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Developments in frequency domain AEM; tackling drift and noise with a multicomponent, ferrite-core, receiver tipplet

机译:频域aEm的发展;使用多组分铁氧体磁芯接收器接头来解决漂移和噪声问题

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摘要

The polar oceans' sea ice cover is a challenging geophysical target to map. Current state of practice helicopter-electromagnetic (HEM) ice thickness mapping is limited to 1D interpretation due to common procedures and systems that are mainly sensitive to layered structures. We present a new generation Multi-sensor, Airborne Sea Ice Explorer (MAiSIE) to overcome these limitations. As the actual sea ice structure is 3D and in parts heterogeneous, errors up to 50% are observed due to the common 1D approximation. With MAiSIE we present a new EM concept based on one multi frequency transmitter loop and a three component receiver coil triplet without bucking The small weight frees additional payload to include a line scanner (lidar) and high accuracy INS/dGPS. The 3D surface topography from the scanner with the EM data at from 500 Hz to 8 kHz, in x, y, and z direction, will increase the accuracy of HEM derived pressure ridge geometry significantly. Experience from two field campaigns shows the proof-of-concept with acceptable sensor drift and receiver sensitivity. The preliminary 20 ppm noise level @ 4.1 kHz is sufficient to map level ice thickness with 10 cm precision for sensor altitudes below 13 m.
机译:极地海洋的海冰覆盖是一个极具挑战性的地球物理目标。由于通用的程序和系统主要对分层结构敏感,因此目前的实践状态直升​​机电磁(HEM)冰厚映射仅限于一维解释。我们提出了新一代的多传感器机载海冰探测器(MAiSIE),以克服这些限制。由于实际的海冰结构是3D的,并且部分是异质的,由于常见的1D逼近,观察到的误差高达50%。借助MAiSIE,我们提出了一种新的EM概念,该概念基于一个多频发射器环路和一个三分量接收线圈三重态而不会失压。小巧的重量释放了额外的有效载荷,包括了行扫描器(激光雷达)和高精度INS / dGPS。扫描仪在x,y和z方向上使用EM数据为500 Hz至8 kHz的3D表面形貌将显着提高HEM衍生的压力脊几何形状的精度。两次野战的经验表明,该概念证明具有可接受的传感器漂移和接收器灵敏度。初始的20 ppm噪声水平@ 4.1 kHz足以在13 m以下的传感器高度上绘制10 cm精度的水平冰厚。

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