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Electromagnetic Interferences between Power Systems and Pipelines. Field Vs. Circuit Theory based Models

Authors:
  • SINT Ingegneria s.r.l.

Abstract and Figures

The simulation of the electromagnetic interference between power lines and pipelines at power frequency (50 or 60 Hz) is today a topic of great interest. The reason why this interest is related to the increasing number of situations of interference, but also to the increasing interference effects due to the more performing covering used in modern pipelines. The theory related to the electromagnetic interference phenomenon is directly derived from Maxwell equations and it is well known. The soil reaction can be calculated using the Sommerfeld integrals, a set of equations developed about 100 years ago but still not very well known and difficult to manage. Anyway, Maxwell equations and Sommerfeld integrals can be used for the calculation of the electromagnetic interference in practical cases only using numerical methods implemented in computer programs. The numerical methods suitable for electromagnetic interference simulations can be divided in two classes; field theory based and circuit theory based. The methods based on field theory are general and rigorous but also time consuming in the modelling stage. On the other side, the methods based on the circuit theory in some case are easier in the modelling stage but their accuracy it is not always adequate. This document gives an overview and a comparison between field and circuit based models suitable for electromagnetic interference simulations.
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Electromagnetic Interferences between
Power Systems and Pipelines.
Field Vs. Circuit Theory based Models
R. Andolfato, SINT Srl, Bassano del Grappa (Italy)
D. Cuccarollo, SINT Srl, Bassano del Grappa (Italy)
I. Fara, SINT Srl, Bassano del Grappa (Italy)
ABSTRACT
The simulation of the electromagnetic interferences between power lines and pipelines at
power frequency (50 or 60 Hz) is today a topic of great interest. The reason why this interest
is related to the increasing number of situations of interference, but also to the increasing
interference effects due to the more performing covering used in modern pipelines.
The theory related to the electromagnetic interferences phenomenon is directly derived from
Maxwell equations and it is well known. The soil reaction can be calculated using the
Sommerfeld integrals, a set of equations developed about 100 years ago but still not very well
known and difficult to manage.
Anyway, Maxwell equations and Sommerfeld integrals can be used for the calculation of the
electromagnetic interferences in practical cases only using numerical methods implemented
in computer programs.
The numerical methods suitable for electromagnetic interferences simulations can be divided
in two classes; field theory based and circuit theory based.
The methods based on field theory are general and rigorous but also time consuming in the
modelling stage. On the other side, the methods based on the circuit theory in some case are
easier in the modelling stage but their accuracy it is not always adequate.
This document gives an overview and a comparison between field and circuit based models
suitable for electromagnetic interferences simulations.
Keywords: Electromagnetic Interferences, Computer Modelling, PEEC, Phase Component
Method
INTRODUCTION
This document gives an overview about numerical models suitable for electromagnetic
interferences simulations.
The models described in this document are implemented in the XGSLabTM simulation
environment [13], [14] and in particular in the modules XGSA_FDTM (based on the field theory
model) and NETSTM (based on the circuit theory model).
The first part gives a synthetic description of the reference theory (Maxwell equations and
Sommerfeld integrals).
The second part gives a short description of the numerical methods PEEC (Partial Element
Equivalent Circuit) and PCM (Phase Component Method).
The third part compares results from models based on field and circuit theory in some particular
cases.
THEORY
The electromagnetic interferences are governed by the Maxwell equations. The Maxwell
equations in differential form and in the frequency domain taking into account the constitutive
relations are the following:
rot j

H J E
(1)
rot j

EH
(2)
 
div q
E
(3)
 
0div
H
(4)
where H indicates the magnetic field, J the current density, E the electric field and q the charge
density.
A first important consequence of the Maxwell equations is the charge conservation law that
links charge to current density:
div j q
J
(5)
The properties of the propagation medium can be essentially described by the conductivity σ
(or the resistivity ρ=1/σ), the permittivity ε and permeability μ. The complex permittivity,
conductivity and resistivity are linked by the following equations:
1
jjj

