Abstract
In magnetic data processing, a fractional derivative can enhance details without excessively amplifying high-frequency noise. To obtain a fractional derivative numerically, a large number of survey points are required. This article demonstrates how a few survey points can be used to obtain the fractional derivative of a two-dimensional magnetic field through the application of Taylor–Riemann series. First, we derive the measurement method for the fractional gradient. This method is achieved by measuring the magnetic field at several survey points on a circle, then constructing analytical functions and finally calculating the fractional derivative. Next, an experiment is designed and simulated to demonstrate the impact of the fractional derivative start point and the ability to suppress Gaussian noise. Finally, the experiment is performed, which verifies the feasibility of the proposed method in a two-dimensional magnetic field.
1. Introduction
The concept of fractional calculus appears almost at the same time as integer-order calculus [1]. There are many definitions of fractional calculus, some of which are defined for specific applications. Some of them are the Riemann–Liouville (RL) fractional calculus [2], the Grunwald–Letnikov (GL) fractional calculus [3], the Caputo fractional calculus [4], the Atangana–Baleanu (AB) fractional calculus [5,6], the Riesz fractional calculus [7], the Weyl fractional calculus [8], etc. The most general definitions are the RL and GL definitions which are independent of specific applications. They are obtained by generalizing the order of integer-order derivative to an arbitrary real number [9]. In the field of complex analysis, the Cauchy integral formula can also be extended to the fractional order [10].
Fractional order calculus has been widely applied to the modeling and analysis of magnetic phenomena. Aykuta and Beyhana research the effect of fractional analysis on magnetic curves and investigate the trajectories of the magnetic fields [11]. Fractional calculus has been applied to the scalar Helmholtz equation [12]. It has also been used to extend Maxwell’s equations [13]. Although fractional calculus has been widely used, there is currently no universal and concise explanation for fractional calculus. Podlubny proposes a geometric and physical explanation for RL calculus [14]. He interprets the RL integration as the displacement of an object observed in a distorted coordinate system, which can be illustrated as the projection of a fence on two walls. Bai and Xue [15] interpret the 1/2-order RL integral as a curvilinear integral of a specific function along a semicircle. However, both explanations have limitations. Podlubny’s interpretation specifies the motion function of the observer. Bai and Xue’s interpretation specifies the integral order to be 1/2, the integral path to be a semicircle, and the integrand to be a specific function. These non-universal explanations limit their applications.
Since there is no general physical meaning for fractional calculus, in the field of magnetic exploration, fractional calculus is currently used primarily for data processing without considering their physical meanings. These studies primarily utilize the transitional properties of fractional derivatives by adjusting the derivative order to enhance details without excessively amplifying high-frequency noise. Since the 1930s, the derivative of the magnetic data has been used to enhance the details of magnetic anomaly and to suppress slowly changing background fields [16]. This operation behaves like a high-pass filter in the frequency domain [17]. It is susceptible to noise. As the order of the derivative increases, the noise is amplified, and the signal is submerged. The derivative operation is used only to enhance details and has no other physical meaning. From a mathematical perspective, there is no reason to limit the derivative order to integers.
Gunn [18] presents a novel algorithm for enhancing the visual representation of airborne geophysical data. The author uses the fractional derivative to address the issue of noise but does not mention the methodology for evaluating the value of the fractional derivative. Cooper and Cowan [19] use a numerical algorithm [20] to calculate the fractional gradients of magnetic data, thereby achieving a balance between noise and resolution. Furthermore, the fractional derivative is applied to the sunshading operation [21], which is a high-pass filter, to reduce the impact of noise. The shallow-layer separation filter is capable of separating the regional and residual magnetic fields, which is important for magnetic interpretation [22]. Cooper and Cowan extend the vertical derivative to the fractional order, providing a flexible approach to shallow-layer separation filtering. Arisoy [23] uses the fractional derivative to enhance and detect the edge of magnetic data, which is achieved by adjusting the order of the fractional derivative. Arisoy transforms the calculation of the fractional derivative into the frequency domain to reduce the requirements of memory size caused by the nonlocality property of the fractional derivate.
