1. Introduction
In 1896 A. Sommerfeld first proposed integrals for describing the diffraction of a plane wave in a problem on a half-line with ideal boundary conditions, which later received his name [
1]. Later, at the beginning of the 20th century, Sommerfeld used the apparatus of SIs to solve the problem of diffraction of a plane wave at angles [
2]. This also includes the exact solution of the problem of diffraction on an ideally reflecting half-plane, as well as his famous work on wave propagation in wireless telegraphy, the so-called Sommerfeld problem, involving two half-spaces filled with air and a lossy earth [
3,
4]
The mathematical apparatus of SI was further developed by Carslaw [
5], and by G.D. Malyuzhinets [
6], whose method enables us to solve diffraction problems in angular regions under various boundary conditions regardless of the angle.
From, the voluminous amount of published data, one may refer to the works of Fock [
7], Van der Pol [
8] and many others.
The calculation of SIs has both practical and theoretical significance since they can be used as Green’s functions in the frame of integral equation formulations. In recent years, reports on combining analytical approximations and numerical computations have been published [
9,
10,
11,
12].
The article further considers two asymptotic methods for calculating SIs in the form of a sum of an infinite power series, when under the integral as a rapidly oscillating function there can, as a rule, be an exponential function or its product by the HF.
2. General Solutions of Maxwell’s Equations
Maxwell’s equations for stationary electromagnetic fields with wave number
equations
can be reduced to the Helmholtz equations
The charge density
can be removed from the equation (2) by expressing it through the current density
j using the charge conservation law
.
We will assume that all dynamic quantities in the above equations depend on time according to the harmonic law
. The dipole radiates time-harmonic electromagnetic (EM) waves at angular frequency
[
13] (
time dependence is assumed).
By performing the convolution operation on both sides of the equations (
1), (2) and taking into account the equation for the Green’s function
we obtain general form of solutions to the Helmholtz equations
Using the Fourier operator, solutions to the equations (
3), (4) can be written as
where
are the Green function and its Fourier transform respectively,
j is the current density,
is its Fourier transform, ∗ is the convolution symbol through all coordinates. Note that when performing the Fourier transform into (
3) and (4) it is convenient to use the formal substitution
3. Field of a Hertz Point Radiator in Integral Representation
Prior to calculating the SIs, it is necessary to get integral representations of the fields of a Hertz point emitter, as the dipole current density is determined quite simply.
A vertical point (Hertzian) dipole, characterized by dipole moment
,
, is directed to the positive
z axis, at altitude
. The dipole moment
p corresponds to the current density
and its Fourier image
Fourier inversion (
5) in a cylindrical coordinate system
can be easily calculated using the integral representation of the Bessel function
and the residue on the complex
plane.
Substituting the expression (
10) into (
5) and keeping in mind the relation
, we finally obtain the integral representation of the magnetic field of the emitter (in the form of the so-called inverse Hankel transform)
Making similar calculations in (6), we find the integral representation for the electric field
Now, using the transformation (
A1) (see
Appendix A), we can replace the Bessel function in the expression (
12) for the magnetic field by the HF
This can be done similarly for the electric field in (
13)
Note that the integral (
14) can be calculated accurately
using the integral representation of the spherical wave
The same result can be easily obtained from (
3) by calculating the convolution directly
It should be noted that the exact expression for the integrals, as in (
14), (
18), can serve as an auxiliary integral, called the standard integral [
14].
It is easier to obtain an exact expression for the electric field by calculating the curl of the expression (
16) in a cylindrical coordinate system, according to the equations (3) and (
3)
In a spherical coordinate system it will take the form
due to transformations of basis vectors
4. Generalized Asymptotic Formula for SI
Let us represent SI in the general form
where
is an analytical function, and the phase function
is rapidly oscillating, which, according to the condition
has a saddle point
.
Let us expand the function at the saddle point into a Taylor series
by series coefficients
Then SI (
23) can be reduced to the auxiliary integral (
A4) and represented as an infinite series
4.1. Calculation of HF Asymptotics
Consider as the integral
I in (
23) SI representation of HF
In order to obtain the asymptotic formula for the HF in the form of a power series, it is sufficient to make the following substitutions in (
23):
and calculate the initial coefficients of the series
As a result, we get the well-known asymptotic expansion of HF of the first type for
(see [
15])
The main term of the series is (
)
5. Asymptotic Expansion of the Integral Transformation Whose the Kernel is the Product of the Exponential and HF
Consider an integral of the type
where
is a complex-valued function,
Here we have to use the auxiliary (standard) integral
which follows from (
32) (in the case of
) and can be directly calculated using the expression (
18).
Note that the integrand function
F has a saddle point
, which satisfies the condition
where
The root of the equation (
34) for large values of the argument asymptotically approaches a real value
due to the asymptotics of HFs in (
31) (
).
Table 1 shows the numerical solutions of the equation (
34), as well as their approximate values, according to the asymptotics in (
35) for
,
.
Table 1.
Exact and approximate values of saddle points (, ).
Table 1.
Exact and approximate values of saddle points (, ).
Saddle point |
Approx. |
|
Calcul. error |
Error ratio |
|
|
|
(in %) |
(in %) |
49,4+i 9.5 |
49.5 |
2 |
0 |
19 |
62.7+i 4.9 |
62.6 |
4 |
0 |
8 |
68.0+i 2.4 |
66.4 |
6 |
|
4 |
69.4+i 1.4 |
67.9 |
8 |
|
3 |
69.8+i 0.9 |
68.6 |
10 |
|
2 |
69.9+i 0.6 |
69.0 |
12 |
|
1.5 |
To calculate the integral (
32), we first expand the function in a Taylor series
in the saddle point
.