   
 
(6)
The permeability of the propagation media involved in electromagnetic interferences between
power system and pipelines, i.e. air and soil, can be considered uniform and equal to the free
space permeability.
The Maxwell equations can be expressed also in an alternative form using the vector potential
A and the scalar potential U. This approach reduces the unknowns of the problem from six (Ex,
Ey Ez, Hx, Hy Hz) to four (Ax, Ay, Az, U).
The vector potential can be defined as follows:
1rot
HA
(7)
Using (2) it follows:
(8)
An irrotational vector can be expressed as gradient of a scalar potential.
Using the scalar potential U it follows:
gradU j
  EA
(9)
However, A and U are not yet uniquely determined. It is possible to impose an extra condition
using the Lorentz gauge condition:
1
U div div
 
   AA
(10)
Using (10), U can be derived from A and is not strictly necessary to calculate it separately.
Using A, U and the Lorentz gauge condition, the Maxwell equations can be rewritten according
to the following two inhomogeneous and decoupled wave equations also called Helmholtz
equations:
2

 A A J
(11)
2q
UU
 
(12)
In previous equations, Δ indicates the Laplace operator (Δ=div grad), and γ indicates the
coefficient of propagation of the medium:
()jj
  

(13)
The Helmholtz equations indicate that A is related only to currents while U is related only to
charges. The solutions of the Helmholz equations for an unbounded uniform medium are given
by the following two integrals:
4J
r
V
edv
r
AJ
(14)
1
4q
r
V
e
U q dv
r

(15)
were VJ and Vq are respectively the space regions where currents and charges density
distributions are present.
If currents and charges are bordered in thin conductors, previous integrals on volumes can be
replaced by the following integrals along the conductor axis L:
ˆ
4
r
L
e
I dl
r
Al
(16)
1
4
r
L
e
U q dl
r

(17)
In previous equations, l is the length variable along the conductor axis L, and r represents the
distance from a source point along the conductor axis and the field point.
According to (5), the charge density distribution q can be replaced with the leakage current
density distribution dI/dl, and (17) can be then replaced with the follows:
1
4
r
L
dI e
U dl
dl r


(18)
The equations (16) and (18) are the base for numerical integral methods. Some methods like
MoM (Method of Moments) use equations (16) and (10), other methods like PEEC use
equations (16) and (18).
At low frequency, it is usually possible to apply the quasi static approximation. In such case,
the coefficient of propagation effects can be neglected and (16) and (18) became:
1ˆ
4L
I dl
r
Al
(19)
11
4L
dI
U dl
dl r


(20)
This assumption simplify the calculations but can be used only if the size r of the system
composed by sources and victims of the electromagnetic interference is small if compared to
the wavelength of the electromagnetic field λ and then if:
0
23162rf
f

 
 
(21)
At power frequency, this condition is generally fulfilled but it must be checked in case of large
system size or small soil resistivity.
So far the propagation medium has been supposed uniform and extended to the infinite.
In the reality, many systems used in the practice lie in the air on in the soil but anyway close
to the soil surface and then, close to the interface between two propagation media with very
different properties. In the range of the frequencies of interest, the air can be consider a
dielectric medium, and the soil can be considered a conductive medium but unfortunately not
a perfect conductor, which would greatly simplify the treatment.
The electromagnetic fields and the scalar and vector potentials are affect by the presence of
these different media. If the two media can be represented as two half spaces divided by an
unbounded and flat surface, the problem can be approached using the Sommerfeld integrals.
The Sommerfeld integrals allow to calculate the vector potential in the surrounding of an
infinitesimal Hertz’s dipole placed horizontally or vertically close to the interface that divides
two linear and isotropic half spaces. In other words, Sommerfeld integrals represent the exact
solution of the Maxwell equations related to an infinitesimal Hertz’s dipole in the presence of a
lossy half space, taking into account the continuity conditions at the half space interface.
The components Ax and Az of an horizontal dipole are the following:
 
