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A HTS rf SQUID vector magnetometer for geophysical exploration

机译:用于地球物理勘探的HTS射频SQUID矢量磁力仪

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摘要

We report on a highly sensitive rf SQUID vector (x, y, z) magnetometer system operating at 77 K and suitable for electromagnetic geophysical exploration. We achieved stable long-term operation of all three channels during field trials outside magnetic shielding in urban and rural environments. With sensors on 10×10 mm2 substrates, the white noise level in earth's field was 40 fT/√Hz above 100-300 Hz, in all three channels. The new system meets the high requirements for slew rate (>2 mT/s), dynamic range (>130 dB) and bandwidth (20 kHz) which must be fulfilled in geophysical measurements, especially the TEM (transient electromagnetic) method. We also present results of geophysical TEM field trials over various test sites. We obtained good reproducibility of SQUID data and a good correlation between output signals of reference induction coils and the derivative of SQUID signals. Results from TEM measurements indicate that for late time signals, originating from deeper geological structures, the SQUID magnetometer provides a better signal-to-noise ratio than an induction coil
机译:我们报告了一个高灵敏度的射频SQUID矢量(x,y,z)磁力计系统,工作频率为77 K,适用于电磁地球物理勘探。在城乡环境中的电磁屏蔽以外的现场试验期间,我们实现了所有三个通道的稳定长期运行。在10×10 mm2的基板上安装传感器时,在所有三个通道中,高于100-300 Hz时,地场中的白噪声电平均为40 fT /√Hz。新系统满足了对斜率(> 2 mT / s),动态范围(> 130 dB)和带宽(20 kHz)的高要求,这些要求在地球物理测量中必须满足,尤其是TEM(瞬变电磁)方法。我们还将介绍在各个测试地点进行的地球物理TEM现场试验的结果。我们获得了SQUID数据的良好重现性,并且参考感应线圈的输出信号与SQUID信号的导数之间具有良好的相关性。 TEM测量结果表明,对于较晚的信号,其起源于更深的地质结构,SQUID磁力计比感应线圈提供更好的信噪比

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