专利摘要:
The invention relates to a method for estimating an angular deflection (α) between a reference axis (Aref) of a magnetic object (2) and a collinear magnetic axis at a magnetic moment (m) of said magnetic object ( 2), comprising the following steps: a) positioning (90; 110) said magnetic object (2) vis-à-vis at least one magnetometer (Mi); b) rotating (110) said magnetic object (2) about said reference axis (Aref); c) measuring (110), during rotation, the magnetic field (Bi (tj)), by said magnetometer (Mi); d) estimating (130; 230) the angular deviation (α) from the measurements of the magnetic field (Bi (tj)).
公开号:FR3054041A1
申请号:FR1661693
申请日:2016-11-30
公开日:2018-01-19
发明作者:Saifeddine Aloui;Franck Vial;Jean-Marie Dupre La Tour;Guilhem SAUVAGNAC;Tristan Hautson
申请人:Commissariat a lEnergie Atomique CEA;ISKN SAS;Commissariat a lEnergie Atomique et aux Energies Alternatives CEA;
IPC主号:
专利说明:

Holder (s): COMMISSION FOR ATOMIC ENERGY AND ALTERNATIVE ENERGY Public establishment, ISKN Simplified joint-stock company.
Extension request (s)
Agent (s): INNOVATION COMPETENCE GROUP.
METHOD FOR ESTIMATING AN ANGULAR DEVIATION BETWEEN THE MAGNETIC AXIS AND A REFERENCE AXIS OF A MAGNETIC OBJECT.
FR 3 054 041 - A1
15 /) The invention relates to a method for estimating an angular deviation (a) between a reference axis (A ref ) of a magnetic object (2) and a collinear magnetic axis at a magnetic moment (m) of said magnetic object (2), comprising the following steps:
a) positioning (90; 110) of said magnetic object (2) with respect to at least one magnetometer (M,);
b) rotation (110) of said magnetic object (2) about said reference axis (A ref );
c) measurement (110), during rotation, of the magnetic field (Bj (tj)), by said magnetometer (M,);
d) estimation (130; 230) of the angular deviation (oc) from the measurements of the magnetic field (Bj (tj)).

METHOD FOR ESTIMATING AN ANGULAR DEVIATION BETWEEN THE MAGNETIC AXIS AND A REFERENCE AXIS OF A MAGNETIC OBJECT
TECHNICAL FIELD [001] The invention relates to a method and a device for estimating an angular deviation between the magnetic axis of the magnetic moment of a magnetic object and a reference axis of said magnetic object.
STATE OF THE PRIOR ART It is known to use magnetic objects, in particular within the framework of a system for recording the trace of a magnetic pencil on a writing medium. The magnetic object is understood here as an object with which a non-zero magnetic moment is associated, for example a permanent magnet fixed to a non-magnetic pencil.
For example, the document WO2014 / 053526 describes a system for recording the trace of a pencil to which a permanent annular magnet is fixed. The magnetic object, here the permanent magnet, comprises a magnetic material, for example ferromagnetic or ferrimagnetic, uniformly distributed around a mechanical axis, called the reference axis, which corresponds to its axis of revolution. The magnet is designed so that its magnetic moment is substantially collinear with the reference axis.
The system for recording the pencil trace provided with the permanent magnet comprises a network of magnetometers capable of measuring the magnetic field generated by the permanent magnet. The magnetometers are attached to a writing support.
However, the trace recording method assumes that the magnetic axis of the permanent magnet, defined as the axis passing through the magnetic moment, is effectively collinear with the reference axis, or has an acceptable angular deviation between the magnetic axis and the reference axis. Indeed, an angular deviation of a few tenths of degrees can lead to an error on the reading of the trace which can then present a detrimental lack of precision. It may then be necessary to make a preliminary estimate of the angular deviation between the magnetic axis and the reference axis of the magnetic object.
PRESENTATION OF THE INVENTION The aim of the invention is to propose a method for estimating an angular deviation between a reference axis of a magnetic object and a collinear magnetic axis at a magnetic moment of said magnetic object. For this, the estimation process includes the following steps:
a) positioning of said magnetic object with respect to at least one magnetometer capable of measuring a magnetic field in the presence of the magnetic object;
b) rotation of said magnetic object about said reference axis;
c) measurement, during rotation, of the magnetic field, for different instants of a measurement duration, by said magnetometer;
d) estimation of the angular deviation from measurements of the magnetic field.
[007] Preferably, the estimation step includes:
a sub-step of identifying a so-called minimum magnetic field and a so-called maximum magnetic field from measurements of the magnetic field; and a sub-step for calculating the angular deviation from the minimum and maximum magnetic fields identified, and from geometric parameters representative of the position of the magnetometer with respect to the magnetic object.
Preferably, during the identification sub-step, the minimum and maximum magnetic fields are identified respectively from the minimum and maximum values of the standard of the magnetic field measurements.
Preferably, said geometric parameters are the coordinates and the distance of the magnetometer from the magnetic object, in a plane passing through the reference axis and containing the magnetometer.
The angular deviation can be calculated from a coefficient equal to the ratio of the standard of the vector formed by the subtraction of the minimum and maximum magnetic fields on the standard of the vector formed by the sum of the minimum and maximum magnetic fields, and from said geometric parameters.
The angular deviation can be calculated from the following equation:
a = tan 1
where d is the distance between the magnetometer and the magnetic object, z and r are coordinates of the magnetometer with respect to the magnetic object along an axis, respectively parallel and orthogonal, to the reference axis, and where a is a predetermined coefficient.
During the rotation step, the magnetic object can make at least one revolution around the reference axis.
Said at least one magnetometer comprises at least three axes of detection of the magnetic field, said axes of detection being non-parallel to each other.
Preferably, said at least one magnetometer is a single triaxial magnetometer.
Preferably, said at least one magnetometer is positioned outside the reference axis or outside the perpendicular to the reference axis passing through the magnetic object.
Said at least one magnetometer can be positioned with respect to said magnetic object at a z coordinate along an axis parallel to the reference axis and an r coordinate along an axis orthogonal to the reference axis, so that the z coordinate is greater than or equal to the r coordinate.
The invention also relates to a method for characterizing a magnetic object having an angular deviation between a reference axis of said magnetic object and a collinear magnetic axis at a magnetic moment of said magnetic object, comprising the following steps:
implementation of the angular deviation estimation method according to any one of the preceding characteristics;
calculation of an amplitude of the magnetic moment associated with the magnetic object, from the estimated angular deviation, the maximum magnetic field identified, and said geometric parameters.
Preferably, the amplitude of the magnetic moment is calculated from the ratio between the norm of the maximum magnetic field and the norm of a magnetic field, for a unit amplitude of said magnetic moment, expressed analytically by the equation next :
max (α, ι-, ζ)
where â is the previously estimated angular deviation, d is the distance between the magnetometer and the magnetic object, z and r are coordinates of the magnetometer with respect to the magnetic object along an axis, respectively parallel and orthogonal, to the axis of reference, and where a and b are predetermined coefficients.
According to another embodiment, the estimation method comprises the following steps:
a) positioning of said magnetic object with respect to a measurement plane defined by a network of magnetometers able to measure a magnetic field in the presence of the magnetic object;
b) rotation of said magnetic object about said reference axis;
c) measurement, during rotation, of the magnetic field, for different instants of a measurement duration, by said magnetometers;
d) estimation of a so-called instantaneous magnetic moment of the magnetic object, at said different measurement times, from the measured magnetic field;
e) estimation of the mean angular deviation from said instantaneous magnetic moments.
The step of estimating the average angular deviation may include a substep of estimating an invariant vector in rotation around the reference axis from instantaneous magnetic moments, the estimation of the average angular deviation being carried out, in addition, from said invariant vector.
The estimation of the mean angular deviation may include the calculation of an amplitude of angular deviation between the instantaneous magnetic moments with respect to the invariant vector.
During the magnetic field measurement step, the magnetic object can perform an integer number of turns around the reference axis greater than or equal to 1.
The estimation method may include a step of homogenizing an angular distribution of the instantaneous magnetic moments around the reference axis during the measurement period, this homogenizing step comprising a calculation by interpolation d 'A so-called homogenized time series of instantaneous magnetic moments, starting from a so-called initial time series of instantaneous magnetic moments obtained previously, so that the successive instantaneous magnetic moments of the homogenized time series have a substantially constant angular difference.
The homogenization step may include an iterative phase for calculating interpolated magnetic moments in which a magnetic moment interpolated at a given iteration is obtained from a magnetic moment interpolated at a previous iteration, with a threshold value predetermined and of a unit vector defined from two successive instantaneous magnetic moments of the initial time series.
