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Sensors 2014, 14(5), 8485-8504; doi:10.3390/s140508485
Published: 14 May 2014
Abstract: A complete error calibration model with 12 independent parameters is established by analyzing the three-axis magnetometer error mechanism. The said model conforms to an ellipsoid restriction, the parameters of the ellipsoid equation are estimated, and the ellipsoid coefficient matrix is derived. However, the calibration matrix cannot be determined completely, as there are fewer ellipsoid parameters than calibration model parameters. Mathematically, the calibration matrix derived from the ellipsoid coefficient matrix by a different matrix decomposition method is not unique, and there exists an unknown rotation matrix R between them. This paper puts forward a constant intersection angle method (angles between the geomagnetic field and gravitational field are fixed) to estimate R. The Tikhonov method is adopted to solve the problem that rounding errors or other errors may seriously affect the calculation results of R when the condition number of the matrix is very large. The geomagnetic field vector and heading error are further corrected by R. The constant intersection angle method is convenient and practical, as it is free from any additional calibration procedure or coordinate transformation. In addition, the simulation experiment indicates that the heading error declines from ±1° calibrated by classical ellipsoid fitting to ±0.2° calibrated by a constant intersection angle method, and the signal-to-noise ratio is 50 dB. The actual experiment exhibits that the heading error is further corrected from ±0.8° calibrated by the classical ellipsoid fitting to ±0.3° calibrated by a constant intersection angle method.
Accurate measurement of the geomagnetic field has been widely applied in geophysical research, space magnetic measurement, military defense, mineral resources exploration, and drilling practice . Common magnetometers include a helium optical-pumping magnetometer, a proton magnetometer, a three-axis flux gate magnetometer, and an anisotropic magnetoresistive magnetometer. The former two magnetometers could only be used to measure geomagnetic field magnitude, whereas the latter two magnetometers, belonging to the vector magnetometer type, are the most common magnetic sensors in an attitude and heading reference system (AHRS), which is characterized by low cost and high reliability. However, the magnetometer is full of inevitable errors such as zero deviation, sensitivity errors, non-orthogonal errors, misalignment errors, measurement noise, hard iron errors, and soft iron errors, and consequently there are large errors between the measurement results and actual geomagnetic field vector. As a result, calibration and error compensation should be conducted before the application. The calibration of magnetometers can be divided into the geomagnetic domain calibration and the heading domain calibration. The heading domain calibration only calibrates the heading error of the magnetic compass composed of the magnetometer, but each axis output of the magnetometer has not been calibrated. The geomagnetic domain calibration directly calibrates the output of each axis of the magnetometer. The magnetometer output after calibration can not only calculate the accurate heading angle but also can be used in geomagnetic navigation for providing rich component information.
The “two-step” algorithm directly calibrates the magnetometer error without an external heading reference. The principle of the two-step algorithm is that when the magnitude of the true geomagnetic field is invariable at the calibration spot, the ideal locus of the three-axis magnetometer output lies on a spherical surface, whereas the actual locus of the magnetometer measurement outcome lies on an ellipsoid under the disturbance of error. The first step of the two-step algorithm transforms the non-linear observation equation based on the square of the magnetic field magnitude into a linear equation of the new unknown parameter by a mathematical transformation and acquires the unknown parameter by a batch least squares solution. In the second step, the biases and the scale factors can be derived from an inverse analytical solution , but the non-orthogonal and misalignment errors cannot be calibrated because of the error model, which includes only zero deviation and sensitivity error. The iterative batch least squares method is used in  to obtain the ellipsoid parameter unbiased estimation, from which the initial conditions can be acquired by the aforementioned two-step algorithm. The algorithm possesses consistent convergence, and the posterior covariance could be used as a metric for the compensation effect. The “extension of the two-step” algorithm improves the two-step calibration algorithm by compensating for the non-orthogonal error . However, as the assumed sensor x-axis coincides with the body x-axis (it is also possible that none of the three axes coincides in reality), the misalignment error cannot be calibrated.