4
xi
A G G U Idl
 
(22)
4
zW
A Idl
x
(23)
The component Az of a vertical dipole is the following:
 
4
zi
A G G V Idl
 
(24)
A dipole with an arbitrary inclination can be represented as a combination of an horizontal and
a vertical dipole.
In previous equations:
22
er
e
G r a h h s z
r
 
(25)
22
ei
r
i i i i
i
e
G r a h h s z
r
 
(26)
 
 
0
0
2esz
ea
e
U J a d



(27)
 
 
0
0
2esz
a
e a a e
e
V J a d
 
 

(28)
 
 
 
0
0
2esz
ae
e a e a a e
e
W J a d
  
   


(29)
22
ee
 

(30)
22
aa
 

(31)
Figure 1 - Reference system for Sommerfeld integrals
In (27), (28) and (29), J0 indicates the Bessel functions of first kind and zero order.
The discussion about the Sommerfeld integrals is clearly out of the scope of this document
and the reader can find any detail in [1].
Eexcept for a few special cases, the Sommerfeld integrals cannot be calculated analytically.
Also the Numerical Quadrature of the Sommerfeld integrals poses difficulties related to the
slow decaying, oscillatory behaviour and poles of the integrand and requires special
techniques using the zeros of the Bessel function and accelerating convergence algorithm.
The Numerical Quadrature of Sommerfeld integrals is anyway a time consuming task.
An interesting option to calculate the Sommerfeld integrals is based on the finitely conducting
earth image theory proposed by Bannister and Dube [5]. This approximation can be obtained
by means of mathematical manipulations of the Sommerfeld integrals. The basic idea is to
approximate the Sommerfel integrals with the effects of only a few spherical wave functions
with closed form.
Anyway it is clear Maxwell equations and Sommerfeld integrals in general can be calculated
only using numerical methods.
NUMERICAL METHODS
Numerical methods suitable for solving Maxwell equations and Sommerfeld integrals in
general conditions have been developed starting on the last decades of previous century and
the development of computer technology and numerical technique have made a decisive
contribution to their progress and diffusion.
Numerical methods can consider electrodes with an arbitrary shape and size, and can consider
the effects of self and mutual impedances, propagation, ionization …, but anyway, for
engineering applications, they require some approximation with regard to soil modelling. The
use of approximate soil models such as the multilayer or multizone model is commonly adopted
ad accepted.
The numerical methods suitable for electromagnetic interference belonging to the so-called
Numerical Electromagnetic Analysis (NEA) methods used to study electromagnetic transients
in power systems. There is not a general consensus in the classification of NEA methods and
these short notes will not be able to clarify the differences and peculiarities of all the various
available methods.
In general it is clear that the accuracy and the application range of a method is more extensive
as the approximations introduced with respect to the Maxwell equations and Sommerfeld
integrals are smaller. In this sense, a first distinction is between: 1) full-wave, 2) quasi-static
and 3) static methods.
The methods able to solve the complete set of Maxwell equations without simplifying
assumptions are classified as full-wave methods. These methods can be applied in general.
In some conditions, essentially at low frequency, the quasi-static assumption can be used. In
these conditions, the Maxwell equations can be simplified, the fields are assumed time-
invariant / frequency-independent. The numerical approach is simplified and the calculation is
faster.
Another simple and effective classification of the suitable numerical methods can be the
following [10]:
- Circuit theory and transmission line based methods: these methods are based on
equivalent circuits with lumped or distributed elements respectively. Both methods require
a discretization of the system into electromagnetically coupling small sections. Each
section is represented with lumped or distributed resistance, inductance or capacitance
often calculated with analytical formulas. The calculation of distributed parameters is
usually related to assumption of a quasi TEM propagation. Kirchhoff laws are used to
assemble elements impedance and field sources in a single complete model. Usually
these methods can be applied in a limited frequency range
- Electromagnetic Field Differential methods: these methods solve the Maxwell equations
written in differential form in the space of interest partitioned in elements. Due to limitations
in memory, only a finite space domain is considered in simulation, and appropriate
boundary conditions are used in order to represent the space extension to infinite. These
methods could be very accurate and can consider very realistic scenarios and arbitrary
inhomogeneity of the propagation medium but usually they require considerable hardware
resources and do not allow to represent large systems as they are in reality. The most
diffused methods based on this approach are the finite difference time domain (FDTD)
method and the finite element method (FEM)
- Electromagnetic Field Integral methods: these methods solve the Maxwell equations
written in integral form. In this case, the discretization is applied not to the propagation
medium but to the surface of the field sources. This reduces significantly the problem
dimension in open space problems, the usual condition for engineering applications. The
most diffused methods based on this approach are the MoM and PEEC methods
Taking into account the difficulty with open space problems of the methods based on the
differential form of the Maxwell equations, the most interesting methods for electromagnetic
interference analysis are essentially the MoM and PEEC methods.
The PEEC method was developed after 1990 and is then more recent than the MoM, and
moreover it offers the important advantage of not requesting post process calculations to
obtain potentials rises along the conductors.
The PEEC is the method used in the commercial software considered in this document.
In some conditions and in particular at low frequencies, methods based on the circuit theory
can offer a good option to the methods based on the field theory.
This document will compare results calculated using field and circuit theory in some particular
cases.
The PEEC Method
In the following, the PEEC formulation is limited to thin structures with currents and charges
constrained along conductor axes.
The PEEC method for thin structures is based on the continuity of the tangent axial component
of the total electric field on the conductor surface.
If the conductor is real with an internal impedance per unit length zi, and the current flowing
along the conductor is I, the total electric field on his surface can have tangent components
equal to the internal voltage drop per unit length along the conductor axes and continuity
condition is:
 