The positioning step may include:
a substep for estimating a first dispersion parameter representative of a dispersion of the intensity of the instantaneous magnetic moments of the magnetic object, for different so-called vertical positions of the magnetic object along an axis substantially orthogonal to the plane of measurement;
a substep for positioning the magnetic object in a vertical position for which the value of the first dispersion parameter is less than or equal to a predetermined threshold value.
The estimation method may include, prior to the positioning step, a step of measuring, by said magnetometers, an ambient magnetic field in the absence of the magnetic object, and may include a sub- step of subtracting the ambient magnetic field from the magnetic fields previously measured, so as to obtain the magnetic field generated by the magnetic object.
The estimation method may include a step of applying a low-pass filter to the component values of the instantaneous magnetic moments previously estimated.
The low pass filter can be a sliding average over a given number of samples.
The number of samples can be predetermined so that a bias defined as a difference between a so-called real angular deviation and the estimated average angular deviation is minimal, in absolute value, for a so-called average angular deviation threshold value.
The estimation method may include a step of sorting the magnetic object according to the deviation of the estimated value of the average angular deviation with respect to a value called the average angular deviation threshold.
The estimation method may include a step of estimating a parameter called quality indicator, from the calculation of a second dispersion parameter representative of a dispersion of the values of a parameter called instantaneous radius calculated as being the norm of an instantaneous vector defined between each instantaneous magnetic moment and the invariant vector estimated beforehand.
The estimation method may also include a step of comparing the second dispersion parameter with a predetermined threshold value.
The predetermination of the threshold value can include the following substeps:
obtaining, Q times with Q a non-zero natural integer, of a time distribution of said instantaneous radius, for the same magnetic object;
estimation, for each time distribution, of an average value called mean radius defined as the time average of the instantaneous radius, so as to obtain a distribution of Q estimated mean rays;
estimation, from the distribution of the estimated Q average radii, of an average value and a third dispersion parameter, called the threshold value, representative of a dispersion of the values of the estimated average radii.
The invention also relates to a device for estimating an average angular deviation between a magnetic axis and a reference axis of a magnetic object, comprising:
a network of magnetometers able to measure, at each instant of measurement of a duration, a magnetic field disturbed by the magnetic object along at least one measurement axis, the magnetometers being spatially distributed so as to define a measurement plane;
a holding and rotating member, capable of holding the magnetic object in a position with respect to the measurement plane, and of rotating the magnetic object along its reference axis;
a processor configured to implement the estimation method according to any one of the preceding characteristics.
The invention also relates to an information recording medium, comprising instructions for implementing the estimation method according to any one of the preceding characteristics, these instructions being able to be executed by a processor. .
BRIEF DESCRIPTION OF THE DRAWINGS Other aspects, aims, advantages and characteristics of the invention will appear better on reading the following detailed description of preferred embodiments thereof, given by way of nonlimiting example, and made with reference to the accompanying drawings in which:
Figure 1 is a schematic perspective view of a device for estimating an average angular deviation of a magnetic object according to a first embodiment;
FIG. 2 is a flow diagram of an example of a method for estimating an average angular deviation of the magnetic object according to the first embodiment;
FIGS. 3A and 3B illustrate the instants of rotation when the magnetic moment of the object is contained in a plane defined by the reference axis and the position of the magnetometer, and more precisely when the magnetic moment is contained in the half-plane does not not containing the magnetometer (fig.3A) and when it is contained in this half-plane (fig.3B);
FIG. 4A is a schematic perspective view of a device for estimating an average angular deviation of a magnetic object according to a second embodiment, and FIG. 4B schematically illustrates the temporal evolution of the magnetic moment of l magnetic object during a measurement duration T, thus forming a circle which extends around the reference axis;
FIG. 5 is a flow diagram of an example of a method for estimating an average angular deviation of the magnetic object, according to the second embodiment;
FIG. 6A illustrates an example of the time evolution of the elementary angular difference between two successive instantaneous magnetic moments during the measurement duration T; FIGS. 6B and 6C schematically illustrate an example of non-homogeneous angular distribution of the instantaneous magnetic moments around the reference axis; and FIGS. 6D and 6E schematically illustrate an example of homogeneous angular distribution, around the reference axis, of the instantaneous magnetic moments obtained after an angular homogenization step;
FIG. 7 is a flow diagram of a partial example of a method for estimating an average angular deviation comprising a step of angular homogenization;
FIG. 8A illustrates a schematic example of the temporal evolution of the components of the instantaneous magnetic moment and FIG. 8B illustrates an example of evolution of the value of a bias on the estimation of the estimated mean angular deviation, as a function of the value the actual angular deviation, for different values K of the number of samples taken into account during a filtering step;
FIG. 9 is a flow diagram of a partial example of a method for estimating an average angular deviation comprising a step of filtering instantaneous magnetic moments;
FIG. 10A illustrates an example of evolution of the standard deviation of the standard of instantaneous magnetic moments as a function of the vertical position of the magnetic object with respect to the measurement plane; and FIG. 10B is a flow diagram of a partial example of a method for estimating an average angular deviation comprising a step of prior positioning of the magnetic object.
DETAILED DESCRIPTION OF PARTICULAR EMBODIMENTS In the figures and in the following description, the same references represent the same or similar elements. In addition, the different elements are not shown to scale so as to favor the clarity of the figures. Furthermore, the different embodiments and variants are not mutually exclusive and can be combined with one another. Unless otherwise indicated, the terms "substantially", "approximately", "in the order of" mean to the nearest 10%, and preferably to the nearest 5% or even to the nearest 1%.
The invention relates to a device and a method for estimating the average angular deviation between the magnetic axis associated with the magnetic moment of a magnetic object and a mechanical reference axis of this object.
The magnetic object comprises a material having a magnetic moment, for example spontaneous. It is preferably the material of a permanent magnet. The magnetic object can be a cylindrical permanent magnet, for example annular, as illustrated in the document WO2014 / 053526 cited above, in which case the reference axis corresponds to an axis of symmetry of the magnet, for example the axis of revolution of the magnet. It can also be a utensil or a pencil equipped with such a magnet or comprising a different permanent magnet, for example integrated into the body of the pencil, in which case the reference axis can correspond to the longitudinal axis. along which extends the pencil passing through the point or the pencil writing lead. The term pencil is to be understood in a broad sense and can include pens, felt-tip pens, brushes or any other writing or drawing organ.
The magnetic material is preferably ferrimagnetic or ferromagnetic. It has a non-zero spontaneous magnetic moment even in the absence of an external magnetic field. It can have a coercive magnetic field greater than 100 Am _1 or 500 Am _1 and its intensity is preferably greater than 0.01 Am 2 or even 0.1 Am 2 . It is considered below that the permanent magnet can be approximated by a magnetic dipole. The magnetic axis of the object is defined as being the collinear axis at the magnetic moment of the object. The reference axis here corresponds to an axis of symmetry of the magnetic object. The angular deviation between the reference axis and the magnetic axis is noted angular deviation.
Figure 1 is a perspective view, schematic and partial, of an estimation device 1 of an angular deviation of a magnetic object 2 according to a first embodiment. The magnetic object 2 is here a cylindrical permanent magnet, for example annular.
The estimation device 1 is able to measure the magnetic field at different instants of measurement, during a measurement duration T, in a reference frame (e r , ee, e z ), and to estimate the value of the angular deflection â of the magnetic object 2 based on the measured values of the magnetic field.
Here we define a direct three-dimensional orthogonal coordinate system (e r , ee, e z ), where the axis e z is collinear with the reference axis A re f, and where the axes are e r and and, are orthogonal to the axis e z .
The magnet 2 is intended to be positioned in the center of the coordinate system (e r , ee, e z ), so that the position Po of the magnet 2 has in this coordinate system the coordinates (0,0,0) . The position Po of the magnet 2 corresponds to the coordinates of the geometric center of the magnet 2, that is to say to the unweighted barycenter of the set of points of the magnet 2. Thus, the magnetic moment m of the magnet 2 presents the components (m r , me, m z ) in the coordinate system (e r , ee, e z ). Its norm, also called intensity or amplitude, is noted llm II or m. The magnet is intended to be oriented so that the axis e z , corresponding to the axis of rotation of the magnet 2, coincides with the reference axis A re f of the latter. Thus, when the magnet 2 is rotated about its reference axis A re f, the magnetic moment m will rotate around the direction e z .
The estimation device 1 comprises a sensor for measuring the magnetic field having at least three separate measurement axes di, d 2 , d 3 in pairs, that is to say that the measurement axes are not not parallel to each other, and can thus comprise at least one triaxial magnetometer.