Due to the complexity of the definition of fractional calculus, a numerical method is applied to field data in the above applications to obtain fractional derivatives. The numerical method requires a large number of samples to meet accuracy requirements. In contrast to fractional calculus, the physical interpretation of an integer-order derivative is clear. Therefore, the magnetic gradient can be measured directly. This is accomplished by measuring the field at two points and, then, dividing the magnetic difference by the distance between the two points [24]. The first widely recognized instrument used in aeromagnetic measurement is the low-temperature superconducting magnetic gradiometer developed by the Jena Institute for Advanced Technology in Germany in 1997. The experiments were conducted in South Africa, and they obtained the full tensor gradient data graph [25]. In 2010, National Laboratory of Singapore developed a differential tensor instrument with a cross-shaped structure for underwater magnetic measurement [26]. An Italian team developed a differential tensor instrument with a triangular pyramid structure [27]. University of Defense Technology and Jilin University also developed a differential tensor instrument with a cross-shaped structure [28,29].
Can a fractional gradient of the magnetic field be obtained directly from fewer survey points? Tilbrook established the relationship between the magnetic field and its derivatives through the Taylor series of the magnetic field. The orders of the field derivatives correspond to the index of the series terms. When flux gate sensor rotates about an external axis, its output voltage is modulated by the magnetic field and its derivatives of different orders. Since the terms in the Taylor series also correspond to the harmonics of the voltage, the field derivatives can be further obtained [30]. Inspired by his work, the Taylor–Riemann (TR) series is introduced [31]. The terms of the TR series include the fractional derivative factor. We truncate the TR series to approximate the original function. Then, we measure the magnetic field at several points and take them as the original functions to be expanded by the unknown TR series. Take these series as equations and the unknowns as the factors of these TR series. Finally, the fractional derivatives of the field are obtained by solving these equations. In this way, we can obtain the fractional derivative of the magnetic field with fewer survey points and make it possible to measure the fractional derivatives in real time.
2. Derivation of the Measurement Principle
2.1. Introduction to Fractional Derivative
The fractional derivative is a generalization of the integer-order derivative. There are many definitions of the fractional derivative based on different generalizations. The definitions used in this article are the GL fractional derivative, the RL fractional derivative and the Cauchy-type fractional derivative.
The GL fractional derivative comes from the limit of the difference quotient of the higher-order integer-order derivative. It is often used in numerical computations. The definition of the GL fractional derivative at is as follows:
where denote the start point and end point of the derivative, respectively. denotes the order of the derivative. denotes the size of sampling grid. Function [⋅] returns the nearest integer. In this article, we take the GL derivative to obtain the numerical result of the fractional derivative of the magnetic field.
The RL fractional integral is derived from the higher-order integral. It does not involve the limit operation and is often used in analytical analysis. The RL fractional integral at is as follows:
where . The RL fractional derivative is the integer-order derivative of the RL integral:
where . The ceiling function returns the smallest integer which is not less than the input number. If the function is -times continuously differentiable in the interval and is integrable in , the GL and RL fractional derivatives of are equivalent [32]. In this article, we use the RL definitions to derive the expression for the fractional derivative of the two-dimensional magnetic field.
Cauchy-type fractional calculus is a generalization of Cauchy’s integral formula. Cauchy-type fractional calculus at is as follows:
where . and are complex numbers. is the contour of integration. Unlike the previous two definitions, this equation holds in the complex plane. The TR series in this article is implemented based on the Cauchy-type fractional derivative.
