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The influence of the Earth's magnetic field on strapdown inertial gravimetry using Q-Flex accelerometers: static and dynamic experiments

机译:地球磁场对Q-Flex加速度计的轴向惯性重量的影响:静态和动态实验

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摘要

In recent strapdown airborne and shipborne gravimetry campaigns with servo accelerometers of the widely used Q-Flex type, results have been impaired by heading-dependent measurement errors. This paper shows that the effect is, in all likelihood, caused by the sensitivity of the Q-Flex type sensor to the Earth's magnetic field. In order to assess the influence of magnetic fields on the utilised strapdown IMU of the type iMAR iNAV-RQH-1003, the IMU has been exposed to various magnetic fields of known directions and intensities in a 3-D Helmholtz coil. Based on the results, a calibration function for the vertical accelerometer is developed. At the example of five shipborne and airborne campaigns, it is outlined that under specific circumstances the precision of the gravimetry results can be strongly improved using the magnetic calibration approach: The non-adjusted RMSE at repeated lines decreased from 1.19 to 0.26 mGal at a shipborne campaign at Lake Muritz, Germany. To the knowledge of the authors, a significant influence of the Earth's magnetic field on strapdown inertial gravimetry is demonstrated for the first time.
机译:在最近的塞子空气传播和船载重力运动中具有广泛使用的Q-Flex类型的伺服加速度计,通过依赖依赖性测量误差损害了结果。本文表明,在所有可能性中,效果是由Q-Flex型传感器到地球磁场的敏感性引起的。为了评估磁场对IMAR型INAV-1003的利用刻度IMU的影响,IMU已经暴露于3-D亥姆霍兹线圈中的已知方向和强度的各种磁场。基于结果,开发了垂直加速度计的校准函数。在五个船载和空中运动的例子中,概述了,在特定情况下,可以使用磁校准方法强烈改善重食结果的精度:重复线的未调整RMSE在船上的1.19降至0.26 mgal在德国默特茨湖的运动。对于作者的知识,第一次对地球磁场对围绕惯性重力的显着影响。

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