共查询到17条相似文献,搜索用时 109 毫秒
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1 前言自从对 IMP 和 OGO 卫星系统和部件进行磁试验以来,退磁已经做为一种把试验物体恢复到近零的原始磁状态的方法。1962年和1963年间,在部件磁试验设备(CMTF)中使用了直流退磁。近此时候完成的退磁试验是用60Hz 交流磁场退磁,代替了直流退磁。在一般的情况下,用初始磁场强度等于材料的矫顽力的磁场强度为铁磁材料退磁,肯定会退掉由材料磁性饱和引起的剩磁。 相似文献
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卫星地面磁测量是卫星环境试验的一个重要组成部分,精确的磁测量必须磁场或可控磁场中做。在没有大型磁设备的情况下,提出在地磁场中做磁测量题。本文分析了在地磁场中做磁测量的特点和影响测量精度的因素,指出了在场中做磁测量的应用范围,测量方法及在测量中应注意的问题,给出了在地磁做磁矩测量的几个试验测量结果。 相似文献
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这篇文章描述了在位于 Malibu 的 TRW Malibu 磁试验设备中完成的 OGO 和 ERS 卫星磁特性的试验结果和使用的试验方法。最关心的卫星磁特性是在星载磁探测器位置处的卫星磁场,包括永磁场和感磁场。同时还关心星的"硬"磁场,即永磁场的大小和可以被一般磁化环境引起变化的"软"磁场的大小。一般磁化环境是指卫星在发射进入轨道前,会遇到的磁化环境。另外关心的磁特性是卫星磁场的分布图和位于卫星中心的偶极子矩和高阶的多极子矩,其中包括永磁矩和感磁矩。Malibu 试验室由安装在地下室6.4m 的三轴 Fanselau—Braunbeck 线圈系统和一些试验楼组成。转台位于其中的一座试验楼里,在这座试验楼里给卫星做没有线圈的磁试验。例如,OGO 卫星太大了,不能放入 Fanselau—Braunbeck 线圈系统中,因此就在此试验楼里进行试验。有线圈和没有线圈的试验方法是将卫星相对于固定的三轴磁通门探测器进行两轴旋转。旋转周期要比能觉察到的环境地磁场的变化周期短。可用一个远距离的探测器对地磁场的变化进行补偿,来满足上述的要求。磁通门探测器的输出由多通道 Sanborn 记录仪和 X—Y绘图仪记录,X—Y绘图仪可以立即按比例绘制旋转平面的磁矩大小,还可以给出在卫星座标系中的磁矩方向。卫星再绕另一相互垂直正交轴旋转,记录其数据。从这些数据中可以得到的总的磁矩矢量。ERS 卫星是一个280mm 的八面体,所以很容易将其放入 Fanselau—Braun-beck 线圈系统。在线圈系统中能够分别测量卫星场永磁分量和感磁分量。 相似文献
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针对现有洛伦兹力磁轴承功耗较高、工作气隙磁场非均匀性问题,提出一种基于组合磁钢叠加磁场的新型洛伦兹力磁轴承设计方法。首先建立了传统洛伦兹力磁轴承电磁力矩模型,揭示了洛伦兹力磁轴承功耗和控制精度与其磁场性能之间的对应关系。在此基础上,引入了磁场强度均值和磁场均匀度的概念,并以此为依据设计出一种轴向整环充磁磁钢与径向分块充磁磁钢组合工作的新型方案。其中轴向充磁磁钢产生主磁场,保证工作气隙周向均匀性,辅助以径向充磁磁钢,使磁场主要聚集在工作气隙处。相比现有洛伦兹力磁轴承,在相同尺寸约束条件下,新型洛伦兹力磁轴承径向磁场均匀度提升了8.7%,磁场强度提升了51.8%,周向磁场连续性显著提高。仿真结果表明,新型洛伦兹力磁轴承可以有效降低功耗、提升控制精度,研究成果可为研制超高精度磁悬浮惯性机构提供一条新的技术途径。 相似文献
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地磁环境下卫星磁试验中的外干扰磁场控制补偿方法 总被引:1,自引:1,他引:0
针对地磁环境下外干扰磁场影响卫星磁试验精度问题,综合分析外干扰源场和卫星近场特性;通过合理布局(包括位置和方式)外干扰磁场监测传感器和卫星磁场采集传感器,增设动态磁场采集的A/D取样扫描频率循环控制、信号统计、滤波、数据拟合等信号处理功能,解决了监测传感器和采集传感器所得到的干扰信号的同步性、等效性、一致性,以及采集传感器信号中卫星真实磁场与干扰磁场之间的不相干性;实现了卫星磁试验的外干扰磁场有效闭环控制、自动跟踪、补偿和修正。通过24 h实时监测,外干扰磁场波动控制在0.5~1.0 n T范围内,获得地磁环境下卫星24 h"准零磁"环境磁试验条件,满足卫星磁试验对磁环境的技术要求。 相似文献
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A. A. Tikhonov 《Cosmic Research》2002,40(2):157-162
When solving problems related to the induction of the Earth's magnetic field, the potential of which is expressed in the form of a series of spherical harmonic functions, it is necessary to use an approximate model of the geomagnetic field that satisfies the two conflicting requirements of simplicity and accuracy. As is noted in [3, p. 10], at the stage of design of satellites, especially at the stage of preliminary analysis of their dynamics, simple models of the geomagnetic field are usually employed. This offers additional possibilities for theoretical analysis of the problem. The averaged model and the model of a right dipole are just such simple models. The quadrupole model of the geomagnetic field developed in [4] is more accurate, but also more complex. The model of an oblique or skewed dipole is intermediate. The quadrupole model generalizes the simpler models mentioned above, and its analysis allows estimation of the accuracy of each model. It turns out that the oblique dipole model, which differs from the model of a right dipole by small correcting terms, does not take into account other correcting terms caused by the quadrupole part of the geomagnetic field, which are greater in magnitude. The evolution of the rotary motion of a charged rigid body in the geomagnetic field is considered, and the incorrectness of the oblique dipole model is demonstrated. The effect of the quadrupole component of the geomagnetic field on the body dynamics is revealed. 相似文献
