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

被引:220
作者
de Vries, W. H. K. [1 ,2 ]
Veeger, H. E. J. [1 ,3 ]
Baten, C. T. M. [2 ]
van der Helm, F. C. T. [1 ]
机构
[1] Delft Univ Technol, Dept Biomed Engn, Fac Mech Maritime & Mat Engn, NL-2600 AA Delft, Netherlands
[2] Roessingh Res & Dev, Enschede, Netherlands
[3] Vrije Univ Amsterdam, Dept Human Movement Sci, Res Inst MOVE, Amsterdam, Netherlands
关键词
Inertial magnetic sensing; Magnetic distortion; Orientation estimation; Kalman filter;
D O I
10.1016/j.gaitpost.2008.12.004
中图分类号
Q189 [神经科学];
学科分类号
071006 ;
摘要
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 20-30 s). 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 20-30 s in a heavily distorted earth magnetic field. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:535 / 541
页数:7
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