It is proposed in literature  that there are only nine independent parameters in the fitting ellipsoid model. Failing to clarify the 12 parameters in the calibration model mathematically could also be interpreted to mean that there is more than one method to decompose the ellipsoid coefficient matrix into two orthogonal matrixes (error parameter matrix). According to matrix theory, an orthogonal rotation matrix (indicating the rotation transform in three-dimensional space) exists between matrixes, resulting from different decomposition methods. In other words, magnetometer data can be compensated for sensor errors and the presence of magnetic distortions by mapping an ellipsoid of data to a sphere; however, the rotation of the sphere is unknown [5,6]. The essence of this difference discloses the failure to clarify the three-axis misalignment error. It has been shown in  that the magnetometer measurement noise is zero-mean Gaussian white noise, but the noise of the square of the magnetometer output is not zero mean, and ordinary least square (OLS) estimation is an inconsistent biased estimation. Adaptive least square (ALS) is utilized to obtain a consistent unbiased estimator of ellipsoid parameters because of the continuous adjustment procedure to the OLS cost function. This adjustment requires a known noise variance. Consistent estimation to an unknown noise variance, however, can be realized . ALS improves the accuracy of the ellipsoid fitting, but the calibration parameters derived by eigen decomposition are not always true because of the different matrix decomposition methods mentioned above. In addition, the coefficient matrix of the ellipsoid fitting could also be used to derive the error parameter matrix from singular value decomposition . However, the error model of this method approximates a symmetric matrix, which contains only nine undetermined coefficients; thus, the application of this method has limitations. In  a geomagnetic field vector and some auxiliary vector dot products are choosen as the constants to exam the effect of the rotation matrix in rectifying and compensating the error. This method does not require additional calibration, and the compensation accuracy depends on the choice of auxiliary vector. When the auxiliary vector is nearly parallel with the geomagnetic vector, the worst compensation result is obtained, whereas the best result is obtained when the former vector is perpendicular to the latter vector. Because the auxiliary vector is a constant vector of the earth coordinate system, it should be converted into components of the body coordinate system in a mathematical operation. Maximum likelihood estimation is used in the error parameter fitting, and misalignment error requires additional independent calibration for identification .
The transition matrix defined in  between the sensor coordinate system and body system contains six unknown parameters. This matrix completely describes the non-orthogonal error and misalignment error and adopts the “three-step” algorithm in magnetometer pre-calibration before flight, without reference to any direction information. The misalignment rotation matrix can be derived from the condition that the vertical component of the geomagnetic field remains unchanged while rotating the magnetometer respectively around the x-axis, y-axis, and z-axis in the geoid. It is proposed in  that the rotation matrix of the misalignment error could be obtained when the sensor rotates around an axis, and the projection of the magnetic field output is invariable, which lies on the plane that is perpendicular to the said axis. This method is more valuable in engineering as it is unnecessary to keep leveling. This paper is based on the constant intersection angle between the geomagnetic field vector and gravitation field vector , without additional independent calibration and coordinate system conversion, and seeks to derive a rotation matrix more conveniently, furthering the compensation of magnetic field measurement error and heading error.
2. Error Modeling
Because of the influence of the manufacturing processes and environment, a three-axis magnetometer has manufacturing, installation and environmental errors. The manufacturing error contains a zero-deviation H0 and sensitivity error Ks; installation error includes non-orthogonal error knor and misalignment error ; environmental error includes the soft iron error Cs and hard iron error Hp. On account of all the errors listed above, the relationship between the true geomagnetic field He and the three-axis magnetometer output Hm is demonstrated in Equation (1), in which Hn indicates the Gaussian white noise is zero-mean and its standard deviation is σ:
The different types of errors are specifically shown in Subsections 2.1–2.6.
2.1. Sensitivity Error
Sensitivity represents the proportional relationship between the magnetometer input and output. Sensitivity error results from the inconsistency between the amplification of the measuring electronic circuit and its nominal value, which can be expressed as:
If sensitivity is the only error that affects the sensor, the Equation (2) refers to the measurement Hm = Ks · He.
2.2. Zero Deviation
There is often a small voltage bias in the sensor output signal, even when there is no magnetic intensity. In such conditions, the sensor produces non-zero output, which can be expressed as:
If zero deviation is the only error that affects the sensor, the Equation (3) refers to the measurement Hm = He + H0.
