热处理对FeCo-2V-0.5Cr软磁合金力学与磁学性能的影响

针对FeCo-2V-0.5Cr软磁合金,研究了真空热处理时间对其微观组织结构、力学与磁学性能的影响规律,发现在800℃下热处理时间为2h左右时,合金的抗拉强度和延伸率达到最佳,同时仍保持良好的软磁性能,抗拉强度、延伸率以及矫顽力分别为867.8MPa、10.4%以及2.0Oe。进一步对该合金进行附加磁场下的真空热处理,重点研究了合金的交流损耗与矫顽力随附加磁场方式包括磁场撤除温度与磁场下保温时间的变化规律,发现适当的磁场热处理对合金相关力学性能影响不大,但由于合金中产生了单轴各向异性而使合金矫顽力进一步降至1.6Oe。     

无人机高速DS/FH混合扩频通信系统关键模块设计

针对UAV(Unmanned Aerial Vehicle,无人机)测控链路高抗干扰需求,给出了实现跳频速率20 000次/s的扩跳混合无人机测控数据链系统实现方案.系统采用跳频频率并行捕获模式.跳频源设计采用直接频率合成、DDS(Direct Digital Synthesis,直接数字频率合成)和PLL (Phase-Locked Loop,锁相环)相结合的混合频率合成技术.利用相位响应滤波器,通过正交调制技术完成MSK(Minimum Shift Keying,最小频移键控)、GMSK (GaussianMinimum Shift Keying,高斯最小频移键控)调制.通过推导得出2 bit差分解调输出与载波频率选择有关,且为四分之数据率的整数倍关系.然后通过实例分析给出了跳频频率间隔选取方法,即跳频间隔应当将临近跳频的主瓣分开,同时跳频载波频率应当设在其他跳频频谱的零点处.最后总结了高速扩跳频系统参数设计一般步骤.     

纸基蜂窝模块化固持方法研究

 基于磁场与摩擦学蜂窝芯材料固持原理,提出复杂型面纸基蜂窝零件固持平台的模块化设计思想。运用移动模块、固定模块、模块夹具以及导磁体和隔磁体解决了该原理中磁路控制问题,实现了复杂曲面零件在模块化固持平台上的加工固持。通过理论分析和有限元仿真研究了固持系统中蜂窝孔格的受力,分析了固持系统的特点和可靠性,以及永磁体厚度、固定平台高度、铁粉填充高度和平台间隙对磁场力的影响规律。实验与仿真结果表明,模块化固持平台能够满足复杂曲面蜂窝铣削加工的固持要求。     

构件低周疲劳损伤的金属磁记忆检测试验研究

对18CrNi4A钢缺口试件在三级应力水平下进行了低周疲劳试验和磁记忆信号检测,研究应力集中、疲劳损伤及疲劳应力对磁信号的影响规律。结果表明,利用磁信号Hp(y)曲线突变特征和磁信号梯度K曲线异变峰特征可表征试件损伤位置;采用H′p(y)=Hp(y)N-Hp(y)0的磁信号处理方式,磁信号H′p(y)曲线过零点与试件断裂位置重合,处理后的磁信号过零法可更有效的表征试件损伤位置;磁信号梯度Kmax值随疲劳损伤程度的增加而逐渐增加,反映了构件疲劳损伤程度,可表征试件疲劳损伤程度;磁信号与疲劳应力水平存在强烈的相关性,应力水平越大,磁信号值也越大。     

磁悬浮反作用飞轮速率模式控制系统设计

针对磁悬浮反作用飞轮干扰力矩对输出力矩精度的影响,提出了一种速率模式数字控制方法,实现了正向加速、正向减速、反向加速、反向减速的四象限高精度稳定的转速跟踪控制,减速时,高速段利用飞轮储存的动能进行能耗制动,低速时进行反接制动,从而实现磁悬浮反作用飞轮速率模式控制.     

异种金属材料磁脉冲焊接技术

通过对磁脉冲焊接技术结合机理的阐述,采用5A03Al-5A06Al、1050Al-AZ31Mg异种金属材料进行焊接试验.对所得的焊接接头进行气密性试验和剥离试验,检测其结合质量;结合光学显微镜,对比分析Al-Al、Al-Mg焊接接头的微观形貌特点;并采用SEM/EDS分析界面附近的元素分布;最后通过硬度试验,检测接头界...     

高精度光纤IMU的磁屏蔽方法及实验研究

惯性测量单元(IMU)是位置姿态系统(POS)的核心部分,IMU的精度很大程度上决定着POS精度.由于高精度光纤陀螺(FOG)的光纤线圈对磁场敏感,基于高精度FOG的IMU精度会受磁场影响而降低.本文研究了FOG磁敏感性机理,通过实验得出高精度光纤IMU对磁场敏感的结论.采用电磁场有限元分析软件Ansoft Maxwe...     

多部件组合体分块网格生成技术及应用

给出多部件组合体分块网格生在的一种方案及实践,包括交界面网格生成技术、空间网格生成方法及质量控制。以一个平尾和机翼具有一定高度差的机身－机翼－平尾－立尾组合体外形为例,生成与公共交界面或边界面正交或接近正交的分块网格。用于Ｅｕｌｅｒ方程跨声速来流几个迎角的计算,结果与实验符合较好。     

Relationship Between Substorm Auroras and Processes in the Near-Earth Magnetotail

Although the auroral substorm has been long regarded as a manifestation of the magnetospheric substorm, a direct relation of active auroras to certain magnetospheric processes is still debatable. To investigate the relationship, we combine the data of the UV imager onboard the Polar satellite with plasma and magnetic field measurements by the Geotail spacecraft. The poleward edge of the auroral bulge, as determined from the images obtained at the LHBL passband, is found to be conjugated with the region where the oppositely directed fast plasma flows observed in the near-Earth plasma sheet during substorms are generated. We conclude that the auroras forming the bulge are due to the near-Earth reconnection process. This implies that the magnetic flux through the auroral bulge is equal to the flux dissipated in the magnetotail during the substorm. Comparison of the magnetic flux through the auroral bulge with the magnetic flux accumulated in the tail lobe during the growth phase shows that these parameters have the comparable values. This is a clear evidence of the loading–unloading scheme of substorm development. It is shown that the area of the auroral bulge developing during substorm is proportional to the total (magnetic plus plasma) pressure decrease in the magnetotail. These findings stress the importance of auroral bulge observations for monitoring of substorm intensity in terms of the magnetic flux and energy dissipation.     

Geoeffectivity of Coronal Mass Ejections

Coronal mass ejections and post-shock streams driven by them are the most efficient drivers of strong magnetospheric activity, magnetic storms. For this reason there is considerable interest in trying to make reliable forecasts for the effects of CMEs as much in advance as possible. To succeed this requires understanding of all aspects related to CMEs, starting from their emergence on the Sun to their propagation to the vicinity of the Earth and to effects within the magnetosphere. In this article we discuss some recent results on the geoeffectivity of different types of CME/shock structures. A particularly intriguing observation is that smoothly rotating magnetic fields within CMEs are most efficient in driving storm activity seen in the inner magnetosphere due to enhanced ring current, whereas the sheath regions between the shock and the ejecta tend to favour high-latitude activity.