﻿ Determination of the Electromagnetic Field Created by Line Current and Sheet Current Source at the Earth’s Surface

International Journal of Geosciences
Vol.05 No.13(2014), Article ID:52602,9 pages
10.4236/ijg.2014.513129

Determination of the Electromagnetic Field Created by Line Current and Sheet Current Source at the Earth’s Surface

Ghada M. Sami1,2, Maryam I. Al-Nami1

1Mathematics and Statistics Department, Faculty of Science, King Faisal University, Al-Hassa, KSA

2Mathematics Department, Faculty of Science, Ain Shams University, Cairo, Egypt

Email: g_sami2003@yahoo.com   Received 24 September 2014; revised 20 October 2014; accepted 15 November 2014

ABSTRACT

The electromagnetic field that generated by line current and sheet current at the surface of the earth can be expressed in analytical form. The line current created at the earth’s surface by an infinitely long line current is given by the inverse Fourier integrals over a horizontal wave number. The sheet current can be obtained by integrating the line current expansions using a Neumann and Struve functions; these functions have known mathematical properties, including the series expansions. The series expansions are exact with neglecting the displacement currents. Assuming a uniform earth and that there is no propagation, the three nonzero field components can be expressed in terms of the Neumann and Struve functions. The integrals of line current expansions are calculated by using the numerical methods. The results represented graphically and illustrated by figures. Results can be used to evaluate numerical solutions of more complicated modeling algorithms.

Keywords:

Electromagnetic Field, Transient Analysis, Series Expansions 1. Introduction

In the last few decades, there has been increased interest in the behavior of electromagnetic systems which are operated near a conducting earth. Many of these systems have been successfully used to measure the electromagnetic properties of the earth. That is, if the field of a transmitting source can be calculated in terms of idealized earth models, then measurements of actual fields near a real earth can be interpreted in terms of these models. This method is known as the induction method of geophysical exploration   . A part of the integrand may be inverse Fourier integral form using the fast Fourier transforms such that the resulting integrals are known  . However, they presented only a particular form of decomposition of the integrand. Other studies have been applied to the probing of the fields in geological media  -  , determination of the current in a lightning return stroke  , the detection of nuclear bursts Johler  , and the discrimination of a radar scattered  . In the present study, we will focus on the effects caused by the presence of the earth’s surface. We are interested in the problem of electromagnetic field. Also, few electro-magnetic problems have been investigated along these lines  ,  .

Electromagnetic boundary conditions at the surface of the wire were leading to a characteristic equation that determines the propagation constant along the wire  . Furthermore, Bishay et al.  computed the transient electromagnetic field of a vertical dipole on a two-layer conducting earth. Sami  calculated the influence of a magnetically permeable surface layer on transient electromagnetic field of a vertical magnetic dipole on a two- layer conducting earth. Bishay and Sami  studied Time-domain study of transient fields for a thin circular loop antenna. However, using a quasi-static approach, Wait  has derived closed-form solutions for the fields of loops above the surface of a two-layered earth, that are valid at sufficiently late times. A classical work in this subject is the remarkable book  and Wait  , for the electromagnetic fields of a phased line current over a conducting half-space. A very readable contemporary review was written by Olsen  who provides many significant references. Pirjola  considered the general case of a propagation current wave and derived formulas which give the electromagnetic field at the surface of the earth in an inverse Fourier integral form. The surface fields are also affected by currents induced within the ground and influenced by the conductivity of the Earth. This also has to be taken into account. Neglecting the currents displacement, thus making the quasi-static approximation, which is always permissible in geophysical applications, and assuming a uniform earth and that there is no propagation, the three nonzero field components can be expressed in terms of the Neumann and Struve functions. These functions have known mathematical properties, including their series expansions. The latter are utilized in this work to derive expressions for the electromagnetic field. In the previous work, the magnetic X and Z components are obtained from the electric Y component at the earth’s surface, neglecting the real part of electric field, and imaginary part of magnetic field.