2.3. Non-Orthogonal Error
Non-orthogonal error is caused by the limitation of machining, which leads the x-, y- and z-axes to not being completely orthogonal to each other. This is shown in Figure 1, assuming that the z-axis of the sensor completely coincides with the z-axis of the orthogonal coordinate system Tm:
If non-orthogonal error is the only error that affects the sensor, Equation (4) refers to the measurement Hm = Knor · He.
2.4. Misalignment Error
During the installation, the sensor x-axis may not totally coincide with the body vertical axis, as illustrated in Figure 2. The resultant transition matrix (rotation matrix) exists between the virtual orthogonal coordinate system Tm and the body orthogonal coordinate system , which is equivalent to a slight angle generated from rotations of the sensor around the x-axis, y-axis and z-axis, respectively:
If misalignment is the only error that affects the sensor, the Equation (2) refers to the measurement .
2.5. Soft Iron Errors
Ferromagnetic materials produce an inductive magnetic field under the influence of a geomagnetic field and the induced electric current around the sensor. It also varies with the attitude of the magnetometer and the position in the magnetic field, which can be expressed as:
The aij terms represent the effective soft iron coefficients and are the constants of proportionality between the magnetic field applied to soft iron and the resulting induced magnetic field . For example, axy represents the effective coefficient relating the field generated in the x-direction in response to an applied field in the y-direction, where the effective soft iron coefficients appears insignificant when i ≠ j. Mathematically, the soft iron error for principal diagonal elements is equivalent to the sensitivity error; and non-diagonal elements correspond to the non-orthogonal error and misalignment error. If soft iron is the only error that affects the sensor, Equation (2) takes to the measurement Hm = Cs · He.
2.6. Hard Iron Errors
This type of error results from permanent magnets and magnetic hysteresis, that is, remanence of magnetized iron materials. Mathematically, this error is equivalent to zero-deviation:
If hard iron is the only error that affects the sensor, Equation (2) refers to the measurement Hm = He + Hp.
Ignoring the measurement noise in Equation (1), the geomagnetic field vector He can be derived as:in which .
3. Classical Ellipsoid Assumption Algorithm
When an ideal magnetometer rotates in the calibration spot, the geomagnetic field magnitude remains constant, and the output locus of the three-axis magnetometer is a sphere. In contrast, a non-ideal magnetometer output locus would be an ellipsoid because of the influence of error. The square of He is derived from Equation (8), and sorted into the quadratic form of the surface:Equation (9) is rewritten as a general form of the quadratic surface equation: where ξ = (a, b, c, d, e, f, p, q, r, s)T.
Generally, non-diagonal elements of the soft iron matrix Cs, the non-orthogonal error and misalignment error of the soft iron error, are minuscle, therefore, the error matrix M is strictly diagonally dominant . Therefore GTG is also strictly diagonally dominant, belonging to a positive-definite real symmetric matrix, and Equation (9) is a quadratic ellipsoid equation, then for convenience, Equation (9) can be written as:
where, is the coefficient matrix after ellipsoid fitting, and are the spherical center coordinates. The objective of magnetometer calibration is to conduct ellipsoid fitting based on the set of N measurement data, deriving the coefficient matrix A and spherical center coordinates X0.
The principle of ellipsoid fitting is finding an ideal ellipsoid where the sum of squares of the algebraic distances calculated from the measured data point to the ellipsoid is minimized , which is expressed as Equation (12) or (13):where: .
In order to assure that the fitting result is an ellipsoid, Nikos contends that parameter σ should guarantee that matrix A in Equation (10) is positive definite matrix or negative matrix . This constraint is analyzed in literature , which states that the equality constraint 4ab − b2 = 1 can be imposed for the convenience of calculation, which would not lose its generality and can be expressed in the matrix form:where and .