The triaxial magnetometer M is placed at a defined position Pm (γ, Θ, ζ) with respect to the position Po of the magnet and therefore of the center of the reference frame (e r , ee, e z ). This position is known and constant throughout the duration of measurement T. Knowledge of the position may have a certain tolerance, for example of the order of 10% if a relative uncertainty of the order of 20% on the estimated value of the angular deviation is accepted, or less, for example of the order of 1% for a relative uncertainty of the order of 2% on the value of the angular deviation.
The magnetometer M therefore measures the amplitude and the direction of the magnetic field B disturbed by the magnet 2. More precisely, it measures the standard of the orthogonal projection of the magnetic field B along the measurement axes di, d 2 , d 3 . By disturbed magnetic field B is meant the ambient magnetic field B a , that is to say undisturbed by magnet 2, to which is added the magnetic field B d generated by magnet 2.
The estimation device 1 further comprises a calculation unit 4 capable of storing the measured values of the magnetic field during the measurement period, and of determining the angular deviation â of the permanent magnet 2 from the magnetic field measurements
B.
For this, the magnetometer M is connected to the computing unit 4, electrically or otherwise, by an information transmission bus (not shown). The calculation unit 4 includes a programmable processor 5 capable of executing instructions recorded on an information recording medium. It further comprises a memory 6 containing the instructions necessary for the implementation of certain steps of a method for estimating the angular deviation by the processor 5. The memory 6 is also suitable for storing the information measured at each instant of measured.
The calculation unit 4 implements a mathematical model associating the measurements of the magnetometer M with the magnetic field and the position of the magnetometer M with respect to the magnet 2 in the reference frame (e r , ee, e z ) . This mathematical model is constructed from the equations of electromagnetism, in particular magnetostatics, and is parameterized in particular by geometric parameters representative of the position of the magnetometer M with respect to the magnet 2 in the reference frame (e r , ee, e z ).
To be able to approximate the permanent magnet 2 to a magnetic dipole, the distance between the permanent magnet 2 and the magnetometer M is greater than 2 times, 3 times, or even 5 times the largest dimension of the permanent magnet. 2. This dimension can be less than 20cm, even less than 10cm, or even 5cm.
The estimation device 1 also comprises a member 7 for holding and rotating, capable of maintaining the permanent magnet 2 relative to the magnetometer M, in a known and constant position during the measurement period.
It is also able to ensure the rotation of the magnet 2 along its Aref reference axis during the measurement period. Also, during the measurement period, the position of the permanent magnet 2 is fixed and only its orientation around the reference axis A re f varies over time. Thus, the reference axis A re f remains fixed in the coordinate system (e r , ee, e z ). The member 7 for holding and rotating comprises a motor 8 associated with an arm 9. The arm 9 can thus receive and hold the permanent magnet 2 and ensures the rotation of the latter. The arm 9 is made of a non-magnetic material and the motor 8 is sufficiently distant from the permanent magnet 2 and the magnetometer M so as not to induce disturbance of the measured magnetic field. As a variant, the device 1 may not include a motor 8 and may be adapted so that the rotation of the arm 9 is carried out manually.
FIG. 2 illustrates a flow diagram of an example of a method for estimating the angular deviation to which the magnetic object 2 presents, the method being implemented by the estimation device of FIG. 1.
The method comprises a step 100 of prior measurement of the ambient magnetic field B a , that is to say here the magnetic field not disturbed by the presence of the magnet 2. For this, the magnetometer M is positioned at its measurement position Pm, and performs the measurement of the magnetic field Bj a in the absence of the magnet 2, that is to say the acquisition of the projection of the magnetic field B a on each of the acquisition axes di, d2, d 3 .
The method then comprises a step 110 of measuring the disturbed magnetic field B by the magnet 2 in rotation about its reference axis A re f during a measurement duration T.
For this, during a sub-step 111, the permanent magnet 2 is positioned by the member 7 for holding and rotating in the position Po with respect to the magnetometer M, so that the the axis of rotation coincides with the reference axis A re f of the magnet 2. The magnetic moment m of the permanent magnet 2 is non-collinear with the reference axis A re f and forms, opposite from this axis, an angular deviation â to be determined.
During a substep 112, the permanent magnet 2 is rotated by the member 7 about the reference axis A re f. The reference axis A re f is static during the measurement duration T, in other words its position and its orientation in the reference frame (e r , eo, e z ) do not vary during the duration T. The speed of rotation of the permanent magnet 2, denoted Ô, is preferably constant over the duration T.
During the rotation, for the duration T = | ti; în], a single triaxial magnetometer M measures the magnetic field B disturbed by the presence of the permanent magnet 2, at a sampling frequency fc = N / T. We thus obtain N instants tj of measurement. The magnetometer M, at time tj, measures the projection of the vector magnetic field B along the acquisition axes di, d2, d 3 . We thus obtain a time series {B (tj)} N of N measurements of the disturbed magnetic field B.
The method then comprises a step 130 of estimating the magnetic angular deviation â of the permanent magnet 2, from measurements B (tj) of the disturbed magnetic field B.
Beforehand, during a sub-step 121, the calculation unit 4 deduces the magnetic field generated B d (tj) by the permanent magnet 2, at each instant tj, from the measurements of the magnetic field ambient B a and disturbed magnetic field B (tj). For this, we calculate B d (tj) = B (tj) - B a . We therefore obtain a time series {B d (tj)} n of N measurements of the generated magnetic field B d .
During a sub-step 131, the calculation unit 4 identifies a so-called minimum magnetic field Β ^, ίη and a so-called maximum magnetic field Bf ( iax from the measurements B d (tj) of the magnetic field B d . For this, we compute the norm | B d (tj) | of each measurement B d (tj) of the magnetic field generated B d , then we identify the minimal field B ^, in as being the one whose norm is the smallest, ie B ^, in such that | Β ^ ίη | = min ({11B d (tj) 11}), and we identify the maximum field B d , ax as being that whose norm is the most large, ie B d , ax such that | B d iax | = m ax ({| B d (tj) |}). We thus obtain the minimal magnetic fields B ^, in and maximal B d , ax .
These sub-steps 121 of subtraction of the ambient magnetic field B a and 131 of identification of the minimum magnetic fields Β ^ ίη and maximum B d , ax can be carried out continuously, during the sub-step 112 of acquisition of magnetic field measurements B.
In sub-steps 132 and 133, the calculation unit then calculates the angular deviation â from the minimum fields Β ^ ίη and maximum B d , ax identified, and from geometric parameters representative of the position Pm of the magnetometer vis-à-vis the magnet 2.
As illustrated in Figures 3A and 3B, it appears that the minimum fields Β ^ ίη and maximum B d , ax are associated with the magnetic moment m when the latter belongs to a plane Ρ = (Ά ιι [, Ρ ι) of the coordinate system (e r , ee, e z ) containing the reference axis A re f and passing through the position Pm of the magnetometer.
More specifically, the minimum field Β ^ ίη is associated with the magnetic moment m when the latter belongs to the half-plane P 'of the plane P delimited by the reference axis A re f and not containing the magnetometer Pm (fig .3A). And the maximum field B d , ax is associated with the magnetic moment m belonging to the half-plane P ”of the plane P delimited by the reference axis A re f and containing the magnetometer Pm (fig.3B).
The minimal fields Β ^ ίη and maximal B d , ax can be expressed analytically, within the framework of the dipolar hypothesis. Indeed, the magnetic field B d generated by the magnet 2, when it belongs to the plane P of the reference frame (er, ee, e z ), can be expressed by the following equation (1):
B d (r, z) = 10 _1 ^ - (3 (u. P) p - u) (1) where the magnetic moment m = mu is written as the product of an amplitude m and a unit vector director u, and where the position vector P M -Po = dp of the magnetometer M in the plane (e r , e z ) is written as the product of a distance d and of a unit vector director p, the field magnetic being expressed here in microTesla.
From equation (1), the minimum field B ^, in associated with the moment m contained in the half-plane P ′ can be expressed analytically by the following equation (2):
sin (a) - sin (a) r 2 + cos (ct) rz —cos (ct) - + cos (ct) z - sin (a) rz (2) where (r, z) are the Pm coordinates of the magnetometer M in the plane P relative to the magnet
2, r being the coordinate along an axis orthogonal to the reference axis A re f and z being the distance between the magnetometer and the magnetic object.
Similarly, from equation (1), the maximum field BfJ, ax associated with the moment m contained in the half-plane P ”can be expressed analytically by the following equation (3):
—Sin (a) - + sin (a) r 2 + cos (ct) rz _ d 2 _ τ _ —cos (ct) - + cos (ct) z + sin (a) rz (3) [0070] of a sub-step 132, from equations (2) and (3), it is possible to calculate a coefficient CV no longer depending on the amplitude m of the magnetic moment, but only on the angular deviation â and the parameters representative of the positioning of the magnetometer M with respect to the magnet 2 in the plane P.