i c e
E z z I E 
(32)
Outside the conductor, the electric field E is related to scalar potential U and vector potential
A resulting from charges and currents distributions along the conductor axes according to the
following general equation:
U
E j A
l
 
(33)
Combining (32) and (33), it is immediate to obtain the following general differential equation:
 
i c e
U
z z I j A E
l
 
(34)
Equation (34) is valid in full-wave conditions with the only assumption of thin wire structures.
The vector and scalar potential in a generic point of the propagation medium associated to the
current and charge or leakage current distributions along the conductor axis L can be
expressed using (16) and (18) in case of uniform medium and using Sommerfeld integrals in
the presence of a conducting half space.
In order to implement previous equations in a numerical model, the system of conductors is
preliminarily partitioned in short elements composed of current and potential (or charge) cells
(see Figure 2). The distribution of currents, leakage currents and potentials along the
conductor axis are both approximated with pulse functions. Current and potential cells are
interleaved each other. In each current cell, longitudinal current is uniform. The same, in each
potential cell, the leakage current density (or charge density) and the potential are uniform.
The current and potential values are assumed as the average values along the cell. Using
these simple discernments is possible to convert previous differential equation in a linear
system.
Figure 2 - Interleaved current and potential cells
Let us consider a generic current cell i with length li and end points i- and i+.
With the above assumptions on current distributions, the integral of (34) along the cell i can be
rewritten as follows:
si i mij j i k k i k k ei
j i k k
Z I Z I W J W J E

 
 