In this article, we use these three types of fractional derivatives because they are direct extensions of integer-order derivatives without any other constraints. For example, compared to another widely used Caputo calculus, the GL, RL and TR definitions are continuous when their derivative orders approach integers, which shows a good transition. Furthermore, they are equivalent in this application, making it easy to convert and validate against each other. For definitions of fractional calculus such as the Caputo, Atangana-Baleanu, Riesz, Weyl etc., if their series contain the factors of fractional derivatives and hold in the complex plane, they can also be applied by a similar method described below.
2.2. Introduction to Taylor–Riemann Series
Riemann scratched down a generalized Taylor series based on fractional derivatives in 1847, but he never proved it. It was not until 1945 that Hardy proved that it is convergent in a weak sense [33]. Osler gave a proof of pointwise convergence of the series [34]. Munkhammar rewrote Osler’s proof, and we rewrite it as follows:
Theorem 1.
Function is analytic in some simply connected domain containing , and . Then we have
where , is on the circle and .
We call (1) the Taylor–Riemann (TR) series. The derivative in (1) is the Cauchy-type fractional derivative:
The contour of the integration starts at , encircles in the positive sense and returns to .
The variable of the Cauchy-type derivative is the complex number , which consists of two variables and . But the other two definitions, the RL and the GL, are univariate. The TR series given by Munkhammar adopt the Cauchy-type fractional derivative in complex form, which has two variables. Therefore, it is possible to evaluate the fractional derivative of the two-dimensional magnetic field.
The variable keeps its form on both sides of (1), which makes it look like a univariable function. Can we apply the RL derivative to the complex function ? We rewrite the definition given by Munkhammar:
Definition 1.
Function is analytic in some simply connected domain containing the points and . Then we define
with integration along the straight line connecting and .
Then, the relationship between the Cauchy-type fractional derivative and the RL derivative is [31]:
Theorem 2.
The function is analytic in some simply connected domain containing and . Then, the Cauchy-type fractional integral of is a complex generalization of the Riemann–Liouville fractional derivative
for all , except .
Therefore, the Cauchy-type fractional derivative can be transformed into the RL derivative by changing the contour from circle to line , as shown in Figure 1. In addition, the RL derivative is equivalent to the GL derivative. In this article, the GL derivative is used to verify the result of the RL derivative.
Figure 1.
Contour of Cauchy-type fractional integration.
2.3. Implementation of the Measurement Principle
The Taylor–Riemann series (1) is an infinite series. It must be truncated to a finite series to approximate the function . In the proof given by Munkhammar, is also the dummy index of the Fourier series coefficients. Therefore, the terms must be symmetric about , and the number of terms is always odd and . Now, truncate it to N terms about :
where , satisfy . The coefficient is as follows:
Our goal is to evaluate the fractional derivative , which is one of the unknown derivatives . This can be carried out by solving equations. Establish equations as (2) by changing the position on the circle :
Rewrite it in matrix form:
where , and , respectively. Fractional derivatives can be worked out by evaluating . It is difficult to evaluate directly, and we decompose it into . Let and , then:
and are diagonal matrices, and it is easy to calculate their inverse. Rewrite the equation as . Since we only take the element in , the corresponding row is the central row of . is the number of survey points on the circle . Too many survey points make them close to each other, and the magnetic field measured at survey points become similar. Therefore, we usually take no more than nine survey points on the circle. With the help of software Mathematica (Version 12.1, Wolfram Research, Champaign, IL, USA, Inc.), we find that the central row of is for . The others are in and the diagonal of . Therefore,
After the above preparation, we next apply the above process to magnetic field components. The magnetic field components and of the two-dimensional magnetic field are used to construct the function :
where is the real axis of complex plane, and is the imaginary axis. Equation (4) must be analytic in the complex plane . That is, it must satisfy Cauchy–Riemann conditions:
It is known that the magnetic field is a passive field, and its divergence in three-dimensional space is 0, which can be expressed as follows:
In area without current distribution, the magnetic field is irrotational:
The irrotational property (8) makes satisfy (5). But for (6), it can only be satisfied when in (7), which means that the magnetic field component perpendicular to the complex plane remains unchanged in its direction. Therefore, this method is available for two-dimensional magnetic field.
