4.7 Article

Trust-Region Solver of a Nonlinear Magnetometer Disturbance Estimation Problem

Journal

IEEE SENSORS JOURNAL
Volume 21, Issue 20, Pages 22569-22577

Publisher

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/JSEN.2021.3092678

Keywords

Magnetometers; Optimization; Sensors; Linear programming; Estimation; Real-time systems; Magnetic sensors; Magnetometer; disturbance estimation; trust-region method; computational efficiency; navigation

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The study addressed the real-time magnetometer disturbance estimation problem by introducing the trust-region method to improve underwater navigation accuracy. The main challenge lies in finding feasible regions of possible solutions, with geometric analysis and algebraic elimination providing globally optimal solutions. Experimentations confirmed the correctness of the proposed method, showing that the trust-region technique can efficiently estimate high-frequency dynamic magnetic disturbances.
Earth geomagnetic field provides very important information for autonomous navigation. However, in practice, magnetometer measurements are easily distorted by outer disturbances, as shown in the right diagram. In a recent study, the real-time magnetometer disturbance estimation problem has been solved via a constrained nonlinear programming for better underwater navigation accuracy. However, the employed interior-point optimizer will require considerable computational resources and cannot always guarantee optimality during optimization updates. This paper further investigates this problem and refines the solution by introducing the trust-region method. The challenge of the designed approach mainly falls into finding out the feasible regions of the possible solutions. Geometric analysis and algebraic elimination methods are taken into account to give globally optimal solutions to the trust-region solver. Experimentations are conducted to verify the correctness of the proposed method. Moreover, it is also confirmed that the trust-region technique can continuously and accurately propagate so that high-frequency dynamic magnetic disturbances can be efficiently estimated.

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