In order to obtain the extremum under constraints, the first-order derivative could be derived from Equation (15), and Equation (16) could be obtained when the first-order derivative of Equation (15) is set to zero:
Therefore, the extremum under an ellipsoid constraint could be obtained:
It has been proved in  that only one of the generalized eigenvalues in Equation (16) is positive, and its eigenvector is the best ellipsoid fitting parameter ξ. The ellipsoid coefficient matrix A and spherical center coordinate X0 is derived from further calculation. It could be concluded from the comparison between Equation (9) and Equation (10) that:
‖He‖ is not necessarily the actual magnitude of the geomagnetic field because its magnitude only affects the components on the x-axis and y-axis, whereas the heading hinges on the proportion of the geomagnetic field projection on the x-coordinate and y-coordinate . Introducing Hp = G(X0 − H0) to Equation (8), we obtain He = G(Hm − H0) − G(X0 − H0) = G(Hm − X0). Therefore, it is not necessary to use H0. The 3 × 3 matrix G combining scale factors, non-orthogonal errors, misalignments, and soft iron disturbances is not strict symmetrical, including nine independent parameters, and there are three combined biases in the error model. The total number of error parameters should be 12.
Therefore, the key to deriving calibration matrix G is to decompose the ellipsoid coefficient matrix into two orthogonal matrixes. However, the calibration matrix cannot be clarified, as the orthogonal matrix resulting from a different decomposition is not exactly the same. Because G is also a positive definite matrix, the decomposition results G1 and G2 only differ in an orthogonal rotation matrix R, which is equivalent to a fixed rotating angle in the body coordinate system between the geomagnetic field vector after compensation and the true geomagnetic field vector .
This paper provides a constant intersection angle method to solve the rotation matrix R. On the basis of this rotation matrix, the matrix G resulting from orthogonal decomposition could be transformed into the calibration matrix that is needed. The calibrated geomagnetic field could be obtained by solving Equation (8) and Equation (18) simultaneously:where Q = R · G.
4. Constant Intersection Angle Method
Similar to the classical ellipsoid fitting method, the constant intersection angle method also requires calibration in the same location in order to satisfy the condition that the magnitude and direction of the geomagnetic field and gravitation field are invariant. The intersection angle between the geomagnetic field vector and gravitation field vector at the same measurement spot is constant , and the dot product of magnetic field vector He and gravity acceleration vector Ag, which ‖He‖ · Ag · cosθ, is invariable and can be calculated from the model of geomagnetic field and gravitation field. In the said equation, θ is the intersection angle between the geomagnetic field vector and gravitation field vector, and its value can be interpreted to have approximately the same effect as ‖He‖ in Equation (18). Therefore, different values of θ would only affect the magnitude of the geomagnetic field after calibration rather than the heading solution. In addition, the acceleration coordinate system is also the body coordinate system as the accelerometer is fixed on the body and keeps moving with the body. Thus the intersection angle between the geomagnetic field vector He and gravitation field vector Ag at the same measurement spot is constant, even if there is no transformation into a geodetic coordinate system.
4.1. Rotation Matrix Solution
To begin, calibration matrix G is obtained by a singular value decomposition of the positive matrix ‖He‖2 A generated from Equation (18). Then, Hc can be derived as below, by introducing G and X0 into Equation (19) and preliminarily calibrating the geomagnetic field:where the gravity acceleration vector is , the magnetic field vector is He = R · Hc, and R as the undetermined rotation matrix can be represented as . Additionally, the dot product of the magnetic field vector and the gravity acceleration vector could is described as:
The matrix containing As for the set of N input vectors Ag and Hc, is expressed as Equation (23):Y = φ · x.
The least squares solution x = (ΦT · Φ)−1 · ΦT · Y is derived by batch a least squares solution. In the calculation process according to the method proposed in  we find the problem that the condition number of matrix φ is larger, which decrease the estimation accuracy of the rotation matrix. Therefore, the Tikhonov method is adopted to obtain a better estimator.
4.2. Noise Suppression
A high rotation matrix accuracy plays an important role in further correcting the heading error, which is calibrated by the classical ellipsoid fitting method. The measurement noise, however, are inevitable and have influence on the estimator of rotation matrix R. The noise suppression methodology can reduce the sensitivity of the solution to measurement noise.
