共查询到15条相似文献,搜索用时 140 毫秒
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为准确描述和评估航天器的磁特性,建立航天器网格化磁模型,提出航天器磁场信息成像方法。利用立体阵列扫描系统,对航天器测量面的磁场信息进行采集和计算,联合磁梯度张量的模量极值和欧拉反演法确定其内部磁源的水平位置和深度,实现航天器内部、探测面和空间磁信息的可视化分析和展示。航天器模型(格距10 cm)三点磁源试验和计算结果显示,该方法对内部磁源单方向定位偏差小于0.05 m,单方向磁矩偏差小于0.02 A?m2;空间磁场强度和磁矩误差均小于5%。该方法为快速获取类长方体形航天器的磁信息提供了一种新的工程实践手段。 相似文献
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为解决大尺度、大磁矩航天器磁性测量时采用常规近场测试方法带来的整器磁矩偏心误差大、无法获得有效磁矩的难题,采用在航天器几何赤道面上下典型区域多层次布局传感器的方式获得整器柱面静态磁场数据。按10?1器模比例建立航天器垂向标准磁偶极子、双磁偶极子和组合态多磁偶极子磁矩分布模型,按上述多层分布测试方法对标准模型进行仿真试验。结果表明:在异向双磁偶极子和多磁偶极子模型中,当传感器位置高度逼近模型垂向磁赤道区域时,获得的结果更接近模型预置的标准磁矩量值;整器垂向磁性分布特征与异向多极子模型2具有高度相似性,进一步证明航天器磁赤道区域测得的结果更真实代表了垂向磁矩量值。该方法极大地提高了大磁矩航天器整器垂向磁矩准确性及其裕度控制范围。 相似文献
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为了提高无人机航空磁探测精度,文章利用大疆六旋翼无人机作为飞行平台,搭载三轴磁通门传感器及相应的数据采集子系统,组建了旋翼无人机磁场测量系统;分析和测量了六旋翼无人机本底磁性分布特征,优化了无磁伸杆的安装位置;采用综合系数法修正了三轴磁通门传感器的误差;最后进行了野外飞行试验,对旋翼无人机磁测系统的整体性能进行验证。结果表明,系统可持续飞行15 min,可有效完成低空磁场探测和磁矩计算,且飞行稳定性能高。文章进一步提出了技术改进方向。该研究可为无人机磁探技术和工程应用提供参考。 相似文献
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卫星磁性仿真模型建立 总被引:1,自引:0,他引:1
卫星的磁性仿真主要包括卫星的磁矩仿真计算和卫星周围磁场的仿真计算.这两种仿真计算都是利用卫星部件的实际测量结果对卫星整星的磁矩及周围磁场进行预估.这些预估结果对于卫星整星的磁性设计、磁性测量、磁补偿起到指导作用,对于卫星的磁性控制有重要意义. 相似文献
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为了对磁偶极子进行高精度的磁性定位,文章从磁偶极子模型出发,推导出磁偶极子的空间坐标与其产生的磁场及磁场梯度之间的关系式;针对模型及关系式,设计了一种全张量磁场梯度传感器,能够一次测量出精确定位所需的9个磁场梯度值和3个磁场强度值;对比仿真结果和实验结果,发现二者具有较好的一致性,证明了该理论模型的有效性。对于磁偶极子,用半径为0.05 m的梯度传感器对磁矩为2 A·m~2的磁偶极子进行定位测量,在0.5~1 m距离内定位误差不大于10%。文章还对定位测量误差的原因进行了分析,包括梯度测量基线距离及传感器半径对定位误差的影响。 相似文献
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航天器长期在轨运行期间,空间磁场与其自身磁矩相互作用的累积,会对航天器的姿态造成较大影响,加重姿态控制系统负担,降低航天器的可靠性。文章分别针对航天器轨道计算及地磁场模型的使用,对航天器地磁干扰力矩数值的仿真进行了系统的研究,最终得到航天器在轨运行时地磁干扰力矩计算仿真方法。 相似文献
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The results of reconstructing the uncontrolled rotational motion of the Aist small spacecraft prototype during its flight in early 2014 have been presented. The reconstruction was carried out by processing data from onboard measurements of the Earth’s magnetic field. The processing procedure used portions of data covering intervals of time with durations ranging from a few dozen minutes to three hours. Data obtained in each such interval were processed jointly by the least-squares method by integrating the equations of the satellite motion relative to the center of mass. The initial conditions of the motion and the parameters of the used mathematical model during processing have been estimated. The results of processing for several data intervals have provided a fairly complete picture of the satellite motion. This was the weakly disturbed Euler–Poinsot motion. 相似文献
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Based on the results of plasma and magnetic measurements at three different points of the heliosphere and telescopic observations
of the Sun from these points we study simultaneously high-speed streams (HSS) of the solar wind (SW) near the Earths’s orbit
and coronal holes (CH) that have generated them. The data from spacecraft STEREO-A, STEREO-B, ACE, and SOHO are used together with ground-based observations from March 2007 to May 2008. In this period there existed HSS whose sources
represented CH of various polarity, geometry, and location relative to the heliographic and heliomagnetic equators. Dependence
of SW parameters on mutual positions of spacecraft with respect to CH and heliospheric current sheet, and also on heliolatitude
and geometry of the CH is revealed. A difference of more than 5° in locations of spacecraft with respect to the heliospheric
current sheet in November 2007 allowed us to discover a heliolatitude velocity gradient of the SW streams between the STEREO-A and STEREO-B spacecraft. On the average this gradient at that time was equal to 20 km/s per degree. Substantial variations in SW streams
associated with variations of the HSS SW sources during a few hours or days were also observed. This variability makes it
difficult to use the data of spacecraft STEREO-B for sufficiently accurate prediction of SW properties in the near-Earth space by the method of simple advanced ti me shift
due to heliolongitude difference between a spacecraft and the Earth even in solar activity minimum. 相似文献