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Sensors
  • Correction
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20 June 2012

Correction: Renaudin, V. et al. Use of Earth’s Magnetic Field for Mitigating Gyroscope Errors Regardless of Magnetic Perturbation. Sensors 2011, 11, 11390-11414

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Department of Geomatics Engineering, Schulich School of Engineering, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4, Canada
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This article belongs to the Section Physical Sensors
Although the equations' derivation in our paper published in Sensors 2011 [1] is correct, a typo has been found in the summarizing Equations (48) and (49). The dot on the B in the skew matrix should be removed. Equations (48) and (49) should be corrected as:
δ B ˙ Q S F k + 1 b = [ 0 3 × 3 [ B Q S F k + 1 b × ] ] [ ɛ n δ b ω ] + [ 0 1 × 3 0 1 × 3 0 1 × 3 [ ω ^ B b × ] ] [ 0 3 × 1 η B ]
[ δ B Q S F k + 1 n δ B ˙ Q S F k + 1 b ] δ z = [ [ B Q S F k n × ] 0 3 × 3 0 3 × 3 [ B Q S F k + 1 b × ] ] H QSF [ ɛ n δ b ω ] δ x + [ C b n ω ^ B b ] η B

Reference

  1. Afzal, M.H.; Renaudin, V.; Lachapelle, G. Use of Earth's Magnetic Field for Mitigating Gyroscope Errors Regardless of Magnetic Perturbation. Sensors 2011, 11, 11390–11414. [Google Scholar]

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