The main objective of paper is to determine the electromagnetic field due to a line current and sheet current. Sheet current having a finite width implies a more realistic model. It can be obtained by integrating the line current expansions using a Neumann and Struve functions. These functions have known mathematical properties  , including the series expansions. The medium in which the line current lies in non-conducting (the air), and the other half-space is conducting (the earth). In this paper, the electric X and Z components are obtained from the magnetic Y component at the earth’s surface, we are considering the real and imaginary parts of electric field components and taking into account.

2. Line Current Model

In the Cartesian coordinate system (x, y, z), we assume that the earth’s surface is the xy plane, and the line current J flows is parallel to the y-axis at a height z = −d. The line current oscillating harmonically in time above a uniform half-space. The earth, characterized by a conductivity σ, a permittivity , a permeability μ, and a propagation constant K, where . (1)

A model containing an infinitely long line current parallel to the surface between two half-spaces is frequently used in electromagnetic applications extending from geophysics. The medium in which the line current lies is nonconducting (the air), and the other half-space is conducting (the earth). The line current flows parallel to the y-axis at a height Z = ‒d. Neglecting displacement current effects, and assuming that is the vacuum permeability, then the propagation constant ᶄ of the earth is defined by . (2)

The magnetic field has only the magnetic field component , and the non-zero electric field components are and , now we shall give the expressions for the electromagnetic field as , (3) , (4) . (5)

R is the reflection coefficient at the earth’s surface is depending on the conductivity structure of the earth, and is given by, (6)

and J gives the magnitude of the line current oscillating harmonically in time . To get the electric and magnetic fields at the earth's surface, then from Equations (3)-(5) we get, (7) (8) (9)

The components of the electric fields are expressed in terms of through the relations

, (10)

. (11)

Equation (7) can be written in Terms of Struve function of the first order and the Neumann function of the first order  :

(12)

The Neumann function and the Struve function can be expressed as a series expansion  ,

, (13)

, (14)

where denotes the Bessel function of the first order, is Eulers constant (≈0.5772) and is given by

(15)

The function has the series expansion

(16)

where is given by 

. (17)

and is defined by

. (18)

The gamma function Г satisfies,

. (19)

The expansions of the Neumann and Struve functions Equation (13) and (14) with (16) may now be substituted into (12) to obtain a series representation for the magnetic field, which is straight forward algebra. It appears that the terms resulting from the function on the right-hand side of (13) exactly cancels the last term in (12), and the final series expansion can be written as

, (20)

where

, (21)

and

, (22)

. (23)

By applying the series expression of in (10) and (11) the series expansions of the components of the electric fields and are obtained in a straightforward manner as

(24)

.(25)

3. Sheet Current Model

To determine the electromagnetic field created by the sheet current source at the surface, a sheet current can be lies in non-conducting (the air), and the other half-space is conducting (the earth). The sheet current having a finite width implies a more realistic model. It can be obtained by integrating the line current expansions using Neumann and Struve functions. We now consider an infinitely long sheet current on surface of the Earth. Let be the current distribution in the sheet. If the function can be normalized as follow,

. (26)

Applying [(7)-(9)] for each line current lying at, the following formulas are obtained for the electric and magnetic fields at the Earth’s surface at a location determined by x can be written in the form

, (27)

, (28)

. (29)

The electric field by (28) and (29) is expressible in terms of the magnetic field (28)

, (30)

. (31)

Rewriting (20) with and K replaced by and, this yields

, (32)

where

, (33)

and

, (34)

, (35)

where is the equivalent propagation constant and defined as

, (36)

and if we assume that the wave number then the plane wave surface impedance can be written as

. (37)

Let us define the functions and by

, (38)

and

. (39)

We know that

, (40)

(41)

, (42)

and

. (43)

A straightforward algebraic manipulation now allows for expressing (32) as

, (44)

the quantities and given by

, (45)

and

(46)

where

(47)

We now consider a uniform sheet located between and, then

(48)