When the condition number of matrix φ in Equation (23) is very large, the matrix is approximately singular, or when observation data is inaccurate, the solution will be submerged by errors. The Tikhonov regularization method could solve the problem by adding other information about the solution, so as to identify a meaningful, stable solution . The principle of adding information is that the 2-norm of the solution should be minimized. The regular solution defined by the regularization method is shown below :
Where L is generally a unit matrix, λ is a regularization parameter that controls the sensitivity of Φ, and Y is the disturbance caused by the solution. The selection of λ mainly relies on experience to guarantee matrix is of full column rank. A least squares solution is derived as the solution of Equation (24) is equivalent to the solution of Equation (25):
Equation (25) can be derived from the QR (decompose a matrix into a orthogonal and an upper triangular matrix) orthogonal least square algorithm, which is equivalent to solving the following linear equations:
USVT is then obtained by singular value decomposition of the coefficient matrix (φTφ + λ2LTL). The coefficient matrix is a square matrix; matrix U is an orthogonal matrix and matrix S is a diagonal matrix containing the eigenvalues, V = U. Then x = (USVT)−1 φT y = V−TS−1U−1φT y and rotation matrix R will obtain by recasting matrix x. Though the noise suppression can reduce the influence of measurement noise, other methods are needed to ensure that R is close to a rotation matrix. For example, a quite large number of samples can improve the estimation accuracy. Another method is set a constraint RTR = I on matrix R, and try to minimize ‖R − Rm‖ to obtain rotation matrix R. where Rm is recast by matrix R, R is the constrained optimization rotation matrix, its determinant is one. R is more close to the true rotation matrix R0 than Rm. Introducing it into Equation (19) or the equation He = R · Hc, heading error will be calibrated completely.
5. Simulation Study
During magnetometer calibration, to ensure the quality of the measurement data set, a proper uniform distribution of the data over all directions must be accomplished . Firstly, 46 data points are collected for the simulation, which are evenly distributed on the sphere. According to the principles of the equivalent intersection angle, regarding the sphere center as the coordinate origin, and the radius of the sphere as one, the x-axis, y-axis and z-axis coordinates are collected in the D46raw matrix, which is composed of 46 sample points. The collection method is shown in Figure 3, where the intersection angles ∠D1 O D2 and ∠D1 O D3 between any two adjacent data points are equal. Secondly, 46 data points are collected for the acceleration data, of which the magnitude is 9.8. As demonstrated in Figure 4, assuming that the acceleration vector and unit sphere intersects each other in Ai and Aj, ∠Di O Ai is equivalent to ∠Dj O Aj.
Then assuming that error matrix , zero deviation , and hard iron error , the output of the three-axis magnetometer influenced by the errors is D46ellipse = D46raw · M′, which is distributed on the disturbing ellipsoid. Then, the Gaussian white noise of N(0, 0.0022) is added into D46ellipse, where 0.002 is the standard deviation of the noise.
After determining the ellipsoid coefficient matrix, the preliminary calibration matrix G is derived by singular value decomposition. Regarding the heading as a reference, which is calculated from the original data set D46raw that is free from the influence of the error matrix, the heading error calibrated by matrix G is shown in Figure 5a. The heading error is ±1° where the blue dashed line refers to the heading error curve after a preliminary calibration of matrix G, which is derived from the classical ellipsoid fitting. Because the ellipsoid model after fitting only contains nine independent parameters, it can’t determine the 12 error parameters in the error model completely. In other words, the classical ellipsoid fitting method can transform the ellipsoid into a sphere, where transformed sphere and the original sphere differ by an undetermined rotation matrix R. Consequently, this influences the accuracy of the heading calibration. The proposed constant intersection angle method can derive R.
The constant intersection angle method is not necessary for the additional calibration procedure mentioned in reference [11,12] and the coordinate transformation mentioned in reference . Rotation matrix R can be derived from three-axis magnetometer and accelerometer data. The calibration matrix G derived from ellipsoid fitting coefficients is further corrected by rotation R, allowing us to improve the estimation of the calibration matrix Q. the heading error calibrated by matrix Q is lower than ±0.2°, which smaller than the heading error of ±1° when calibrated by classical ellipsoid fitting, shown as the red solid line in Figure 5a.
When the standard deviation of the Gaussian white noise is 0.003, and the magnitude of the simulation data is one, the heading error shown is shown in Figure 5b. The heading error calibrated by the constant intersection angle method decreases to ±0.4° from the value of ±1° when calibrated by the classical ellipsoid fitting. When the standard deviation of the noise is 0.005, the heading error is also shown in Figure 5c. The heading error decreases from ±1.2° to ±0.6° when calibrated by the constant intersection angle method. The error increases with the noise.