(35)
The meanings of previous parameters are shortly the following:
- Zs i represents the self impedance of an element, that is the sum of internal, coating and
external impedance
- Zm I,j represents the mutual inductive coupling between two elements
- Wi,i represents the self coefficient of potential of an element
- Wi,j represent the mutual conductive and capacitive coupling between two elements
The calculation of previous parameters are out of the scope of this document. Of course, the
evaluation of such parameters is crucial, as anticipated, the PEEC method is full-wave but its
application range depends on the accuracy in the calculation of its parameters.
Previous equations are related to the equivalent circuit of a PECC current cell as illustrated in
the Figure 3.
Figure 3 - Equivalent circuit of a PEEC current cell i
With the previous formulations, the Maxwell equations have been rewritten in a linear equation
where the unknowns are currents and leakage currents.
In general, the system of conductors will be fragmented in N cells also called elements or
segments. Each cell introduces two unknowns, the longitudinal current and the leakage current
in cell. The total number of unknowns is anyway 2N. In order to have a determined linear
system is then necessary to have 2N independent linear equations.
Equation (35) provides N equations. The missing N equations can be obtained by applying the
first Kirchhoff to each cell, eventually taking into account also a forced injection current Je.
For the potential cell k it follows:
0
k ek k k
I J I J

  
(36)
The 2N equations can be assembled in a complete model in a single determined linear system.
The system of conductors can be energized with voltage generators, with current generators
or with induced electromotive force or potentials due to inductive, capacitive or conductive
couplings as already seen.
At the end, the solution of the linear system gives the distribution of longitudinal current,
leakage current and potentials along the system of conductors.
With a post processing calculation is then possible to calculate the distribution of potential,
electric and magnetic fields in each point of the propagation medium.
The calculation of these quantities can be performed as superposition effects of each single
cell. This is possible if the system is linear, which is a fundamental requirement.
The PEEC approach in the frequency domain can be extended to the time domain using
Fourier direct and inverse transforms.
The PCM
Using the PEEC method, the Maxwell equations have been rewritten in a linear system of
equations where the unknowns are currents and leakage currents. A similar system of equation
can be obtained also directly by using the circuit theory. The two systems will be different, but
in some conditions, results can be substantially equivalent.
As known, the analysis of electrical networks can be done using the graphs theory and
essentially using the following two methods:
- SCM (Sequence or Symmetrical Components Method)
- PCM (Phase Components Method)
The SCM is based on the Kirchhoff laws and the Fortescue technique and in some conditions
is rigorous, in other conditions acceptable, in other conditions not applicable. Essentially, the
SCM cannot be used in case of multiple grounded systems or in case of problems that involve
currents to earth. This is typically the situation involved in electromagnetic interference
condition.
The PCM is based only in the Kirchhoff laws and is for general applications with balanced or
unbalanced systems and with symmetrical and unsymmetrical systems. The PCM works in
multi-conductor mode, so it increases the size of the linear system involved with the problem
and requires considerable memory resources and computing power.
But this is not a problem with modern computers.
In order to apply the PCM, the electrical network is divided in cells connected through buses.
A cell indicates a multi-port cell with one or more group of ports as represented in Figure 4.
Figure 4 - Generic two sides cell
A bus can be represented as a multi-port connector as indicated in Figure 5.
Figure 5 - Generic bus
If Ii and Ui indicate currents and potentials at port i, and p indicates the number of ports of the
cell, using the Kirchhoff equations inside the cell it is possible to obtain the system of equation:
U1 out, I1 out
U2 out, I2 out
Un out, In out
Un in, In in
U1 in, I1 in
U2 in, I2 in
Ie out
Ie in
 
 
 
2
p
p p p
p
I
AN
U







(37)
For all cells, if P indicates the total number of ports, the system is:
 
 
 
2
P
P P P
P
I
AN
U







(38)
The missing P equations can be calculated at the bus connections and then from the network
topology. For all cells and buses, the final system is:
 
 
 
 
2
20
P
PP P
P
PP P
I
AN
BU


 
 

 

 