Assuming to be valid, , then the electric field components are obtained as:

, (49)

, (50)

where

(51)

and

(52)

(a) (b) (c) (d) (e) (f) (g) (h) (i) (j) (k) (l)

Figure 1.(a)-(d) represent the imaginary part of the magnetic field component Hy due to a line current of 1 MA with different values of distance x at the periods 10 s, 50 s, 100 s, and 700 s, respectively. (e)-(h) represent real and imaginary parts of the electric field component Ez, and (j)-(l) represent real and imaginary parts of the electric field component Ex, at the earth’s surface due to a line current of 1 MA with different values of x at the periods 10 s, 50 s, 100 s, and 700 s, respectively. The continuous and dots curves correspond to the real and imaginary part of the electric field, respectively.

(a) (b) (c) (d) (e) (f) (g) (h) (i) (j) (k) (l)

Figure 2.(a)-(d) represent the imaginary part of the magnetic field component Hy due to sheet current of 1 MA with different values of distance x at the periods 10 s, 50 s, 100 s, and 700 s, respectively. (e)-(h) represent real and imaginary parts of the electric field component component Ez, and (j)-(l) represent real and imaginary parts of the electric field component Ex, at the earth’s surface due to sheet current of 1 MA with different values of x at the periods 10 s, 50 s, 100 s, and 700 s, respectively. The continuous and dots curves correspond to the real and imaginary part of the electric field, respectively.

4. Numerical Results

Numerical computation of the electromagnetic field that generated by line current and sheet current at the surface of the earth can be easily performed, based on the Equations [(12), (24) and (25)] and [(44), (49) and (50)], respectively. The following parameters have been chosen to draw the curves shown by Figures 2(a)-(l):, , , and conductivity.

The electromagnetic field defined as a function of x coordinate at the surface of the earth due to line current and sheet current and plotted against the distance x.

For line current, Figures 1(a)-(d) represent the imaginary part of magnetic field component, Figures 1(e)-(h) describe the real and imaginary part of electric field components, and, at the periods 10 s, 50 s, 100 s, and 700 s, respectively.

For sheet current, Figures 2(a)-(d) represent the imaginary part of magnetic field component, Figures 2(e)-(h) describe the real and imaginary part of electric field components, and, at the periods 10 s, 50 s, 100 s, and 700 s, respectively.

The magnetic and electric fields were treated as complex quantities, the real part of the right-hand side of Equations (3)-(19) is ignored. It is seen that the magnetic field component is dominated by the imaginary part, and the real part of the electric field components and are larger than the imaginary part.

The results we obtained that with increasing in the period indicate to increase in the imaginary part of magnetic field component, and with increasing in period corresponding increasing in the values of the real and imaginary parts of the electric field components and.

We compared the magnetic and electric fields at the surface of a uniform earth with those produced by line current and sheet current.

In the sheet current, the values of the imaginary part of the magnetic field component are less than the values of the imaginary part of the magnetic field component in the line current. The real and imaginary parts of the electric field component in the sheet current are less than the electric field component which obtained in the line current for the periods 10 s, 50 s, 100 s, and 700 s, respectively.

From a physical point of view, this means that the series expansions including the propagation constant is reasonable, the propagation constant depends on the surface impedance. The absolute values of and are less with. While the sheet current of 1 MA parallel to the y-axis at height z = −d, the values of the real and imaginary parts of the electric field component, is greater than the values of the real and imaginary parts of in the line current, for the periods 10 s, 50 s, 100 s, and 700 s, respectively.

5. Conclusions

We conclude that the electromagnetic field at the earth’s surface created by line current can be expressed in terms of the Neumann and Struve functions, and take the conductivity of the earth into consideration.

The magnetic and electric fields were derived in new series expansions and computations. Also we present the magnetic and electric fields due to sheet current obtained by integrating the line current expansion. The results are represented graphically. We compared the results of the magnetic and electric fields values at the surface of a uniform earth with those produced by line current with sheet current.

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