分解、模型预测以及分形特征这几方面对海杂波抑制技术进行综述、分析和总结,为后续对海面目标检测提供参考.     

Effect of q-nonextensive hot electrons on bifurcations of nonlinear and supernonlinear ion-acoustic periodic waves

Nonlinear and supernonlinear ion-acoustic periodic waves are investigated in a three-component unmagnetized plasma which consists of mobile fluid cold ions, Maxwellian cold electrons and q-nonextensive hot electrons employing phase plane analysis. Using the traveling wave transformation, the plasma system is reduced to a planar autonomous dynamical system. Utilizing phase plane analysis of planar dynamical systems, all possible phase portraits including nonlinear homoclinic orbit, nonlinear periodic orbit, supernonlinear homoclinic orbit and supernonlinear periodic orbit are presented depending on physical parameters $q,\alpha ,\sigma$ and V. Using numerical simulations, nonlinear and supernonlinear ion-acoustic periodic waves are shown for different conditions. It is found that the nonextensive parameter q plays a crucial role in the bifurcations of nonlinear and supernonlinear ion-acoustic periodic waves. Our study may be applicable to understand the nonlinear and supernonlinear periodic features in auroral plasma.     

无源无线声表面波压力传感器校准技术研究

声表面波压力传感器是一种新型传感器,它的一大优势是具有无源无线信号传递特性,可以突破传统传感器线缆连接的限制,近年来受到国内外研究机构普遍重视。本文探讨了SAW压力传感器的校准技术,对某种商业传感器进行校准,使用最小二乘法分析校准结果,并进行不确定度评估。校准结果显示该传感器在误差、线性、重复性等方面可满足一定精度要求,通过进一步发展,有望在航天领域得到实际应用。     

基于模态反转的半球谐振陀螺零位自校准方法

针对半球谐振陀螺的零位漂移问题，本文研究了基于模态反转电路控制技术的零位自校准方法。首先，从动力学模型引入阻尼不对称、频率裂解等非理想因素，讨论半球谐振陀螺的工作机理及驻波漂移特性。其次，通过理论分析模态反转的零位校准以及虚拟进动控制的模态反转技术。最后，基于FPGA数字控制平台，设计并实现了半球谐振陀螺零位自校准半实物仿真实验。实验结果表明，基于模态反转的半球谐振陀螺零位校准，实现了半球谐振陀螺的零位从15 降低至2 ，短期零偏稳定性和长期稳定性也分别提高了11.8％和45.86％，有效地抑制了零位漂移，提高了半球谐振陀螺测量精度。     

Injection of 40-kHz-modulated electron beam from the satellite: II. Excitation of electrostatic and whistler waves

Beam-plasma interaction effects are studied during the active space experiment with electron and Xe-ion beam injections in an ionospheric plasma. Permanent 40-kHz-modulated electron beam injection occurs simultaneously with a xenon-ion beam injected by the Hall-type plasma thruster operating in a square-pulse mode (100/50 s for a job/pause duration). The unusual behavior of the background charged particle fluxes and wave activity stimulated during the beam-plasma interaction have been registered by the scientific instruments onboard Intercosmos-25 station (IK-25) and Magion-3 subsatellite. The longitudinal and electromagnetic wave instabilities and their mutual relationship are considered in order to explain the observed effects. The excitation of electrostatic waves by the electron injection has been considered for different resonance conditions near the linear stability boundary. Beam-driven electromagnetic instability is responsible for the backward-propagating whistler waves excited via cyclotron resonance. Competition of these two beam instabilities is one of the subjects of the present study.     

一种冲击响应谱试验设备校准装置的研制

介绍了冲击响应谱基本概念及其试验设备的分类与工作原理，参考现行冲击试验台检定规程提出了针对该设备的校准方法，设计了一种基于虚拟仪器技术的新型冲击响应谱试验设备校准装置，给出了典型冲击波形（半正弦、矩形、后峰锯齿）的冲击响应谱仿真计算结果并进行了验证，计算结果与理论结果完全一致，证明算法准确可靠，能够实现对冲击响应谱试验设备的校准。     

Case study of inclined sporadic E layers in the Earth’s ionosphere observed by CHAMP/GPS radio occultations: Coupling between the tilted plasma layers and internal waves

We have used the radio occultation (RO) satellite data CHAMP/GPS (Challenging Minisatellite Payload/Global Positioning System) for studying the ionosphere of the Earth. A method for deriving the parameters of ionospheric structures is based upon an analysis of the RO signal variations in the phase path and intensity. This method allows one to estimate the spatial displacement of a plasma layer with respect to the ray perigee, and to determine the layer inclination and height correction values. In this paper, we focus on the case study of inclined sporadic E (E_s) layers in the high-latitude ionosphere based on available CHAMP RO data. Assuming that the internal gravity waves (IGWs) with the phase-fronts parallel to the ionization layer surfaces are responsible for the tilt angles of sporadic plasma layers, we have developed a new technique for determining the parameters of IGWs linked with the inclined E_s structures. A small-scale internal wave may be modulating initially horizontal E_s layer in height and causing a direction of the plasma density gradient to be rotated and aligned with that of the wave propagation vector k. The results of determination of the intrinsic wave frequency and period, vertical and horizontal wavelengths, intrinsic vertical and horizontal phase speeds, and other characteristics of IGWs under study are presented and discussed.