6.1. Measurement Equipment and Measurement Spot
In order to compare the calibration results between the classical ellipsoid fitting method and the constant intersection angle method proposed earlier, the nonmagnetic turntable experiment adopts a self-developed magnetic compass, which is mounted on the nonmagnetic turntable. The magnetic compass adopts a PIC24HJ128GP504 microprocessor (Microchip Technology, Chandler AZ, USA), equipped with a fluxgate sensor as the magnetic sensing element, and a Honeywell QA-T160 accelerometer (Honeywell Conglomerate Company, Morristown, NJ, USA) is used. The output heading angle of the optical–electrical encoder is regarded as the true heading reference, where the error is less than 3′. As shown in Figure 6, the magnetic compass is fixed on the nonmagnetic turntable. Where the body coordinate frame (b) takes the forward direction in the magnetic compass as the direction of xb-axis, taking the downward direction as the zb-axis, and setting the yb-axis in conformity with the left-hand rule, the navigation coordinate frame (n) takes a direction in the north-east-downward frame. It can be inferred from the body coordinate frame and navigation coordinate frame that the clockwise heading angle is positive, and the heading angle is 0° when the xb-axis points northward.
The experiment was performed in a Beijing suburb, where the magnetic environment in the vicinity of the magnetometer is better than that in the laboratory in the city. The principle of the constant intersection angle is adopted to ensure that the data points are distributed evenly on the sphere. The data collection is composed of 46 sets of data spread on the x-axis, y-axis and z-axis, collected as follows. To begin, where the magnetic compass is fixed on the nonmagnetic turntable, and the roll angle is 0°, and pitch angle is 60° and −60°, respectively, the nonmagnetic turntable is rotated clockwise such that the magnetic compass xb-axis can intersect with the north direction at angles of 6°, 66°, 126°, 186°, 246° and 306°; Where the roll angle is 0°, and the pitch angle is respectively 60° and −60°, the nonmagnetic turntable is rotated clockwise such that the magnetometer xb-axis can intersect with the north direction at angles of 6°, 42°, 78°, 114°, 150°, 186°, 222°, 258°, 294° and 330°. Where both the roll angle and the pitch angle are 0°, the nonmagnetic turntable is rotated clockwise such that the magnetometer xb-axis can intersect with the north direction at angles of 6°, 36°, 66°, 96°, 126°, 156°, 186°, 216°, 246°, 276°, 306°, and 336°. Where the roll angle is 0°, and the pitch angle is 90° and −90°, the xb-axis is vertically upward and downward, respectively. The accelerometer data should be collected simultaneously at the same 46 positions, because the method is attitude-dependent.
Then, magnetometer preliminary calibration can be conducted through the ellipsoid assumption method. The heading angle ψ could be is derived Equation (27). It should be noted that magnetic field data in the body coordinate frame should be transformed to the navigation coordinate frame . The transformation matrix is shown in Equation (28):where .
θ and γ respectively refer to the pitch angle and roll angle, which are determined by the three-axis accelerations gx, gy, and gz, when either angle is not zero and where :
6.2. Accelerometer Calibration
As a type of inertial sensor, accelerometers are reliable, independent, and immune to environmental impacts. The primary errors of accelerometers are bias, sensitivity error, and non-orthogonal error. Such errors are similar to the magnetometer errors, as observed in Equation (1–3). The following equation describes the accelerometer observation:where, g0 is the bias of accelerometer, ge is the actual acceleration of gravity, and is derived from Equation (1) and Equation (3). Generally, the non-orthogonal angle of a three-axis accelerometer provided by the manufacturer is less than 0.5°. For calculation purposes, the trigonometric functions of Equation (3) can be simplified. The actual acceleration of gravity is derived from Equation (31) as follows:
The output trajectory of the three-axis accelerometer accords with the ellipsoid hypothesis as well. There are nine unknown parameters consisting of three sensitivity errors, three non-orthogonal error and three bias. Thus, the error parameters of the accelerometer can all be derived from the coefficients of the ellipsoid equation. The experiment is performed on the turntable shown in Figure 6 by mounting the magnetic compass on the aligned turntable, aligning the body frame of the magnetic compass with the turntable by using the location pins, and then rotating the turntable to different angular positions. The results in Figure 7 show that the absolute error declines from 0.1582 m/s2 to 4.6323 × e−4 m/s2, and the mean square root error drops from 0.0545 m/s2 to 1.0358 × e−4 m/s2; thus, the maximum error of the accelerometer can be reduced by a factor of approximately 1,000.