This coefficient CV is advantageously a so-called coefficient of variation, expressed here as the ratio of the norm of the vector formed by the subtraction of the minimum fields B ^, in (â, r, z) and maximum field B aiax (a, r, z) on the norm of the vector formed by the sum of the minimal fields B ^, in (â, r, z) and maximal BfJ, ax (a, r, z), as expressed analytically by the equation (4) following:
(4) It thus appears that the coefficient of variation CV no longer depends on the amplitude m of the magnetic moment, and that it is formed of the product of a first term depending only on the angular deviation â and d a second term depending only on known geometric parameters such as the coordinates (r, z) of the magnetometer M in the plane P and the distance d separating the magnetometer M from the magnet 2.
Furthermore, the coefficient of variation CV can also be calculated from the minimum magnetic fields BjJ, j n and maximum BfJ, ax previously identified, as expressed by the following relation:
(5) Also, during a sub-step 133, the angular deviation a can be estimated by the following equation (6) obtained from equations (4) and (5):
a = tan 1 yl r2 z 2 + (z 2 - d2 / 3 ) Z
J r2z2 + ( r2 - d2 / 3 ) 2 (6) Thus, the estimation method according to this first embodiment makes it possible to simply estimate the angular deviation â of the magnetic object 2 on the basis of a simplified analytical model of the magnetic field B d generated by magnet 2 associated with the measurements B d (tj) of the magnetic field generated B d by magnet 2 and with geometric parameters representative of the position of the magnetometer in a frame of which axis is collinear with the axis of rotation, itself being confused with the reference axis A re f of the object 2. It is thus not necessary to determine the amplitude and the orientation of the magnetic moment, and this method is also independent of the orientation of the magnetic sensor. Furthermore, it is not limited to low values of the angular deviation. Furthermore, it only requires the use of at least one triaxial magnetometer, and advantageously of a single triaxial magnetometer.
Preferably, the magnetometer M is positioned relative to the magnet 2 so that the z coordinate of the magnetometer in the plane P is greater than or substantially equal to the coordinate r. The coordinates r and z are advantageously substantially equal, thus making it possible to improve the accuracy of the estimate of the angular deviation â.
Furthermore, the magnetometer M is preferably located outside the reference axis Aref corresponding to the axis of rotation of the magnet 2, and outside the axis orthogonal to the reference axis A re f and passing through the position Po of the magnet 2. This arrangement makes it possible to clearly distinguish the minimum magnetic fields B ^, in and maximum B aiax from one another. In addition, in order to obtain a good signal-to-noise ratio, the magnetometer is arranged with respect to the magnet 2 outside the deflection cone formed by the magnetic moment m in rotation.
As a variant, several magnetometers M; can be used to estimate the angular deviation â. According to one approach, it is possible to carry out the estimation method for each of the magnetometers, so as to obtain a plurality of values â; angular deviation â, each being associated with a magnetometer M ;. The angular deviation â is then calculated by averaging, in a weighted manner or not, the values â; obtained. The average is advantageously weighted as a function of the intensity of the signal received by each magnetometer.
As a variant of the analytical approach developed above, it is possible to estimate the angular deviation from the fields B ^, in and B aiax identified during the step 305, step 131, with the use of several distinct magnetometers. each other in terms of positioning. Thus, in the case where the magnetic sensor comprises several triaxial magnetometers, the estimate of the angular deviation â can be obtained by optimization by minimizing for example the quadratic error between the fields Β ^, ίηί and previously identified by each magnetometer M; and minimal fields
B ailll l (d, fn, η, ζ ( ) and maximum rh, η, Zj) expressed by equations (2) and (3). We seek here to solve the minimization problem formalized by the following expression:
bJÎP Wj ((B n) axi (ot, m, rj, Ζ;) - B maxi ) + (B mini (a, m, rj, Z;) - B m j n j) where a is the estimated value of the angular deviation, rh is the estimated amplitude of the magnetic moment, and where r; and Z; are the coordinates of each magnetometer M ;. The term W; here is a weighting term, for example dependent on the inverse of the noise associated with each magnetometer M ;. Similarly, this minimization expression can be adapted to the case where the magnetic sensor comprises a plurality of scalar magnetometers which measure the norm of the magnetic field. In this case, the quadratic error between the magnetic field norm is minimized. These examples are given for illustrative purposes only and other approaches are possible.
Furthermore, preferably, the sampling frequency, the direction and / or the speed of rotation are chosen so as to improve the quality of the estimation of the angular deviation â, and more precisely of the identification of the minimum magnetic fields B ^, in and maximum magnetic fields BfJ, ax . Thus, when the sub-step 131 for identifying the fields B {J, j n and B aiax is carried out during the sub-step 112 for acquiring the measurements of the field B, the rotation of the magnet 2 may include a decrease in the speed of rotation and / or an increase in the sampling frequency as one approaches the minimum min ({11B d (tj) |}) and maximum max ({| B d (tj) |}) of the norm of the magnetic field generated B d . The rotation of the magnet 2 may also include phases of oscillations, that is to say of changing the direction of rotation, around these values. This reduces the relative uncertainty associated with the minimum and maximum values, which improves the quality of the identification of the minimum magnetic fields B {J, jn and maximum B d iax, and therefore of the estimation of the deviation angular â.
Furthermore, in the context of a method for characterizing the magnetic object, it may be advantageous to further determine the amplitude m of the magnetic moment m, here in the advantageous case where a single triaxial magnetometer is used .
The amplitude m can thus be determined from the estimated angular deviation â, the maximum magnetic field B d , ax identified, and said geometric parameters, namely the coordinates (r, z) of the magnetometer M and the distance d between the latter and the magnet 2.
More precisely, the amplitude m of the magnetic moment m can be calculated from the ratio between the standard | B aiax | of the maximum magnetic field B aiax identified, and the norm | Bm ax (â, r, z) | of the maximum magnetic field B aiax (a, r, z), for an amplitude max max max max unit of said magnetic moment m, expressed analytically by equation (7) from equation (3):
—Sin (a) —H sin (a) r 2 + cos (ct) rz _ a 2 _ τ _ —cos (ot) - + cos (ct) z + sin (a) rz (7) where a is the previously estimated angular deviation and (r, z) and d are the known geometric parameters.
The amplitude m is thus calculated from the following equation (8):
which then makes it possible to characterize the magnet 2 by the value of the amplitude m on the one hand, and of the value of the angular deviation on the other hand.
As a variant, the amplitude m can be calculated from the minimal magnetic field Bmin identified and from its analytical expression of equation (2). The use of the maximum magnetic field B aiax however makes it possible to obtain better precision.
Figure 4A is a perspective view, schematic and partial, of an estimation device 1 of an angular deviation called average âd'un magnetic object 2, according to a second embodiment, the magnetic object being here a permanent cylindrical magnet, for example annular. The instant magnetic moment estimated here is the vector magnetic moment estimated at a given instant, and instantaneous angular deviation the value of the angular deviation estimated at a given instant.
The estimation device 1 is able to estimate the instantaneous magnetic moment at different measurement instants during a measurement duration T, in a frame of reference XYZ. More specifically, the device 1 makes it possible to estimate the position of the permanent magnet 2, and its magnetic moment, at different times, in the XYZ coordinate system. In other words, the device 1 makes it possible to locate the position and the orientation of the permanent magnet 2 at different times in the XYZ coordinate system.
We define here and for the remainder of the description a three-dimensional direct coordinate system (Χ, Υ, Ζ), where the axes X and Y form a plane parallel to the measurement plane of the network of magnetometers, and where the axis Z is oriented substantially orthogonal to the measurement plane. In the following description, the terms "vertical" and "vertically" extend as being relative to an orientation substantially parallel to the axis Z, and the terms "horizontal" and "horizontally" as relate to an orientation substantially parallel to the plane (X, Y). In addition, the terms "lower" and "upper" extend as being relative to an increasing positioning when one moves away from the measurement plane in the + Z direction.
The position Pd of the permanent magnet 2 corresponds to the coordinates of the geometric center of the magnet 2. The geometric center is the unweighted barycenter of all the points of the permanent magnet 2. The magnetic moment m of magnet 2 presents the components (m x , m y , m z ) in the frame XYZ. Its norm, or intensity, is noted llm II.
The device 1 comprises a network of magnetometers M; distributed one against the other so as to form a measurement plane P me s · The number of magnetometers M; may be, for example greater than or equal to 2, preferably greater than or equal to 16, for example equal to 32, in particular when it is a triaxial magnetometer. However, the network of magnetometers includes at least 3 measurement axes which are distant from each other and not parallel in pairs.