Solution is also a complex number. According to the linear property of fractional derivative, it can be written as follows:
To determine the value of in (2), it is necessary to determine the center and the radius of the circle , as well as the position of the survey points on the circle . For other variables, is the dummy index, and is the derivative order.
The principle of measuring two-dimensional magnetic anomalies using the TR series has been derived above. Next, an example is designed to simulate the measurement process.
3. TR Method Simulation
3.1. Simulation Setup
In this example, current-carrying wires are used to generate a two-dimensional magnetic field. The simulation setup is shown in Figure 2.
Figure 2.
Simulation setup.
A pair of long wires with the length of is perpendicular to the complex plane. Their coordinates in the complex plane are and . The complex plane is located at the center of long wires. The wires carry a current of 14.4 A in opposite directions. Take the circle , in the complex plane. During actual measurement, the magnetic field is unknown, so we set survey points uniformly distributed on circle . We evaluate the fractional derivative at by the magnetic components , measured at on the circle. Next, we have to determine the length to make it similar enough to a two-dimensional field.
The cylindrical coordinate system is established. One of the long wires is the rotation axis , and the center of the wire is the origin, as shown in Figure 3. The complex plane is perpendicular to the -axis and passes through the point . is the rotation angle in the cylindrical coordinate system.
Figure 3.
Evaluate the magnetic field of the finite line current.
When and , the magnetic field at point is given by the following:
Since there is no component in z direction, any straight line can generate a two-dimensional field. The factor only affects the field strength. When ,. The length of the wire tends to be infinity with respect to , and the field can be regarded as a two-dimensional field. In practice, the length can be increased to approximate the infinite case.
In addition, the impact of the short sides with the length of must be considered. It can be seen from (10) that the long sides with the length of do not generate the magnetic field component . Short sides and long sides form a current loop, and the short sides produce the magnetic field component , and the gradient (component disappears in the complex plane because of the symmetric position of the short sides around the complex plane and the inverse direction of the current). They are added to the magnetic field and the magnetic derivative of two long sides, which can make the magnetic field away from of the infinitely long wire and violate the constraint . Therefore, the short sides must be away from the complex plane, which can also be achieved by increasing .
When , in the complex plane, the contours of of short sides and long sides are shown in Figure 4. The range of Figure 4 covers the measurement area.
Figure 4.
(a) of short sides; (b) of long sides.
For the vertex at 0.7 + 1.5 i that is farthest from the left line source, = 0.9273. It means that the strength of the magnetic field generated by the finite long wire is at least 92.73% of that of an infinitely long wire in this region. We consider it the field of the infinitely long wire. The overall of short sides is in the range of 479 nT~546 nT, while that of the long sides is thousands of nanotesla in most of the given range. We also plot the contours of of the short sides and long sides separately in Figure 5.
Figure 5.
(a) of the short sides; (b) of the long sides.
The situation is similar to the previous one. of the long sides is quite larger than that of the short sides. Therefore, the short sides hardly affect and generated by the long sides.
3.2. Single Point Simulation
After determining the magnetic field, we perform a single point simulation to obtain the fractional derivative at . First, we generate the magnetic field component , at the survey points and construct according to (4). Then, we substitute all parameters into (3) and evaluate it. Finally, we separate and from according to (9). Since the real part is always 0 at , we consider only . Figure 6 shows under different derivative orders and the start point of the fractional derivative.
Figure 6.
under various derivative order and start point .
The curves of with different intersect many times when the start point approaches the point . We divide these curves into several segments at the intersections and sort by the value of in descending order in each segment. When , the order is 0.2, 0, 0.5, 0.8, 1. Note that and . When , the order is 0.2, 0.5, 0, 0.8, 1. We can see that the order changes. The orders in other segments are also different. It shows that affects the peak value of . The fractional derivative is a transition between integer-order derivatives, and the value of should monotonically change as increases from 0 to 1. Additionally, the closer is to , the larger the value of , which is unstable. Therefore, must be set to keep the derivative interval wide enough as the first segment shown in Figure 6.