(39)
The matrix of the linear system (39) is usually strongly sparse and can be stored and solved
using specific numerical routines.
With a limited number of cells (Sources, Longitudinal and Transverse Impedances, Lines,
Cables, Conductors, Transformers …) it is possible to represent any kind of network.
Again, at the end, the solution of (39) gives currents and potentials at each port. The module
used, includes a special cell (called Hybrid) where it is possible to mix cables, lines and
conductors like pipelines, railroads ... This cell has been developed also for the calculation of
electromagnetic interferences between power lines and pipelines when they lie parallel or can
be represented as series of parallel conditions using the approach in [7].
It is important to remember that the PEEC method considers the ends effects related to the
use of short conductors. The PCM is based on the assumption of a quasi TEM propagation
and uses equations based on the assumption of conductors infinite long, parallel and horizontal
and the ends effects are not taken into account.
This, together with the difference in fragmentation can imply differences in results.
Infinite Conductor Modelling
In order to represent the extension to infinite of a conductor, it is possible to use its
characteristic impedance:
0z
Zy
(40)
where:
0
Z
() = characteristic impedance
z
(/m) = self impedance
y
(S/m) = admittance to earth
If the conductor is a long pipeline, tacking into account that pipelines are usually coated, self-
impedance and transverse admittance can be calculated using the following equations:
int coat ext
z z z z 
(41)
int 22
mm
zj
d

(42)
02
ln
2c
coat dt
zj d
(43)
04 1 4
ln
2 1.78 2 3
ext e
e
z j h
d



 


(44)
0
ee
j

(45)
11
22
ln
cc
c
yj
dt
d
 




(46)
where:
2f

(rad/s) = angular frequency
int
z
(/m) = internal impedance
coat
z
(/m) = coating impedance
ext
z
(/m) = external impedance of an infinite long conductor
m
(m) = resistivity of the pipeline wall
m
(H/m) = permeability of the pipeline wall
d
(m) = pipeline outer diameter coating excluded
c
t
(m) = pipeline coating thickness
e
(1/m) = earth propagation constant
e
(m) = earth propagation resistivity
h
(m) = pipeline depth referred to the pipe axis
c
(m) = resistivity of the pipeline coating
c
(H/m) = permittivity of the pipeline coating
COMPARISON BETWEEN FIELD AND CIRCUIT BASED MODELS
The methods based on field theory are general and rigorous but also time consuming in the
modelling stage. On the other side, the methods based on the circuit theory is some case are
easier in the modelling stage but their accuracy it is not always adequate.
In the following, the comparison between these methods is limited to two cases and to final
results. i.e. the induced current and potential from a power system to a pipeline.
The first case is related to an interference scenario where power system and pipeline are
parallel (near and far). This scenario can be found in case of share corridors or in railways.
The second case is related to an interference scenario where power system and pipeline are
not parallel.
Power System and Pipeline Parallel
In this first case, power system and pipeline are considered parallel.
Power System main data:
- Rated voltage: 220 kV
- Frequency: 50 Hz
- Average span: 400 m
- Tower foot resistance to earth: 10 Ω
- Phase conductor: ACSR, diameter 31.5 mm
- Sky wire: Al, diameter 11.5 mm
- Single phase to earth current: 10 kA
Pipeline main data:
- Outer diameter: 300 mm
- Wall: Steel, thickness 9.5 mm
- Covering: PE 20 years, thickness 2.5 mm
- Axis depth: 1 m
- Characteristic impedance: 0.964 + j 0.751
Other data:
- Interference length: 10 km
- Horizontal distance from tower and pipeline axes: 20 m
- Soil resistivity: 100 Ωm
- Layout: see Figure 6
Figure 6 Power system and pipeline
In following figures the distribution of induced current and potential calculated with field and
circuit theory respectively.
Figure 7 Induced current distribution on pipeline - Field theory 20 m
Figure 8 Induced current distribution on pipeline - Circuit theory 20 m
Figure 9 Induced potential distribution on pipeline - Field theory 20 m
Figure 10 Induced potential distribution on pipeline - Circuit theory 20 m
The agreement between results calculated using field and circuit theory is excellent.
The only visible differences are related to the induced potential distribution at the pipeline ends.
This can be related to the end effects and it was expected.
In following figures the same results but with an horizontal distance from tower and pipeline
axes 500 m.
Figure 11 Induced current distribution on pipeline - Field theory 500 m
Figure 12 Induced current distribution on pipeline - Circuit theory 500 m
Figure 13 Induced potential distribution on pipeline - Field theory 500 m
Figure 14 Induced potential distribution on pipeline - Circuit theory 500 m
The agreement between results calculated using field and circuit theory is now good but not
excellent.
The differences related to the end effects are now more evident.
In general, these differences grow with the ratio between interference distance and length.
In such conditions the equations used in the circuit theory approach, based on infinite long and
parallel conductors gradually lose their validity.
Power System and Pipeline Not Parallel
In this second case, power system and pipeline are not parallel.
Power system and pipeline main data are as in previous case.
Other data as in previous case and moreover:
- Power System length: 10 km
- Power System route: straight, see Figure 15
- Pipeline length: 11.2 km
- Pipeline route: see Figure 15
The maximum distance between power system and pipeline in Figure 15 is at the starting
point and is 2927 m.
Figure 15 Power system and pipeline
The interference scenario in Figure 15 is reduced to a series of parallel sections by partitioning
power system and pipeline using the rules in [7] Appendix C 1.2.
In each section, the number of spans “n” is set as:
l
n round s