The magnetometers M; are fixed to a protective plate 3 and can be located at the rear face of the plate 3, the latter being made of a non-magnetic material. By fixed means that they are assembled to the plate 3 without any degree of freedom. They are here aligned in rows and columns, but can be positioned mutually in a substantially random manner. The distances between each magnetometer and its neighbors are known and constant over time. For example, they can be between 1cm and 4cm.
The magnetometers M; each have at least one measurement axis, for example three axes, denoted x ;, y ;, Zj. Each magnetometer therefore measures the amplitude and the direction of the magnetic field B disturbed by the permanent magnet. More precisely, each magnetometer M; measures the norm of the orthogonal projection of the magnetic field B along the axes Xj, y ;, z; of the magnetometer. The sensitivity of magnetometers M; may be 4.10 7 T. By disturbed magnetic field B is meant the ambient magnetic field B a , that is to say not disturbed by the magnet, to which is added the magnetic field B d generated by the magnet .
The estimation device 1 further comprises a calculation unit 4 able to calculate the position and the orientation of the magnetic moment of the magnet 2 in the frame XYZ from the measurements of the magnetometers M ;. It also makes it possible to determine the mean angular deviation of the permanent magnet 2 from the measurements of the magnetic moment.
For this, each magnetometer M; is electrically connected to the computing unit 4 by an information transmission bus (not shown). The calculation unit 4 includes a programmable processor 5 capable of executing instructions recorded on an information recording medium. It further comprises a memory 6 containing the instructions necessary for the implementation of certain steps of a method of estimation of the average angular deviation by the processor 5. The memory 6 is also suitable for storing the information calculated at each instant of measurement.
The calculating unit 4 implements a mathematical model associating the position of the permanent magnet 2 in the frame XYZ, as well as the orientation and the intensity of the magnetic moment, with the measurements of the magnetometers M ;. This mathematical model is constructed from the equations of electromagnetism, in particular magnetostatics, and is parameterized in particular by the positions and orientations of the magnetometers in the XYZ coordinate system.
Preferably, to be able to approximate the permanent magnet 2 to a magnetic dipole, the distance between the permanent magnet 2 and each magnetometer M; is greater than 2 or even 3 times the largest dimension of the permanent magnet 2. This dimension may be less than 20cm, even less than 10cm, or even 5cm.
The estimation device 1 also comprises a member 7 for holding and rotating, capable of maintaining the permanent magnet 2 with respect to the measurement plane, in any position with respect to the plane of measured. The permanent magnet can be located above, that is to say facing, the network of magnetometers Mi, in a vertical position along the constant axis Z for the duration T of measurement. It is also able to ensure the rotation of the magnet 2 along its reference axis A re f during the measurement period. Also, during the measurement period, the vertical position of the permanent magnet 2 is fixed and only its angular position varies due to the rotation along the reference axis A re f. The member 7 for holding and rotating comprises a motor 8 associated with an arm 9. The arm 9 can thus receive and hold the permanent magnet 2 and ensures the rotation of the latter. The arm 9 is made of a non-magnetic material and the motor 8 is sufficiently distant from the measurement plane P mes and from the permanent magnet 2 so as not to induce disturbance of the magnetic field measured.
FIG. 5 is a flow diagram of an example of a method for estimating the mean angular deviation exhibited by a magnetic object, the method being implemented by the estimation device in FIG. 4A.
The method comprises a step 100 of prior measurement of the ambient magnetic field B a , that is to say here the magnetic field not disturbed by the presence of the magnet 2. For this, each of the magnetometers M; measures the magnetic field Bi a in the absence of the magnet 2, that is to say the projection of the magnetic field B a on each acquisition axis x ;, y ;, z; different magnetometers M ;.
The method then comprises a step 110 of measuring the magnetic field disturbed by the magnet 2 in rotation about its reference axis A re f during a measurement duration T.
During a substep 111, the permanent magnet 2 is positioned with respect to the measurement plane P mes by the member 7 for holding and rotating, which defines the orientation of the axis reference A re f of the permanent magnet 2 with respect to the measurement plane P mes in the frame XYZ. In this example, the permanent magnet 2 is positioned above the measurement plane P mes but any other positioning is possible. The orientation of the axis A re f can be arbitrary, but can advantageously be substantially orthogonal to the measurement plane P me s · The magnetic moment m of the permanent magnet 2 is not collinear with the reference axis A re f and forms, with respect to this axis, an angular deviation a to be determined.
In a sub-step 112, the permanent magnet 2 is rotated by the member 7 around the reference axis A re f. The reference axis A re f is static during the measurement duration T, in other words its position and its orientation in the frame XYZ do not vary during the duration T. The speed of rotation of the permanent magnet 2, noted Ô, is preferably constant over the duration T.
During the rotation, for the duration T = [ti; în], each magnetometer M; measures the magnetic field Bj (tj) disturbed by the presence of the permanent magnet 2, at a sampling frequency fc = N / T. We thus obtain N instants tj of measurement. Each magnetometer Mi, at time tj, measures the projection of the magnetic field B along the axis or axes of acquisition x ,, y ;, z ;. We thus obtain a time series (Bi (tj)} n of N measurements of the disturbed magnetic field.
The method then comprises a step 120 of estimating the instantaneous magnetic moment m (tj) of the permanent magnet 2, for each measurement time tj, from measurements of the disturbed magnetic field Bi (tj).
During a sub-step 121, the calculation unit 4 deduces the magnetic field generated Bi d (tj) by the permanent magnet 2, for each magnetometer M; and at each instant tj, from the measurements of the ambient magnetic field Bj a and the disturbed magnetic field Bj (tj). For this, we calculate Bj d (tj) = Bj (tj) - Bp.
During a sub-step 122, the calculation unit 4 estimates the position Pd of the permanent magnet 2 as well as its instantaneous magnetic moment m (tj), at each instant tj, from the magnetic field Bj d (tj) previously calculated. For this, the calculation unit 4 solves a mathematical model of electromagnetism equations associating the position and the magnetic moment of the permanent magnet 2 with the magnetic field that it generates Bi d (tj) = f (Pd; m (tj)). Thus, at each measurement instant, the calculation unit 4 determines the coordinates of the position of the permanent magnet 2 as well as the components m x , m y , m z of the instantaneous magnetic moment, in the reference frame XYZ. We thus obtain a time series {m (tj)} n of N instantaneous vectors of the magnetic moment m (tj).
As shown in Figures 4A and 4B, the time series {m (tj)} N forms a circle C which extends around the reference axis A re f. At the circle C can be associated instantaneous rays R (tj) relative to the instantaneous magnetic moments m (tj), as well as an average radius R whose value depends on the mean angular deviation à to be determined.
The method then comprises a step 230 of estimating the mean angular deviation â formed by the angular difference between the magnetic moment m of the magnetic dipole and the reference axis A re f.
During a sub-step 231, the calculation unit estimates an invariant vector mo during the rotation of the permanent magnet 2. For this, the time average is produced, over the N instants tj of measurement, of each coordinate m x (tj), m y (tj), m z (tj) of the instantaneous magnetic moment m (tj) in the frame XYZ. Thus, nio = (<m x (tj)>N;<m y (tj)>N;<m z (tj)> N ) = <m (tj)> N. The operator <> n corresponds here to the arithmetic time average, possibly weighted, over the N instants of measurement. A vector mo is thus obtained which is substantially collinear with the reference axis A re f which extends between the position Pd of the magnet 2 and the position P o of the center of the circle C.
During a sub-step 232, the calculation unit estimates a parameter representative of an average amplitude of the angular difference of the instantaneous magnetic moments with respect to the reference axis. Here, this parameter is the mean radius R of the circle C, such that R = <| m (tj) - m 0 | > N , that is to say the time average of the norm of instantaneous vectors m (tj) -m 0 .
In a sub-step 233, the unit determines the mean angular deviation â from the estimated mean radius R and, in this example, from the invariant vector mo- For this, it calculates the arc-tangent of the ratio of the mean radius R to the norm of the invariant vector mo:
â = tan _1 (R / | m 0 |). This gives an estimate of the angular deviation α between the reference axis of the magnetic object and its magnetic axis.
Of course, other equivalent calculations can be made. Thus, as a variant, during sub-step 233, the estimate of the mean angular deviation can be obtained from the arc-sine of the ratio between the mean radius R estimated beforehand and the time mean of the norm of the moment instantaneous magnetic <llm (tj) II> n on the N instants tj of measurement.
It is also possible, as a variant, to estimate, during sub-step 232, the instantaneous radius R (tj) of the circle at each instant tj of measurement and to calculate during sub-step 233, the corresponding instantaneous angular deviation ot (tj) then determining the average angular deviation â as the time average <a (tj)> N of the instantaneous angular deviations over the N instants tj of measurement.