According to the definition of the GL derivative, we can also measure the GL derivatives on the interval from the start point to the end point by sampling magnetic fields on the interval. It is another method to calculate the fractional derivative of the magnetic field. Because the GL and RL definitions are equivalent, we can verify the TR method by the GL method. We take = 10, 30, 100 survey points on the survey line from to , and their results are shown in Figure 7.
Figure 7.
obtained by the GL and TR methods. Number of samples in the GL method: (a) = 10; (b) = 30; (c) = 100.
Open markers denote obtained by the numerical method according to the GL definition. When there is no noise, regardless of the number of survey points in the GL method, the open markers almost overlap the corresponding line obtained by the TR series. Therefore, the value of obtained by the TR series is reliable.
3.3. Survey Line Simulation
We perform a simulation on a survey line whose equation is . We also take the start point into account to show its effect. on the survey line is shown in Figure 8.
Figure 8.
on the survey line when: (a) ; (b) ; (c) .
In terms of the properties of the fractional derivative itself, each subplot shows the same trends that the curve of transforms to as the derivative order increase. When = 0 and = 0.5, the curve forms a flat top near the center, which is similar to the curve of . There are two peaks around the center, which is the characteristic of . As decreases to = 0.2, the flat top rises, and the peaks fall. This means that the partition of increases, and the partition of decreases. And it is reversed as increases to = 0.8. This shows that the fractional derivative has both the properties of and . But as the start point increases and gets closer to the end point , the curves get closer to each other. For example, when = 0.16 m in (c), the curves of = 0.5 and 0.2 are almost the same. Therefore, the start point must not be too close to the end point .
Considering there are many curves in Figure 8, to clearly compare the TR and GL methods, we just plot the difference between them in Figure 9. Because the number of survey points has little effect on the result when there is no noise, we just take .
Figure 9.
Difference between the TR and GL methods. (a) = 0; (b) = 0.08 m; (c) = 0.16 m.
When = 0 as shown in (a), the GL and TR derivatives are inconsistent near 0.5 where the line current is located. This is because circle is too large, and the distribution of survey points on circle is not dense enough to capture the drastic change in . As increases, the circle becomes smaller, and the survey points become closer together. This allows sensors to capture more detail. For example, when = 0.08 m and = 0.16 m in (b) and (c), respectively, compared to = 0, the differences between the TR method and the GL method are smaller.
Next, we add Gaussian noise with a standard deviation of 500 nT to the magnetic field component and simulate the measurement when = 0.08 m and = 5 to study the impact of the noise. The results are shown in Figure 10.
Figure 10.
on the survey line with Gaussian noise when the derivative order in the TR and GL methods is: (a) = 0.2; (b) = 0.5; (c) = 0.8.
Focusing on the curves of the GL method and , we find that the curves of the GL method are proportional reductions of . Then, considering the curves of the TR method, the curves of the TR method are smoother than those of the GL method at the same derivative order, and their shapes are not similar to at all.
The survey points of the GL method are on the straight line from the start point to the end point , which is different from the TR method. The number of the survey points in the GL method can also affect the result when there is noise in the magnetic field. In order to show this, we also plot obtained by the GL method with a different number of survey points. The results are shown in Figure 11.
Figure 11.
of the GL and RL method. The numbers of survey points are the same in each row. The derivative orders are the same in each column.
We can see that with the increase in the derivative order in each row, the amplitudes of the GL method increase rapidly, while the results of the TR method are still stable. In each column, as the number of survey points in the GL method increases, the results of the GL method are increasingly affected by noise.