(47)
where:
l (m) = section length
s (m) = span length
This assumption introduces unavoidable approximations in results.
Another problem in the application of the circuit theory approach is the definition of a reference
length. Each section is reduced to an equivalent parallel section with an equivalent distance
and the reference length related to the power line. This means information along pipeline can
be evaluated only as orthogonal projection to the related power line. This is evident in the
following figures, where pipeline length is 11.2 km using field theory (the true length) and 10
km using circuit theory (the projection on the power line).
Finally, in the specific case, the time in the modelling stage is similar for field and circuit theory.
In following figures, the distribution of induced current and potential calculated with field and
circuit theory respectively.
Figure 16 Induced current distribution on pipeline - Field theory
Figure 17 Induced current distribution on pipeline - Circuit theory
Figure 18 Induced potential distribution on pipeline - Field theory
Figure 19 Induced potential distribution on pipeline - Circuit theory
The agreement between results calculated using field and circuit theory is acceptable only for
a preliminary calculation.
The difference in peak values is about 8% in current and 15% in potential.
These differences are related mainly to the following reasons:
- The division of the interference scenario in sections
- The method used for the reduction of sections to equivalent parallel sections
- The different used equations (Sommerfeld Vs. Carson)
- The end effects
CONCLUSIONS
This document describes the reference theory and two numerical models suitable for
simulation of electromagnetic interferences between power lines and pipelines:
- The model based on the field theory and in particular on the PEEC method
- The model based on the circuit theory and in particular on the PCM method
The models based on field theory are general and rigorous and can be applied in all conditions
but are usually time consuming in the modelling stage. These models are irreplaceable in case
of complex 3D scenarios.
The models based on circuit theory approach are easier in the modelling stage, but only in
case of simple scenarios, for instance in parallel or quasi parallel conditions. In case of complex
scenarios, the time spent in the modelling stage is similar to the time spent with a field theory
approach.
The accuracy of the models based on circuit theory is good only in case of parallel or quasi
parallel conditions. In such cases the accuracy is good in case of small ratio between
interference distance and interference length. A ratio 1/50 for each single parallel or quasi
parallel section can be used as reference value.
In case of complex 3D scenarios, the circuit theory is in general suitable only for preliminary
evaluations.
REFERENCES
[1] Banos A. (1966) Dipole Radiation in the Presence of a Conducting Half Space,
Pergamon Press, Oxford
[2] Sunde, E.D. (1968) Earth Conduction Effects in Transmission Systems, McMillan, New
York
[3] Harrington, R.F. (1968) Field Computation by Moment Methods, Macmillan, New York
[4] Tagg, G.F. (1964) Earth Resistance, Pitman, New York.
[5] P. R. Bannister and R. L. Dube, “Simple expressions for horizontal electric dipole quasi-
static range subsurface-to-subsurface and subsurface-to-air propagation,” Radio
Science, vol. 13, no. 3, pp. 501-507, 1978.
[6] Wait J.R. (1985) Electromagnetic Wave Theory, Harper & Row Publisher, New York