It is also possible, as a variant, to estimate, during sub-step 232, the average radius R by adjusting at least one parameter of an equation of a circle in the frame XYZ traversing the time series instantaneous magnetic moments, for example the series {m (tj)} N- Thus, the equation of the circle can be (m x (tj) -Po, x ) 2 - (my (tj) -Po, y) 2 - (mz (tj) -Po, z ) 2 = R, where Po, x , Po. y , Po, z are the coordinates of the center Po of the circle C deduced from the position Pd of the magnetic moment estimated during the sub-step 122 and the invariant vector mo estimated during sub-step 231, and where m x (tj), m y (tj), m z (tj) are the values of the components of the instantaneous magnetic moment of the time series {m (td)} n considered. The adjustment of the value of the mean radius R can be carried out in a known manner, by conventional regression methods, for example multilinear or polynomial.
For example, the magnetic object is a permanent magnet with symmetry of revolution around its reference axis A re f. It is positioned for example 4 cm vertically from a network of 32 triax magnetometers with a sensitivity of 4.10 7 T spaced, for example, 4 cm. The rotation speed is π / 5 rad / s (1 revolution in 10s) and the sampling frequency is 140Hz. During a duration T of 10 s, the magnetic object performs a single rotation and the determination device acquires 1400 instants of measurement. The calculation unit estimates at 0.165 Am 2 the average intensity of the magnetic moment for RMS (Root Mean Square) noise of 5.10 -4 Am 2 . The determination device estimates the mean angular deviation between the reference axis of the magnet and its magnetic axis at 0.01 °.
Preferably, the duration T of measurement and the speed of rotation θ are chosen so that, during the duration T, the magnetic object has carried out an integer number of complete turns, for example a single turn. Furthermore, in order to obtain a substantially homogeneous angular distribution of the measurement data around the reference axis A re f during the duration T, the elementary rotation Δθ, between two instants of measurement tj and tj + i is substantially constant.
As detailed now, in the case where the measurement data do not have a substantially homogeneous angular distribution around the reference axis A re f for the duration T, an angular homogenization step can be implemented.
FIGS. 6A to 6E and FIG. 7 illustrate a step 140 of homogenizing the angular distribution of the instantaneous magnetic moments around the reference axis Aef during the measurement duration T. This step is based on the resampling of the instantaneous magnetic moments during the measurement duration T by interpolation, here by means of a linear interpolation method, so that the angular differences between two successive instantaneous magnetic moments are substantially constant. In other words, an initial time series of N instantaneous magnetic moments is resampled which have an inhomogeneous angular distribution around the reference axis A re f during the duration T, for example the time series {m ( tj)} N estimated for example during sub-step 122, to obtain a so-called homogenized time series {m h (tj)} N 'of N' instantaneous magnetic moments which have a substantially homogeneous angular distribution.
This step is advantageous when, as illustrated in FIGS. 6A to 6C, the angular distribution of the instantaneous magnetic moments around the reference axis Aef is not homogeneous during the duration T. This results in the fact that the angular deviations Δβ, defined between two instantaneous magnetic moments m (tj) and m (tj + i), at successive measurement instants tj and tj + i, exhibit a large dispersion around the mean value Δβ.
In this case, the vector mo, calculated during the sub-step 231 described above, may not be invariant in rotation, that is to say may not be collinear with the reference axis A re f. This error on the calculation of the vector mo can introduce a bias on the estimated value of the mean angular deviation â. This homogenization step 140 thus makes it possible to reduce the error on the estimation of the invariant vector mo. With reference to FIG. 7, this homogenization step 140 may include an optional sub-step 141 in which one estimates all first the angular deviations Δβ, defined by the estimated magnetic moments m (tj) and m (tj + i) at successive measurement instants of the initial time series, for example here {m (tj)} N. For this, we can calculate the angular difference Δβ, from the arc sine of the norm of the vector product of these two vectors: = sin ” 1 | m (tj) xm (t j + 1 ) | / (| m (tj) |. | m (t j + 1 ) |) where the symbol "x" represents the vector product and the symbol ". »The product of scalars.
Then, during a sub-step 142 which is also optional, the estimate of the dispersion of the angular deviations Δβ can be obtained by calculating the standard deviation σΔβ, or an equivalent parameter, over the angular deviations Δβ, estimated. If the value of the standard deviation σΔβ is less than a predetermined threshold, the measurement data have a substantially uniform angular distribution. Otherwise, the angular distribution of the instantaneous magnetic moments around the reference axis A re f is homogenized during the measurement duration T.
In a sub-step 143, the initial time series {m (tj)} N is resampled by interpolation to obtain a so-called homogenized time series {m h (tk)} N 'of N' magnetic moments interpolated, whose angular deviations Δβο are substantially constant. This is oversampling when N '> N but the number N' can be less than or equal to N.
For this, an approach illustrated in FIG. 6D consists in discretizing the angular difference Δβ, between two successive instantaneous magnetic moments m (tj) and m (tj + i) of the initial time series {m (tj)} N when its value is greater than a predetermined threshold value Δβο, for example by linear interpolation (as shown in FIG. 6D) or by another interpolation, for example polynomial.
Thus, we consider two magnetic moments m (tj + i) and m (tj) measured at successive times tj and tj + i, whose angular deviation Δβ, here has a value greater than the threshold Δβο- We determine a unit vector ej, j + i = (m (tj + i) -m (tj)) / llm (tj + i) -m (tj) ll. Then, one or even several interpolated magnetic moments are calculated such as: mj, k + i = ffij, k + Δβο-ejj + i, with ihj.kn = m (tj). The iteration on k continues as long as the angular difference between m (tj + i) and mj, k + i is greater than Δβο. By way of illustration, we consider the magnetic moments m (ti) and m (t 2 ) measured at successive instants ti and t 2 , for which the angular difference Δβι here has a value greater than the threshold Δβο- We determine the unit vector ei , 2 = (m (t 2 ) m (ti)) / llm (t 2 ) -m (ti) ll. Then, we calculate one or even several interpolated magnetic moments such as: ffiu + i = mi, k + Δβο-ei, 2 , with mi, k = o = m (tj = i) and as long as the angular difference between m ( t 2 ) and mi, k + i is greater than Δβο. This sub-step 143 can be applied to all the pairs of magnetic moments m (tj) and m (tj + i) measured at successive times, for which Afij> Afio- As an example, in FIG. 6D, three interpolated vectors m 2 i, m 22 , m 2 3 are calculated between the instantaneous magnetic moments m (t 2 ) and m (t3) so that the angular differences between these magnetic moments m (t2), ÎH21, 1H22, 1ÎÎ23 and m (t3) are substantially constant and equal to Δβο.
We thus obtain a homogenized time series {m h } N 'of N' instantaneous magnetic moments {m h } N 'corresponding to the N magnetic moments of the initial time series {m (tj)} N estimated during the sub step 122 to which are added the interpolated magnetic moments m.
As a variant (not shown), one can construct a homogenized time series {m h } N 'without having to incorporate, as previously, the initial time series {m (tj)} N- Thus, one can calculate N '' interpolated magnetic moments such as: ink + i = ffik + Δβο-ej.j + i, with ιϋι, -ί, = m (tj = i) and with the unit vector ej, j + i = (m (tj + i) -m (tj)) / llm (tj + i) m (tj) ll. The iteration on k continues as long as the angular difference between lük + i and m (tj + i) is greater than Δβο, and as long as the product of the number k of iterations and of Δβο is less than one or more times 2π. In addition, the unit vector ej.j + i is defined in j and j + 1 so that the angular differences between m (tj) and lük + i on the one hand, and between mk + i and m (tj + i ) on the other hand, are less than the angular difference Δβ] between m (tj) and m (tj + i). We thus obtain the homogenized time series {m h } N'of N'moments magnetic interpolated.
Prior to sub-step 143 of calculating the homogenized time series {m h } N ', it is possible to oversample the initial time series, for example {m (tj)} N , preferably by polynomial interpolation, possibly using splines, to thus obtain a new time series to be homogenized by means of sub-step 143 described above.
Thus, the standard deviation calculated on the angular deviations Δβ 'associated with the homogenized time series {m h } N' is then minimal or substantially zero insofar as they are substantially equal to the value Δβο. The instantaneous magnetic moments m h (tk) then have a substantially homogeneous angular distribution around the reference axis A re f during the measurement duration T.