Substituting the function
in (
32), the integral
can be reduced to a simple integral, which can be calculated by
n multiple differentiation of the integral (
33) with respect to the parameter
z
Thus, the integral (
32) is represented as an infinite series
Here the main term of the asymptotic series is
Note that the traditional calculation of the integral (
32) using the saddle point method along the Sommerfeld contour on the complex plane
gives the same result as in (
39)
where integration is carried out over the angular integration parameter
, according to the transformation
.
6. Discussion
SI is represented as an infinite power series. Such an asymptotic series (
26) allows one to calculate SIs with a given accuracy if
G and
are analytic functions. Using the example of the asymptotic expansion of HF (
30) in subsection 4.1, we demonstrate an estimate of the accuracy of calculating SI, where
G and
are chosen as integer functions. However, it should be noted that the expression (
26) loses its validity when the functions
G and
have singularities near the saddle point.
Obviously, the function , as a rapidly oscillating part of the integrand, affects the accuracy of the asymptotics of SIs. Therefore, in
Section 5, a special integration technique is proposed. It should be noted that the value of the saddle point, because HF
is complex, and its imaginary part becomes vanishing at large values of the function argument.
It is interesting to note that the wave attenuation does not depend on the imaginary values of
and
. In fact, the exponent of the initial two terms of the series
does not contain
or
, although, on the other hand, they are components of the wave vector (
).
It should be noted that the integral in (
32) can be effectively applied in solving the Sommerfeld problem in a half-space [
16]. For the magnetic field of reflected waves
where the main term of the series is expressed through the magnetic field of the emitter (
16) and
. Here the function
R has the meaning of the Fresnel reflection coefficient. It is convenient to calculate the electric field
E through the rotor of the magnetic field
H, similar to (
20).
Further, we plan to take into account the case when the meromorphic function G has singularities on the complex plane in the form of a pole and a branch point.
7. Conclusions
A generalized asymptotic formula for SI is obtained in the form of a complete power series (
26) under the condition that
G and
are analytic functions. The proposed method for integrating SI involves a rapidly oscillating function of an exponential type, therefore, in solving practical problems, the asymptotics of HFs can often be used as an exponent. The integration technique was tested on the example of finding the asymptotics of HFs in the form of a series, where it (
30), as expected, turned out to be identical to the previously known formula. The inverse Hankel transformation is reduced to the form of an integral along the real axis (
32), where the rapidly oscillating part of the integrand, in addition to the exponential, contains HF. Moreover, the integrand function (
32) has a singularity in the denominator in the form of a branch point.
The integral is represented as the sum of the asymptotic series (
38) at the saddle point
. It is shown that the value at the saddle point is complex, whereas far from this point it tends to a real value.
In the quasi-static approximation
the formula (
41) is obtained, which leads to the interesting conclusion that the imaginary value of the saddle point, as can be seen from the formula, practically does not participate in the attenuation of waves, despite the fact that
is actually a component of the wave vector of the beam. It is shown that the leading term of the infinite series (
39) and SI along a contour on the complex plane
calculated by the saddle-point method are, as one would expect, identical. The integral
F in (
32) can be effectively used in solving the Sommerfeld problem for the magnetic field of reflected waves (
42). In this case, the electric field is more easily determined through the rotor of the magnetic field.
Author Contributions
Conceptualization, S.S.; methodology, S.S.; software, M.S.; visualization, K.B.; data curation, M.P.; formal analysis, M.P. and K.B.; investigation, S.S. and M.S.; writing—original draft preparation, S.S. and M.S.; writing—review and editing, S.S., M.S. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by the Science Committee of the Ministry of Education and Science of the Republic of Kazakhstan (Grant No. AP19676900).
Acknowledgments
The authors are grateful to L.E. Strautman for her help in translating the text into English.
Conflicts of Interest
The funders had no role in the design of the study; in the collection, analyses, or interpretation of data; in the writing of the manuscript; or in the decision to publish the results.
Abbreviations
The following abbreviations are used in this manuscript:
SI |
Sommerfeld integral |
HF |
Hankel function |
Appendix A. Replacing the Bessel Function by HF in the Inverse Hankel Transformations
Let an arbitrary function
satisfy the condition
then there is a representation of the inverse Hankel transform of order
of the function
Proof. Using the representation of the Bessel function
and the analytical continuation of HF of the second kind
the integral along the negative real semi-axis can be expressed through HF of the first kind. Then the integrals are combined into one, which is contained on the right side of the expression (
A1), based on the equality of the integrands and the above condition.
It should be kept in mind that HF has a cut along the negative real semi-axis. Therefore, the integration path must run parallel to the cut from above to a vanishingly small imaginary value , which will be omitted in further presentation.
In particular, according to the above condition, the function must be even with respect to the function or .
Appendix B. Auxiliary Integral for Calculating SIs
Asymptotic calculations of SIs can be performed using the following auxiliary integral
In order to calculate the auxiliary integral, we first deform the contour
to the imaginary axis on the complex plane, which passes from top to bottom and slightly deviates from it by an infinitesimal real value to ensure the convergence of the integral. Then the integral can be represented successively as
where the last integral can be found by
m-fold calculation of the derivative with respect to the parameter
on both sides of the equal sign of the expression for the integral
taking into account the representation of the gamma-function
The last integral (
A6) can be easily obtained
using Fresnel integrals [
15] and the substitution
.
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