- Source: Magnetic current
Magnetic current is, nominally, a current composed of moving magnetic monopoles. It has the unit volt. The usual symbol for magnetic current is
k
{\displaystyle k}
, which is analogous to
i
{\displaystyle i}
for electric current. Magnetic currents produce an electric field analogously to the production of a magnetic field by electric currents. Magnetic current density, which has the unit V/m2 (volt per square meter), is usually represented by the symbols
M
t
{\displaystyle {\mathfrak {M}}^{\text{t}}}
and
M
i
{\displaystyle {\mathfrak {M}}^{\text{i}}}
. The superscripts indicate total and impressed magnetic current density. The impressed currents are the energy sources. In many useful cases, a distribution of electric charge can be mathematically replaced by an equivalent distribution of magnetic current. This artifice can be used to simplify some electromagnetic field problems. It is possible to use both electric current densities and magnetic current densities in the same analysis.: 138
The direction of the electric field produced by magnetic currents is determined by the left-hand rule (opposite direction as determined by the right-hand rule) as evidenced by the negative sign in the equation
∇
×
E
=
−
M
t
.
{\displaystyle \nabla \times {\mathcal {E}}=-{\mathfrak {M}}^{\text{t}}.}
Magnetic displacement current
Magnetic displacement current or more properly the magnetic displacement current density is the familiar term ∂B/∂t It is one component of
M
t
{\displaystyle {\mathfrak {M}}^{\text{t}}}
.
M
t
=
∂
B
∂
t
+
M
i
.
{\displaystyle {\mathfrak {M}}^{\text{t}}={\frac {\partial B}{\partial t}}+{\mathfrak {M}}^{\text{i}}.}
where
M
t
{\displaystyle {\mathfrak {M}}^{\text{t}}}
is the total magnetic current.
M
i
{\displaystyle {\mathfrak {M}}^{\text{i}}}
is the impressed magnetic current (energy source).
Electric vector potential
The electric vector potential, F, is computed from the magnetic current density,
M
i
{\displaystyle {\mathfrak {M}}^{\text{i}}}
, in the same way that the magnetic vector potential, A, is computed from the electric current density.: 100 : 138 : 468 Examples of use include finite diameter wire antennas and transformers.
magnetic vector potential:
A
(
r
,
t
)
=
μ
0
4
π
∫
Ω
J
(
r
′
,
t
′
)
|
r
−
r
′
|
d
3
r
′
.
{\displaystyle \mathbf {A} (\mathbf {r} ,t)={\frac {\mu _{0}}{4\pi }}\int _{\Omega }{\frac {\mathbf {J} (\mathbf {r} ',t')}{|\mathbf {r} -\mathbf {r} '|}}\,\mathrm {d} ^{3}\mathbf {r} '\,.}
electric vector potential:
F
(
r
,
t
)
=
ε
0
4
π
∫
Ω
M
i
(
r
′
,
t
′
)
|
r
−
r
′
|
d
3
r
′
,
{\displaystyle \mathbf {F} (\mathbf {r} ,t)={\frac {\varepsilon _{0}}{4\pi }}\int _{\Omega }{\frac {{\mathfrak {M}}^{\text{i}}(\mathbf {r} ',t')}{|\mathbf {r} -\mathbf {r} '|}}\,\mathrm {d} ^{3}\mathbf {r} '\,,}
where F at point
r
{\displaystyle \mathbf {r} }
and time
t
{\displaystyle t}
is calculated from magnetic currents at distant position
r
′
{\displaystyle \mathbf {r} '}
at an earlier time
t
′
{\displaystyle t'}
. The location
r
′
{\displaystyle \mathbf {r} '}
is a source point within volume Ω that contains the magnetic current distribution. The integration variable,
d
3
r
′
{\displaystyle \mathrm {d} ^{3}\mathbf {r} '}
, is a volume element around position
r
′
{\displaystyle \mathbf {r} '}
. The earlier time
t
′
{\displaystyle t'}
is called the retarded time, and calculated as
t
′
=
t
−
|
r
−
r
′
|
c
.
{\displaystyle t'=t-{\frac {|\mathbf {r} -\mathbf {r} '|}{c}}.}
Retarded time accounts for the accounts for the time required for electromagnetic effects to propagate from point
r
′
{\displaystyle \mathbf {r} '}
to point
r
{\displaystyle \mathbf {r} }
.
= Phasor form
=When all the functions of time are sinusoids of the same frequency, the time domain equation can be replaced with a frequency domain equation. Retarded time is replaced with a phase term.
F
(
r
)
=
ε
0
4
π
∫
Ω
M
i
(
r
)
e
−
j
k
|
r
−
r
′
|
|
r
−
r
′
|
d
3
r
′
,
{\displaystyle \mathbf {F} (\mathbf {r} )={\frac {\varepsilon _{0}}{4\pi }}\int _{\Omega }{\frac {{\mathfrak {M}}^{\text{i}}(\mathbf {r} )e^{-jk|\mathbf {r} -\mathbf {r} '|}}{|\mathbf {r} -\mathbf {r} '|}}\,\mathrm {d} ^{3}\mathbf {r} '\,,}
where
F
{\displaystyle \mathbf {F} }
and
M
i
{\displaystyle {\mathfrak {M}}^{\text{i}}}
are phasor quantities and
k
{\displaystyle k}
is the wave number.
Magnetic frill generator
A distribution of magnetic current, commonly called a magnetic frill generator, may be used to replace the driving source and feed line in the analysis of a finite diameter dipole antenna.: 447–450 The voltage source and feed line impedance are subsumed into the magnetic current density. In this case, the magnetic current density is concentrated in a two dimensional surface so the units of
M
i
{\displaystyle {\mathfrak {M}}^{\text{i}}}
are volts per meter.
The inner radius of the frill is the same as the radius of the dipole. The outer radius is chosen so that
Z
L
=
Z
0
ln
(
b
a
)
,
{\displaystyle Z_{\text{L}}=Z_{0}\ln \left({\frac {b}{a}}\right),}
where
Z
L
{\displaystyle Z_{\text{L}}}
= impedance of the feed transmission line (not shown).
Z
0
{\displaystyle Z_{0}}
= impedance of free space.
The equation is the same as the equation for the impedance of a coaxial cable. However, a coaxial cable feed line is not assumed and not required.
The amplitude of the magnetic current density phasor is given by:
M
i
=
k
ρ
{\displaystyle {\mathfrak {M}}^{\text{i}}={\frac {k}{\rho }}}
with
a
≤
ρ
≤
b
.
{\displaystyle a\leq \rho \leq b.}
where
ρ
{\displaystyle \rho }
= radial distance from the axis.
k
=
V
s
ln
(
b
a
)
{\displaystyle k={\frac {V_{\text{s}}}{\ln \left({\frac {b}{a}}\right)}}}
.
V
s
{\displaystyle V_{\text{s}}}
= magnitude of the source voltage phasor driving the feed line.
See also
Surface equivalence principle
Notes
References
Kata Kunci Pencarian:
- Resonansi magnet inti
- Senyawa siklik
- Kastel Koral
- Aurora
- Motor listrik
- Elektromagnetisme
- Magnet superkonduktor
- Tata Surya
- Skizofrenia
- Posisi misionaris
- Magnetic current
- Eddy current
- Electric current
- Magnetization
- Magnetic moment
- Magnetic monopole
- Biot–Savart law
- Magnetic field
- Dipole
- Earth's magnetic field