6.3. Experimental Result
The calibration matrix G of Equation (18) is derived from the ellipsoid coefficient matrix by eigen-value decomposition and singular value decomposition in the classical ellipsoid fitting method. Then G is introduced into Equation (20) to calibrate the measurement of the geomagnetic field Hm and obtain Hc calibrated by the classical ellipsoid fitting method. However, calibration matrix G is not the actual calibration matrix, which should be multiplied by the rotation matrix R mentioned earlier. R is obtained using the constant intersection angle method to further improve the accuracy of magnetic sensor. This method can be used to other type of three-axis inertia sensor including misalignment error. Then, the complete calibration geomagnetic field He = R · Hc is obtained. The heading error is shown in Figure 8a. The red solid line refers to the heading error calibrated by the constant intersection angle method, which is less than ±0.3°, and the blue dashed line refers to the heading error calibrated by the classical ellipsoid fitting method, which is within the range of ±0.8°.
Figures 8b,c are the results of two other experiments conducted in the laboratory in the city, where the red solid line refers to the heading error calibrated by the constant intersection angle method, and the blue dashed line refers to the heading error calibrated by the classical ellipsoid fitting method. The maximum heading errors calibrated by the constant intersection angle method are ±0.35° in Figure 8b and ±0.4° in Figure 8c. The maximum heading errors calibrated by the classical ellipsoid fitting method are approximately ±0.9° in Figure 8b and ±1.1° in Figure 8c. This shows that the constant intersection angle method has similar calibration performance in the laboratory in the city. The heading errors after calibration are slightly larger because magnetic perturbations are larger in the city.
As mentioned in Section 4.2, the accuracy of rotation matrix R affects the heading error directly. The measurement noises, however, are inevitable and have influence on the estimator of rotation matrix R. The noise suppression methodology can reduce the sensitivity of the solution to measurement noise, and the constrained optimization (set a constraint RTR = I on matrix R) can further improve the estimation accuracy of R. In order to verify the effect of this methodology, we conduct a comparison experiment shown in Figure 9.
The green line refers to the heading error that the rotation matrix R is estimated directly by the measurement data; the red line is the heading error that the estimation of R is adopted the noise suppression methodology. It can be seen from Figure 9 that the heading error decrease from ±0.48° to ±0.32°.
This study thoroughly analyses the three-axis magnetometer measurement errors and establishes a complete error model including 12 independent parameters, which is more universal and conforms to the ellipsoid restriction. However, the calibration matrix derived from the ellipsoid coefficient matrix by a different matrix decomposition method is not unique, and there exists an unknown rotation matrix R between them . A constant intersection angle method (angles between geomagnetic vector and gravitational vector are fixed in the same location) is proposed to estimate R. The geomagnetic field vector and heading error are further corrected by R. The simulation experiment indicates that the heading error declines from ±1° when calibrated by the classical ellipsoid fitting method to ±0.2° when calibrated by the constant intersection angle method, and the signal-to-noise-ratio is 50 dB. The actual experiment demonstrates that the heading error is further corrected by the constant intersection angle method decreases from the value of ±0.8° when calibrated by the classical ellipsoid fitting method to a value of ±0.3°. The method proposed is convenient and practical, as it is free from any additional calibration procedure mentioned in references [11,12] and the coordinate transformation mentioned in reference . In addition, the noise suppression methodology can reduce the sensitivity of the solution to measurement noise and obtain higher accurate estimator of the rotation matrix than reference .
This paper is supported by “Projects from National Natural Science Foundation of China” (No.61273082) and “Fundamental Research Funds for the Central Universities” (No.FRF-TP-09-017B). Furthermore, the authors would also like to thank all who have helped with this study.
Conflict of Interest
The authors declare no conflict of interest.
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