The homogenized time series {m h } N 'corresponds to a resampling of the measurement data at a new frequency fe' = N7T, so that each instantaneous magnetic moment m h (tk) of the homogenized time series { m h } N 'can be seen as an estimate of the magnetic moment at different instants tk of measurement, with k = {1, 2, The method for estimating the mean angular deviation ang between the magnetic axis and the reference axis is then continued with step 230 described above. During sub-step 231, the invariant vector mo is deduced from the instantaneous magnetic N'moments m h (tk) of the homogenized time series {m h } N 'and no longer from the N instantaneous magnetic moments m ( tj) of the time series {m} n obtained during sub-step 122. In addition, during sub-step 232, the mean radius R of circle C is calculated from the magnetic moments m h (tk) of the homogenized time series and / or from the magnetic moments m (tj) of the filtered time series {m (tj)} N described below, and not from the magnetic moments m (tj) of the time series obtained during of sub-step 122.
As detailed now, it may be advantageous to perform a step 150 of low-pass filtering of the values of the components of the instantaneous magnetic moments in the frame XYZ, with the aim of reducing the temporal dispersion, in other words the measurement noise , which they can present, for example using an arithmetic or exponential moving average calculated on a number K of samples. This is particularly advantageous when the mean angular deviation is less than 0.2 ° and / or when the noise associated with the components of the magnetic moments is of the same order of magnitude as the value of the mean radius R of the circle C.
FIG. 8 A is a diagram which schematically illustrates the temporal dispersion of the values of the components m (tj) of the instantaneous magnetic moments m (tj) in the frame XYZ, here derived from the time series {m (tj) } N obtained during sub-step 122.
This dispersion of the values of the components m (tj) over time can induce a bias in the estimation of the mean angular deviation â. The bias is here noted b and is defined as the difference between the real angular deviation ot r of the permanent magnet 2 and the mean angular deviation â, that is b = a - a ,.
In order to reduce the time dispersion of the values of the components m (tj), step 150 of low-pass filtering by a sliding average, or moving average, can be performed (Figure 9).
During an optional sub-step 151, the unit calculates the standard deviation a (llm (tj) II) on the N values of the norm llm (tj) ll of instantaneous magnetic moments, or a parameter equivalent representative of the dispersion of the values of the standard llm (tj) ll of instantaneous magnetic moments. If the value of the standard deviation a (llm (tj) II) is greater than a predetermined threshold value, the 3N component values m (tj) are filtered.
In a sub-step 152, the unit applies a filter H K (tj) of low-pass type, here by sliding average over K samples, for example an arithmetic or exponential average, or a type of filter equivalent, over the time series of 3N values {m (tj)} N of the components of instantaneous magnetic moments in the frame XYZ. We therefore have a new time series such that (m (tj)} = Ηκ (ύ). {Ιη (tj)}, where m (tj) is the filtered values of the components of the instantaneous magnetic moment in the frame XYZ, at l 'instant tj. This gives a so-called filtered time series {m (tj)} N of instantaneous magnetic moments which is then taken into account for the execution of step 230 of estimation of the mean angular deviation â.
Of course, this step 150 of low-pass filtering of the components of the instantaneous magnetic moments can be applied to the time series {m (tj)} N obtained during sub-step 122, as to the homogenized time series { m h (tk)} N '· Preferably, the number K of samples is chosen so that the product of K with the mean angular deviation <Δβ,> of the time series considered, for example the series {m (tj)} N resulting from sub-step 122, is less than a given value, for example 45 °, and preferably 10 °, even 5 ° and preferably 1 °. Alternatively, the mean angular deviation <AQj> can be obtained by the speed of rotation of the rotation member multiplied by the sampling frequency. This avoids applying excessively restrictive filtering to the time series considered, which would risk masking the dynamics of the rotation signal.
It is advantageous to carry out step 140 of homogenization beforehand of step 231 of estimation of the invariant vector m ". Furthermore, it is advantageous to perform the filtering step 150 before the step 232 of estimating the average radius R of the circle C. It is finally advantageous to perform the filtering step 150 before the step 140 of homogenization so that the time series taken into account in step 140 of homogenization is less noisy.
As shown schematically in Figure 8B, the value of the bias b = d - a, may vary depending on the value of the real angular deviation ot r . It is illustrated in FIG. 8B by an affine function, but it can have another type of function. Thus, it appears that the value of the bias is positive for low values of angular deviation and negative for high values. It also appears that the value of the real angular deviation for which the value of the bias b is substantially zero depends in particular on the number K of samples taken into account in the sliding average, in particular in the case of an arithmetic sliding average.
When the method for estimating the mean angular deviation â comprises an additional substage of classification of the permanent magnet 2 with a view to sorting as a function of a reference value a t h of the deviation angular, it may be advantageous to determine the number K of samples to be taken into account in the moving average so that the value of the bias is substantially zero at the reference value a t h- By way of illustration only, for a reference value a t h equal to 0.5 ° and for a time series of 1400 instant magnetic moments whose average intensity is 0.165 Am 2 noised by an RMS signal of 5.10 -4 Am 2 , a sliding average over K = 10 samples can suit. The value of the bias for the reference value a t h is reduced or even canceled out. The classification sub-step comprises the comparison of the estimated value of the mean angular deviation â with the predetermined reference value a t h- Thus, one can operate a classification and therefore a sorting of the magnetic objects according to whether the mean angular deviation â is greater or less than the reference value a t h.
By way of illustration, for a reference value of 0.5 °, it can be considered that the permanent magnet 2 can be used when its estimated angular deviation is less than or equal to the reference value a t h and that it should be discarded when it is greater than the reference value. Indeed, for an estimated value less than the threshold value a t h, the bias is positive, that is to say that the real value ot r is less than the estimated value. The permanent magnet can then be used. On the other hand, for an estimated value â greater than the threshold value a t h, the bias is negative, that is to say that the real value ot r is greater than the estimated value. The permanent magnet is then to be removed. Of course, the reference value and the sorting decision depend on the applications planned for the permanent magnet.
Furthermore, the method for estimating the angular deviation may include a step 90 prior to vertical positioning of the permanent magnet 2 with respect to the measurement plane P me s, described with reference to FIGS. 10 A and 10B.
This positioning step includes a sub-step 91 for estimating a parameter representative of the dispersion of the values of the intensity of the instantaneous magnetic moment, for different vertical positions along the Z axis above the plane of measurement P mes For this, steps 110 and 120 are carried out for different values of vertical positioning of the object along the Z axis. For each vertical position, a time series of instantaneous magnetic moments is thus obtained, for example the time series {m (tj)} N obtained during sub-step 122, and we deduce for example the standard deviation σ (llm (tj) II) on the N values of the intensity llm (tj) ll instant magnetic moments. With reference to FIG. 10 A, a spatial series is thus obtained which gives the value of the standard deviation a (llm (tj) ll) for different vertical positions Z occupied by the magnetic object.
In a sub-step 92, a vertical position value Zp is selected for which the value of the standard deviation a (llm (tj) II) on the intensity of the instantaneous magnetic moment is less than one threshold value G re f. Then, the magnetic object is positioned so that it occupies the vertical position Zp.
The method for estimating the mean angular deviation â is then continued with step 100 and the steps 120 and 230 described above, possibly supplemented by steps 140 and 150.
In addition, the method may include an additional step of estimating a quality indicator of the measurements made during the measurement duration T. This step can preferably take place after the execution of step 120 or step 150.
For this, the calculation unit 4 determines the standard deviation gr on the N values of the instantaneous radius which is estimated from the instantaneous magnetic moments m (tj). The instantaneous radius can be calculated by the relation R (tj) = llm (tj) -m ο II- It is calculated here from the time series {m (tj)} n obtained during sub-step 122. L he quality indicator here is the quantity gr / t / n which characterizes the precision of the series of measurements. Other quality indicators can be used from the standard deviation gr, for example asin ((g r / a / N) / (<llm (tj) ll> N )) or atan ((g r / VN) / (| m 0 1 |)).
In order to detect a possible anomaly that occurred during the measurement series, the standard deviation gr on the N values of the instantaneous radius can be compared with a reference value g (R) previously determined. This value g (R) can be determined by performing a large number Q of estimates of the average radius R for the same type of permanent magnet 2. The number Q can be greater than 100 or even greater than or equal to 1000. The average radius R is for example estimated by executing steps 120 and 230, possibly supplemented by steps 140 and 150. Thus, we obtain Q times a time distribution {R (tj)} N of said instantaneous radius R (tj), for the same object magnetic. Q is a non-zero natural integer, preferably greater than or equal to 50 or even 100. Then we estimate, for each of the Q time distributions {R (tj)} N, a mean value called mean radius R defined as the time mean of the instantaneous radius <R (tj)> N. We thus obtain a distribution {R} q of Q estimated mean radii R. From this distribution, we estimate the mean value <R> q as well as a parameter for estimating the dispersion of the values of the estimated mean radii R around of the mean <R> q, such as the standard deviation g (R). We compare the quantity g r to g (R), for example by calculating the ratio gr / g (R). When this ratio is greater than or equal to a threshold value, for example 1, 2 or even
3, it can be estimated that the measurements made during the period T are not representative and therefore should not be taken into account. This measurement-related error may be due to a mechanical problem, for example a problem with the stability of the reference axis, or even a problem with magnetic detection, for example excessive magnetization of one or more magnetometers.