To explain this, we take the values of as the complex random variable and the values of as the complex random variable [35]. Then, we denote the variance of as . Note that because . From (3) we can see that is linear function of . According to the properties of variance, can be expressed as follows:
According to the definition of the GL fractional derivative, is also a linear combination of measured on the survey line from to , which can be approximated as follows:
where , . Let the value of be the random variable and the value of be the random variable . The variance of is . can be evaluated by the following:
The magnetic gradient can be approximated by the difference quotient of and on adjacent survey points. That is,
Therefore, the variance of can be expressed as follows:
Substituting the values of the parameters previously set in (11) and (12), we obtain the variance of the TR and GL methods shown in Table 1:
Table 1.
The variance of obtained by the TR method and the GL method at various derivative order .
The value of is 1730.1 , which is much larger than all of those in Table 1. The variances of obtained by the GL method are much larger than those of the TR method. All of them are consistent with Figure 10 and Figure 11.
Therefore, compared to the GL numerical method, the TR method can effectively reduce Gaussian noise. In addition to the fact that the fractional derivative itself can suppress noise by sacrificing resolution, the TR method can also suppress noise during measurement.
4. Experiment Implementation
Finally, we put the measurement into practice. We choose a value of 0.08 m for the start point and the values of the other parameters are the same as before.
As shown in Figure 12, a rectangular coil is placed on the ground, with the long side = 10.5 m and the short side = 1 m. In order to avoid the influence of the fluctuation of the magnetic field in the urban area, a sinusoidal current with an amplitude of 14.4 A and a frequency of 10 Hz is introduced into the coil. Then, the magnetic field generated by the sinusoidal current can be separated by Fourier transform.
Figure 12.
Measurement of the fractional derivative on survey line by the TR series. The symbols Re and Im indicate the real axis and the imaginary axis respectively, and the symbol z denote the z-axis. The symbol is the distance between two long sides, and it is also the length of the short sides.
The yellow board is in the complex plane. It is perpendicular to the long sides and at the center of the long sides. The real axis is vertical, and the imaginary axis is horizontal. The radius of the circle is 0.17 m. Five holes are uniformly distributed on the circle to hold the fluxgate sensor. The start point is on the circle , and the end point is the center of the circle.
The survey line is horizontal and 0.25 m above the ground. We use the aluminum rail with a ruler attached to indicate the horizontal position on the survey line. The center of the circle is on the survey line, and its range of movement on the survey line is (−1.5 m, 1.5 m). The distance between the survey points is 0.1 m. Then, the measurement is performed, and the magnetic field components , measured at each survey point are shown in Figure 13.
Figure 13.
Magnetic field components measured at . Field components: (a) ; (b) .
We also plot the exact values in Figure 14 for comparison.
Figure 14.
Exact values of the magnetic field component at each . Field components: (a) ; (b) .
We find that the measured values near y = ±0.5 m where the current is located are larger than expected. This is because the magnetic field changes rapidly near the current as shown in Figure 14b, and a small position error can cause significant changes in the measured values.
Then, we calculate with the order of = 0.2, 0.5, 0.8 according to (3). The results are shown in Figure 15.
Figure 15.
Measured and accurate value of with the derivative order of: (a) = 0.2; (b) = 0.5; (c) = 0.8.
The calculated result is close to the analytical result. Therefore, the TR method is valid for fractional derivative measurement and can suppress the noise.
5. Conclusions
In this article, a method for measuring the fractional derivative of the two-dimensional magnetic field is derived by using the Taylor–Riemann series and the analytic function of the two-dimensional magnetic field. The simulation and experiment show the effectiveness of this method. Furthermore, this method can effectively suppress Gaussian noise, and it is possible to obtain fractional derivatives in real time from a few survey points.
Author Contributions
Conceptualization, Y.S.; methodology, Y.S.; software, R.W.; validation, R.W. and Y.S.; writing—original draft preparation, R.W.; writing—review and editing, R.W. and Y.S. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by National Key Research and Development Program of China, grant number 2021YFB3900200.
Data Availability Statement
Data are contained within the article.
Conflicts of Interest
The authors declare no conflicts of interest.
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