"探测一号"电磁验证模型星磁控制技术

对于磁洁净度要求严格的卫星在研制前要进行磁设计,研制过程中要进行磁控制,才能保证卫星磁性指标的实现.文章介绍了"探测一号"电磁验证模型星的磁设计与控制技术.     

三维捷联磁传感器误差分析及补偿

磁传感器在导航系统中的应用日益广泛。在车载导航系统工作环境中,外界干扰磁场复杂,严重影响了磁航向测量的精度。因此对磁航向进行适当的罗差补偿是提高磁航向测量精度的有效途径。文中介绍了用磁传感器进行磁航向测量的原理,分析了由于磁场矢量叠加产生的罗差,提出了基于傅立叶级数的罗差模型和补偿方法。工程实践表明,上述方法的使用收到了较好的效果。     

航天器空间动态磁场模拟技术

文章论述了卫星空间动态磁场模拟技术的原理和方案,阐述了对方案的工程化实现所进行的必要计算及对系统的各个部分所进行的研究设计。在此基础上建立了一套动态磁场模拟系统,为卫星空间动态磁场模拟试验提供了条件。     

小卫星磁场分布测量方法研究

文章通过分析卫星磁场与地磁场的关系,确立了磁场分布的测量方法,并对测量误差进行了分析.     

电磁脉冲武器对抗空袭飞机研究

电磁脉冲武器已在现代战争中崭露头角,它的出现为抗击空袭飞机(包括隐身飞机)提供了一条新的思路。在分析电磁脉冲武器特点和国内外电磁脉冲武器研究进展的基础上,论述了电磁脉冲武器抗击来袭飞机(包括隐身飞机)的可行性和方法。     

某型号卫星磁性分析与控制

某型号卫星的有效载荷之一高能望远镜对磁场敏感,因此在设计阶段即需分析卫星在轨时载荷所处的磁场环境,并尽可能提高载荷的抗磁场干扰能力。文章根据卫星的构型,对整星的磁场分布进行了计算;对载荷的抗磁场干扰能力进行了测试;对载荷的磁屏蔽方案进行了仿真与测试;分析了抗磁场干扰设计对整星磁性控制的影响,证明卫星可以满足总磁矩不大于5.0 A?m2的姿态控制要求。     

基于复杂网络理论的复杂电磁环境分析与度量

将复杂电磁环境看作由能产生、接收、反射（散射）和吸收电磁信号的实体所构成的复杂系统.并将该系统抽象为以其组分为节点、以各节点间通过“电磁信号”的相互作用和影响为连边的复杂加权有向网络,其连边的权值反映节点相互作用和影响的程度.通过对这个复杂加权有向网络的特征量的研究,提出了基于复杂网络理论的复杂电磁环境度量新方法.     

Geosynchronous magnetic field response to the large and fast solar wind dynamic pressure change

We present a comparison of large and sharp solar wind dynamic pressure changes, observed by several spacecraft, with fast disturbances in the magnetospheric magnetic field measured by the GOES-8, 9 and 10 geosynchronous satellites. Almost 400 solar wind pressure changes in the period 1996–2003 were selected for this study. Using the large statistics we confirmed that increases (decreases) in the dynamic pressure always results in increases (decreases) in the magnitude of geosynchronous B_z component. The amplitude of the geosynchronous B_z response strongly depends on the location of observer relative to the noon meridian, from the value of solar wind pressure before the disturbance arriving and firstly – from the amplitude of the pressure change.     

单通道和双通道微波衰减测量系统中的射频泄漏分析

研究了单通道和双通道微波衰减测量系统中的射频泄漏所导致的测量误差。使用电磁屏蔽箱和以铝片包裹连接头的方法降低外部辐射泄漏,在双通道衰减测量系统中使用隔离器以减小内部泄漏。利用高灵敏度锁相放大器测量了射频泄漏信号,通过在60 MHz和5 GHz所得的实测数据比较了单通道和双通道衰减测量系统的射频泄漏误差。实验结果表明射频泄漏得到了有效的抑制。     

On the application of the boundary element method in coronal magnetic field reconstruction

Solar magnetic field is believed to play a central role in solar activities and flares, filament eruptions as well as CMEs are due to the magnetic field re-organization and the interaction between the plasma and the field. At present the reliable magnetic field measurements are still confined to a few lower levels like in photosphere and chromosphere. Although IR technique may be applied to observe the coronal field but the technique is not well-established yet. Radio techniques may be applied to diagnose the coronal field but assumptions on radiation mechanisms and propagations are needed. Therefore extrapolation from photospheric data upwards is still the primary method to reconstruction coronal field. Potential field has minimum energy content and a force-free field can provide the required excess energy for energy release like flares, etc. Linear models have undesirable properties and it is expected to consider non-constant-alpha force-free field model. As the recent result indicates that the plasma beta is sandwich-ed distributed above the solar surface (Gary, 2001), care must be taken in modeling the coronal field correctly. As the reconstruction of solar coronal magnetic fields is an open boundary problem, it is desired to apply some technique that can incorporate this property. The boundary element method is a well-established numerical techniques that has been applied to many fields including open-space problems. It has also been applied to solar magnetic field problems for potential, linear force-free field and non-constant-alpha force-free field problems. It may also be extended to consider the non-force-free field problem. Here we introduce the procedure of the boundary element method and show its applications in reconstruction of solar magnetic field problems. This revised version was published online in August 2006 with corrections to the Cover Date.