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Magnetic distortion in motion labs, implications for validating inertial magnetic sensors.

机译:运动实验室的磁畸变对验证惯性磁传感器的意义。

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BACKGROUND: Ambulatory 3D orientation estimation with Inertial Magnetic Sensor Units (IMU's) use the earth magnetic field. The magnitude of distortion in orientation in a standard equipped motion lab and its effect on the accuracy of the orientation estimation with IMU's is addressed. METHODS: Orientations of the earth magnetic field vectors were expressed in the laboratory's reference frame. The effect of a distorted earth magnetic field on orientation estimation with IMU's (using both a quaternion and a Kalman fusing algorithm) was compared to orientations derived from an optical system. FINDINGS: The magnetic field varied considerably, with the strongest effects at 5 cm above floor level with a standard deviation in heading of 29 degrees , decreasing to 3 degrees at levels higher than 100 cm. Orientation estimation was poor with the quaternion filter, for the Kalman filter results were acceptable, despite a systematic deterioration over time (after 20-30s). INTERPRETATION: Distortion of the earth magnetic field is depending on construction materials used in the building, and should be taken into account for calibration, alignment to a reference system, and further measurements. Mapping the measurement volume to determine its ferromagnetic characteristics in advance of planned experiments can be the rescue of the data set. CONCLUSIONS: To obtain valid data, "mapping" of the laboratory is essential, although less critical with the Kalman filter and at larger distances (>100 cm) from suspect materials. Measurements should start in a "safe" area and continue no longer than 20-30s in a heavily distorted earth magnetic field.
机译:背景:带有惯性磁传感器单元(IMU)的动态3D方向估计使用地磁场。解决了在配备标准设备的运动实验室中取向失真的程度及其对使用IMU进行取向估计的准确性的影响。方法:在实验室参考系中表达了地球磁场矢量的方向。将变形的地球磁场对使用IMU(同时使用四元数和卡尔曼融合算法)进行方位估计的影响与从光学系统得出的方位进行了比较。结果:磁场变化很大,在离地面5 cm处的影响最强,航向标准偏差为29度,在100 cm以上的水平处下降至3度。尽管随着时间(在20到30秒后)系统地退化,但四元数滤波器的方向估计效果不佳,因为卡尔曼滤波器的结果是可以接受的。解释:地磁场的失真取决于建筑物中使用的建筑材料,在校准,与参考系统对齐以及进行进一步测量时,应将其考虑在内。在计划的实验之前对测量体积进行映射以确定其铁磁特性可以挽救数据集。结论:为了获得有效的数据,实验室的“映射”是必不可少的,尽管对卡尔曼滤波器的要求不那么严格,并且距可疑材料的距离较大(> 100 cm)。测量应在“安全”区域开始,并在严重失真的地磁场中持续不超过20-30s。

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