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The relationship between proton aurora and geomagnetic pulsations Pc1, which are an indicator of development of ion-cyclotron instability in the equatorial magnetosphere, are studied on the basis of the observations of proton aurora from the IMAGE satellite, observations of particle fluxes onboard the low-orbiting NOAA satellites, and geomagnetic pulsation observations at the Lovozero observatory. A conclusion is drawn that the subauroral spots in the proton emission projected into the magnetosphere near the plasmapause are two-dimensional images at the ionospheric “screen” of the region of intense scattering of energetic protons into the loss cone at the development of an ion-cyclotron instability. 相似文献
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Magnetic Storms in October 2003 总被引:1,自引:0,他引:1
《Cosmic Research》2004,42(5):489-535
Preliminary results of an analysis of satellite and ground-based measurements during extremely strong magnetic storms at the end of October 2003 are presented, including some numerical modeling. The geosynchronous satellites Ekspress-A2and Ekspress-A3, and the low-altitude polar satellites Coronas-F and Meteor-3M carried out measurements of charged particles (electrons, protons, and ions) of solar and magnetospheric origin in a wide energy range. Disturbances of the geomagnetic field caused by extremely high activity on the Sun were studied at more than twenty magnetic stations from Lovozero (Murmansk region) to Tixie (Sakha-Yakutia). Unique data on the dynamics of the ionosphere, riometric absorption, geomagnetic pulsations, and aurora observations at mid-latitudes are obtained. 相似文献
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The stabilization of a magnetically oriented satellite is treated from a new standpoint. Under the assumption of a uniform magnetic field, the system stability is discussed. By imposing a performance criterion, a damping control law is derived. Stabilization characteristics are analyzed using a more realistic geomagnetic field model. The practical approximate methods of the damping control are sought, and their characteristics are analyzed. Finally the flight results of the recent satellites using an approximate method are presented. 相似文献
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The large and sharp changes of solar wind dynamic pressure, found from the INTERBALL-1 satellite and WIND spacecraft data, are compared with simultaneous magnetic field disturbances in the magnetosphere measured by geosynchronous GOES-8, GOES-9, and GOES-10 satellites. For this purpose, about 200 events in the solar wind, associated with sharp changes of the dynamic pressure, were selected from the INTERBALL-1 satellite data obtained during 1996–1999. The large and sharp changes of the solar wind dynamic pressure were shown to result in rapid variations of the magnetic field strength in the outer magnetosphere, the increase (drop) of the solar wind dynamic pressure always lead to an increase (drop) of the geosynchronous magnetic field magnitude. The value of the geomagnetic field variation strongly depends on the local time of the observation point, reaching a maximum value near the noon meridian. It is shown that the direction of the B z component of the interplanetary magnetic field has virtually no effect on the geomagnetic field variation because of a sharp jump of pressure. The time shift between an event in the solar wind and its response in the magnetosphere at a geosynchronous orbit essentially depends on the inclination of the front of a solar wind disturbance to the Sun-Earth line. 相似文献