[7] CIGRE WG36.02 95/1995 “Guide on the Influence of High Voltage AC Power Systems
on Metallic Pipelines”;
[8] IEC 60479-1/2/5: 2005/2007/2007; Effects of current on human beings and livestock
[9] EN 50522:2010-11; “Earthing for power installation exceeding 1 kV a.c.”
[10] CIGRE CG.501 June 2013 “Guideline for Numerical Electromagnetic Analysis Method
and its Application to Surge Phenomena”
[11] IEEE (2013) IEEE Standard 80-2013. Guide for Safety in AC Substation Grounding
[12] CIGRE TB 781 October 2019 “Impact of soil-parameter frequency dependence on the
response of grounding electrodes and on the lightning performance of electrical systems”
[13] XGSLab rel. 10.0.1 User’s Guide - SINT Srl Italy
[14] XGSLab rel. 10.0.1 Tutorials - SINT Srl Italy
Article
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The functionality of buried metallic pipelines can be compromised by the electrical lines that share the same right-of-way. Given the considerable size of shared corridors, computer simulation is an important tool for performing risk assessment and mitigation design. In this work, we introduce an open-source computational framework for the analysis of electromagnetic interference on large earth-return structures. The developed framework is based on FLARE—an efficient finite element solver developed by the authors in MATLAB®. FLARE includes solvers for problems involving static electric and magnetic fields, and DC and time-harmonic AC currents. Quasi-magnetostatic transient problems can be studied through time-marching or—for linear problems—with an efficient inverse-Laplace approach. In this work, we succinctly describe the optimization of time-critical operations in FLARE, as well as the implementation of a transient solver with automatic time-stepping. We validate the numerical results obtained with FLARE via a comparison with the commercial software COMSOL Multiphysics®. We then use the validated time-marching analysis results to test the accuracy and efficiency of three numerical inverse-Laplace algorithms. The test problem considered is the assessment of the inductive coupling between a 500 kV transmission line and a metallic pipeline buried in the soil.
Article
Contains table of contents for Section 3 and reports on five research projects.
Article
Simple engineering expressions for the quasi-static fields produced by a subsurface horizontal-electric-dipole (HED) antenna have been derived by employing finitely conducting earth-image theory techniques. Both subsurface-to-subsurface and subsurface-to-air propagation cases are considered. It is shown that the resulting subsurface-to-air propagation field-strength expressions are the result of simple modifications to the previously derived quasi-static range air-to-air propagation equations of one of the authors.
Dipole Radiation in the Presence of a Conducting Half Space
  • A Banos
Banos A. (1966) Dipole Radiation in the Presence of a Conducting Half Space, Pergamon Press, Oxford
Earth Conduction Effects in Transmission Systems
  • E D Sunde
Sunde, E.D. (1968) Earth Conduction Effects in Transmission Systems, McMillan, New York
Guideline for Numerical Electromagnetic Analysis Method and its Application to Surge Phenomena
  • Cigre Cg
CIGRE CG.501 June 2013 "Guideline for Numerical Electromagnetic Analysis Method and its Application to Surge Phenomena"
IEEE Standard 80-2013. Guide for Safety in AC Substation Grounding
IEEE (2013) IEEE Standard 80-2013. Guide for Safety in AC Substation Grounding