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RS-HC3海洋全张量磁梯度系统及其应用 被引量:1
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作者 赵瑜 张瑾 邓瑞辉 《海洋测绘》 2014年第2期25-27,共3页
介绍了一套海洋全张量磁梯度系统,专门用于测量地球磁场三分量数据及张量磁力梯度数据,并实时采集设备的定位信息及姿态信息,以便于后续数据处理。系统由两组三分量磁力仪、惯导设备、GPS定位设备、温度/压力传感器等组成,特别适用于测... 介绍了一套海洋全张量磁梯度系统,专门用于测量地球磁场三分量数据及张量磁力梯度数据,并实时采集设备的定位信息及姿态信息,以便于后续数据处理。系统由两组三分量磁力仪、惯导设备、GPS定位设备、温度/压力传感器等组成,特别适用于测量地磁场矢量空间的磁场变化率,在磁法勘探中的解释效果明显优于单探头标量测量和三探头标量梯度测量。 展开更多
关键词 海洋磁力测量 磁力 惯导设备 张量磁力梯度
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Multi-spacecraft observations of earthward flow bursts 被引量:8
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作者 MA YuDuan CAO JinBin +3 位作者 REME Henry DANDOURAS Iannis DUNLOP Malcolm LUCEK Elisabeth 《Science China(Technological Sciences)》 SCIE EI CAS 2012年第5期1305-1311,共7页
On the basis of the plasma, electric and magnetic fields jointly observed by Cluster and the Double Star TC-I spacecraft in the Earth's magnetotail, we have investigated the earthward flow bursts by introducing the m... On the basis of the plasma, electric and magnetic fields jointly observed by Cluster and the Double Star TC-I spacecraft in the Earth's magnetotail, we have investigated the earthward flow bursts by introducing the momentum equation in the X-direction in the ideal conditions of magneto hydrodynamics (MHD). One earthward flow burst with a peak in excess of 500 km/s was selected, when the four spacecraft of Cluster were located around -16 RE and TC-1 was located around -10 RE in the X-direction. The inter-spacecraft distances in Y and Z directions were smaller than the statistical spatial scales of the bursty bulk flows. When the Y components of E and -VxB were compared, there was no clear breakdown of the frozen-in condition during the earthward flow burst. With the measured plasma and magnetic parameters from two spacecraft at different positions in the magnetotail, the X component of the pressure gradient was calculated. Magnetic tension was calculated using the mag- netic field measured at four points, which could be compared with the assumed constant in the past research with single satel- lite. When the pressure gradient and the magnetic tension were put into the MHD momentum equation, some samples of the earthward flow bursts were accelerated and some were decelerated. The braking process of the earthward flow burst was more complicated than what the past results had shown. The accelerated samples accounted for about one third of the whole earth- ward flow bursts and discontinuously located among the decelerated elements. The original single earthward flow burst event might be split into several short flow bursts when it was moving to the Earth. Our results may partly illustrate that the duration of fast flows during three phases of substorm becomes short near the Earth. The results are consistent with the past results that fast flows intrude to places earthward the typical braking region. 展开更多
关键词 flow burst pressure gradient magnetic tension BRAKING
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