权利要求:
Claims (17)
[1" id="c-fr-0001]
1. Method for estimating an angular deviation (â) between a reference axis (A re f) of a magnetic object (2) and a collinear magnetic axis at a magnetic moment (m) of said magnetic object (2) , comprising the following steps:
a) positioning (90; 110) of said magnetic object (2) with respect to at least one magnetometer (Mi) capable of measuring a magnetic field (B) in the presence of the magnetic object (2);
b) rotation (110) of said magnetic object (2) about said reference axis (A re f);
c) measurement (110), during rotation, of the magnetic field (Bi (tj)), for different instants (tj) of a measurement duration (T), by said magnetometer (Mi);
d) estimation (130; 230) of the angular deviation (â) from the measurements (Bj (tj)) of the magnetic field (Bj).
[2" id="c-fr-0002]
2. Method according to claim 1, in which the estimation step (130) comprises:
- a sub-step of identifying a so-called minimum magnetic field (Β ^, ίη ) and a so-called maximum magnetic field (B ^ ax) from the measurements (B d (tj)) of the magnetic field (B d ); and
- a sub-step for calculating the angular deviation (â) from the identified minimum (BjJ, in ) and maximum (B ^ æj) magnetic fields, and geometric parameters (r, z; d) representative of the position of the magnetometer (M) relative to the magnetic object (2).
[3" id="c-fr-0003]
3. Method according to claim 2, in which, during the identification sub-step, the minimum (BjJ, j n ) and maximum (BfJ iax ) magnetic fields are respectively identified from the minimum and maximum values of the standard. (| B d (tj) |) of the measurements (B d (tj)) of the magnetic field (B d ).
[4" id="c-fr-0004]
4. Method according to claim 2 or 3, wherein said geometric parameters (r, z; d) are the coordinates (r, z) and the distance (d) of the magnetometer (M) relative to the magnetic object (2 ), in a plane passing through the reference axis (A re f) and containing the magnetometer (M).
[5" id="c-fr-0005]
5. Method according to any one of claims 2 to 4, in which the angular deviation (â) is calculated from a coefficient (CV) equal to the ratio of the norm of the vector formed by the subtraction of the minimum magnetic fields ( B ^, in ) and maximum (Bmax) on U norm of the vector formed by the sum of the minimum (B ^ in) and maximum (B aiax ) magnetic fields, and from said geometric parameters (r, z; d).
[6" id="c-fr-0006]
6. Method according to any one of claims 2 to 5, in which the angular deviation (â) is calculated from the following equation:
a = tan 1
where d is the distance between the magnetometer and the magnetic object, z and r are coordinates of the magnetometer with respect to the magnetic object along an axis, respectively parallel (e z ) and orthogonal (e r ), to the axis of reference (A re f), and where a is a predetermined coefficient.
[7" id="c-fr-0007]
7. Method according to any one of claims 1 to 6, wherein, during the rotation step, the magnetic object (2) performs at least one revolution around the reference axis (Aref).
[8" id="c-fr-0008]
8. Method according to any one of claims 1 to 7, wherein said at least one magnetometer (M) comprises at least three axes of detection of the magnetic field, said axes of detection being non-parallel to each other.
[9" id="c-fr-0009]
9. Method according to any one of claims 1 to 8, wherein said at least one magnetometer (M) is a single triaxial magnetometer.
[10" id="c-fr-0010]
10. Method according to any one of claims 1 to 9, wherein said at least one magnetometer (M) is positioned outside the reference axis (A re f) or outside the perpendicular to the reference axis ( A re f) passing through the magnetic object.
[11" id="c-fr-0011]
11. Method according to any one of claims 1 to 10, wherein said at least one magnetometer (M) is positioned relative to said magnetic object at a z coordinate along an axis (e z ) parallel to the reference axis ( A re f) and a coordinate r along an axis (e r ) orthogonal to the reference axis (A re f), so that the coordinate z is greater than or equal to the coordinate r.
[12" id="c-fr-0012]
12. Method for characterizing a magnetic object (2) having an angular deviation (â) between a reference axis (A re f) of said magnetic object (2) and a collinear magnetic axis at a magnetic moment (m) of said object magnetic (2), comprising the following steps:
- implementation of the angular deviation estimation method (a) according to any one of claims 2 to 11 depending on claim 2;
- calculation of an amplitude (m) of the magnetic moment (m) associated with the magnetic object (2), from the estimated angular deviation (â), the maximum magnetic field (Bmax) identified, and said geometric parameters ( r, z; d).
[13" id="c-fr-0013]
13. The method of claim 12, wherein the amplitude (m) of the magnetic moment is calculated from the ratio of the norm of the maximum magnetic field (Bmax) and a standard of a magnetic field (Bf (iax (a , r, z)), for a unit amplitude of said magnetic moment (m), expressed analytically by the following equation:
where â is the previously estimated angular deviation, d is the distance between the magnetometer (M) and the magnetic object (2), z and r are coordinates of the magnetometer (M) relative to the following magnetic object (2) an axis, respectively parallel (e z ) and orthogonal (e r ), to the reference axis (A re f), and where a and b are predetermined coefficients.
[14" id="c-fr-0014]
14. Estimation method according to claim 1, comprising the following steps:
positioning (90; 110) of said magnetic object (2) with respect to a measurement plane (Pmes) defined by a network of magnetometers (Mj) capable of measuring a magnetic field (B) in the presence of the magnetic object (2);
- estimation (120) of a magnetic moment, called instantaneous, (m (tj)) of the magnetic object (2), at said different measurement instants (tj), from the measured magnetic field (Bj (tj)) ;
- estimation (230) of the so-called average angular deviation (â) from said instantaneous magnetic moments (m (tj)).
[15" id="c-fr-0015]
15. The method of claim 14, wherein the step of estimating (230) the average angular deviation (â) comprises a substep of estimating (231) of a vector (mo) invariant in rotation around the reference axis (A re f) from instantaneous magnetic moments (m (tj)), the estimation (230) of the mean angular deviation (â) being carried out, in addition, from said invariant vector (mo ).
[16" id="c-fr-0016]
16. Device for estimating (1) an angular deviation (â) between a reference axis (A re f) of a magnetic object (2) and a collinear magnetic axis at a magnetic moment (m) of said magnetic object (2), comprising:
- at least one magnetometer (Mi) capable of measuring, at each instant of measurement of a duration (T), a magnetic field disturbed by the magnetic object (2);
- A member (7) for holding and rotating, capable of holding the magnetic object (2) in a determined position with respect to said at least one magnetometer (Mi), and of rotating the magnetic object (2) along its reference axis (A re f);
- a processor (5) configured to implement the method according to any one of claims 1 to 15.
[17" id="c-fr-0017]
17. Information recording medium, comprising instructions for the implementation of the method according to any one of claims 1 to 15, these instructions being
10 able to be executed by a processor.
1/9 i
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同族专利:
公开号 | 公开日
MX2019000455A|2019-12-19|
FR3054040B1|2018-08-17|
FR3054041B1|2018-08-17|
US20190301848A1|2019-10-03|
EP3485299A1|2019-05-22|
FR3054040A1|2018-01-19|
WO2018011492A1|2018-01-18|
CN109716168A|2019-05-03|
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优先权:
申请号 | 申请日 | 专利标题
FR1656785A|FR3054040B1|2016-07-13|2016-07-13|METHOD FOR ESTIMATING AN AVERAGE ANGULAR DEVIATION BETWEEN THE MAGNETIC AXIS AND A REFERENCE AXIS OF A MAGNETIC OBJECT|
FR1656785|2016-07-13|US16/317,434| US20190301848A1|2016-07-13|2017-07-10|Method for estimating an angular deviation between the magnetic axis and a reference axis of a magnetic object|
CN201780054445.XA| CN109716168A|2016-07-13|2017-07-10|Method for estimating the angular deviation between the reference axis of magnetic bodies and magnetic axis|
EP17745436.0A| EP3485299A1|2016-07-13|2017-07-10|Method for estimating an angular deviation between the magnetic axis and a reference axis of a magnetic object|
MX2019000455A| MX2019000455A|2016-07-13|2017-07-10|Method for estimating an angular deviation between the magnetic axis and a reference axis of a magnetic object.|
PCT/FR2017/051870| WO2018011492A1|2016-07-13|2017-07-10|Method for estimating an angular deviation between the magnetic axis and a reference axis of a magnetic object|
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