水下地磁场测量中载波干扰的地磁补偿研究

Zhao Yi-chao, Kang Chong, Fan Li-ming, Liu Yu-yuang, Zhang Xiao-jun
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引用次数: 3

摘要

本文对水下磁载波效应的补偿进行了研究。利用拖曳式磁强计(G882)在水体中进行测量,根据测量结果、地磁倾角和地磁偏角计算磁场的3个分量,建立补偿模型。然后根据另一种测量结果(结合载波的CS-L测量)将这两种数据都代入理论补偿方程,得到补偿系数。目前,已经得出了实验水的真实补偿方程。利用这两种磁强计在其他开阔水域进行测量,可获得两组新测量数据。为了将Cs-l得到的数据代入新建立的实际方程,计算了补偿后的水场数据。然后将这三种数据画在一起,就可以观察到补偿的结果。从图中可以验证这种补偿方式的可靠性。这种方法较好地减小了磁强计与载流子组合时载流子对磁强计的干扰,并拓宽了载流子对磁强计干扰的应用范围。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Research of Geomagnetic Compensation for the Interference which is Caused by Carrier in the Underwater Geomagnetic Field Measurement
This article is about compensating for the effect of underwater magnetic carrier. Using the dragging type magnetometer(G882) to measure in the water's field, and calculating the 3 components of magnetic field according the measuring result, geomagnetic inclination and geomagnetic declination, and then establishing a compensating model. And then according another result (measured by the CS-L which is combined with the carrier) putting all the 2 data into the theory compensating equation to get the compensating coefficient. For now, the real compensating equation for the experimental water has been come out. Using both of the 2 types of magnetometers to survey in the other open water field, 2 groups of the newly measured data can be obtained. To substitute data (obtained by Cs-l) into the real newly established equation, the compensated data of the water field have been calculated. Then drawing a figure which contained all the 3 kinds of data together, the result of this compensation can be observed. From the figure, the reliability of this compensation's way has been verified. This sort of approach is a better way to reduce the interference caused by the carrier when the magnetometer is combined with the carrier and to widening the applied range for the way of reducing the interference caused by the carrier.
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