UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
LECTURE NOTES 16
THE MAGNETIC VECTOR POTENTIAL Ar
We saw in electrostatics that E 0 {always} (due to intrinsic / microscopic nature of the electrostatic field) permitted us to introduce a scalar potential Vr such that: Er Vr {n.b. Vr is uniquely defined, up to an (arbitrary) constant.}
Analogously, in magnetostatics, the Br 0 (always) {no magnetic charges / no magnetic monopoles} permits us to introduce a magnetic vector potential Ar such that:
B rAr S.I. units of the magnetic vector potential Ar = Tesla-meters Teslas 1 m Tesla- Meters
Then: Br Ar 0 {always} The divergence of a curl of a vector field Fr is always zero
Ampere’s Law: 2 In differential form: BrArArArJr o free Now, just as in the case of electrostatics, where Vr was uniquely defined up to an arbitrary constant Vo , then let: Vr Vr Vo 0 then: Er V r Vr Voo Vr V Vr i.e. Er V r Vr
An analogous thing occurs in magnetostatics - we can add / we have the freedom to add to the magnetic vector potential Ar the gradient of any scalar function rrm where 2 m r magnetic scalar potential SI Units of magnetic scalar potential m r Tesla-m
Then: Ar Ar r Ar m r Formally known as a Gauge Transformation
The curl of the gradient of a scalar field (m r here) automatically/always vanishes, i.e.: 0Always !!! BrArArrArrArr m Ar
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 1 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede Note that the magnetic scalar potential m r has same physical units as magnetic flux m : Tesla-m2 = Weber (Magnetic flux, BrdA !!) eeek!!!! m S
Please do NOT confuse the magnetic scalar potential m r (= a scalar point function, whose value can change at each/every point in space, r ) with the magnetic fluxm (which is a constant scalar quantity (i.e. a pure number), independent of position) mmr !!!
Thus, like the scalar potential Vr, the magnetic vector potential Ar is (also) uniquely defined, but only up to an (arbitrary) vector function rrm .
Ar Ar r Ar m r
The definition BrAr specifies the curl of Ar, but in order to fully specify the vector field Ar, we additionally need to specify the divergence of Ar, Ar.
We can exploit the freedom of the definition of Ar to eliminate the divergence of Ar - i.e. a specific choice of Ar will make Ar divergenceless: Ar 0 Coulomb Gauge
If: Ar Ar r Ar m r 2 Then: A r Ar r Ar mm r Ar r
While the original magnetic vector potential, Aris not/may not be divergenceless, we can make Ar Ar r Ar m r divergenceless, i.e. Ar 0 if we chose 2 rrm such that rrArm Coulomb Gauge
A Simple Illustrative Example: Suppose a region of space that has a uniform/constant magnetic field, e.g. BrBz o ˆ . Ary Arx Then: BrBzAro ˆˆ z. xy Thus (here): Ar A r xˆˆ A r y A r zArxAryˆ ˆˆ xy z xy 0 1 1 11 If Ax rBy o and AyorBx , then Ar Byxˆˆ Bxy, and thus we see that this 2 2 22oo choice of magnetic vector potential indeed gives us the correct B -field: Ar y Arx 11 BrAr zBBBzˆˆ 22ooo xy
2 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
1 1 A Ay A By Bx 0 Is A 0 satisfied? A x z 2 o 2 o 0 Yes!!! xyz x y z Note that we could also have instead chosen/used a different magnetic vector potential: Ar Ar r Ar m rwhere e.g. rrAmo , i.e. where Ao is any (arbitrary) constant vector, AAxAyAzooxoyozˆˆˆ . Since (here) rrAmo , then rrAAxAyAzm o oxˆˆ oy oz ˆ means that the gradient of the magnetic scalar
Ax Ayoy Az potential (here) is:rxyzAxAyAzAr oxˆˆ oz ˆˆ ˆˆ moxoyozoxyz and thus the magnetic scalar potential itself (here) is: moxoyozrAxxAyyAzzˆˆ ˆ .
Thus, here for the case of a constant/uniform magnetic field BrBz o ˆ we see that there is in fact a continuum of allowed magnetic vector potentials Ar Ar Aom Ar r that simultaneously satisfy BrBzArˆ and Ar 0 with the addition of an o (arbitrary) constant magnetic vector potential AAxAyAzooxoyozˆˆˆ contribution with corresponding magnetic scalar potential moxoyozrAxxAyyAzzˆˆ ˆ . Note that this is exactly analogous to the situation in electrostatics where the scalar electric potential Vris unique, up to an arbitrary constant, Vo because there exists no absolute voltage reference in our universe – i.e. absolute measurements of the scalar electric potential are meaningless - only potential differences have physical significance!!!
We used this simple example of the constant/uniform magnetic field BrBz o ˆ to elucidate this particular aspect of the magnetic vector potential Ar. Here in this particular example, we found that the addition of an arbitrary constant vector rAAxAyAzooxoyozmˆˆ ˆ rto the magnetic vector potential Ar was allowed, i.e. Ar Ar r Ar Ao , which leaves the magnetic field Br unchanged. In general there are many instances involving more complicated physics situations, where Br constant vector field, where indeed BrAr and Ar 0 are simultaneously satisfied for Ar Ar r, because it is possible to determine/find a 2 corresponding magnetic scalar potential m r for the problem satisfyingm rAr , but it is (very) important to understand that, in general, the allowed rrm (very likely) may not be simply a constant vector field, but indeed one which varies in space (i.e. with position vector, r )! Here again, however, the new Ar Ar rwill also be such that BrAr will be unchanged, exactly analogous to Vr Vr Vo leaving Er V runchanged.
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 3 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede 2 So we see that if m rAr then yes, Ar 0 .
It is always possible to find an rrm in order to make Ar 0 .
Note however that this situation is then formally mathematically identical to Poisson’s Equation, for the magnetic scalar potential m r because: 2 2 Tot r mmrr Analogous to Vr in electrostatics!!! 0 Equivalent magnetic Physically, m r could e.g. be due to bound effective volume charge densit y magnetic charges associated with a magnetic material… If we assume that the equivalent magnetic volume charge density, m r 0 and we want Ar 0 2 Then: Ar r Ar m r 0 Or: Arm r 0 Arm r
Then, the solution to Poisson’s equation for the magnetic scalar potential m r is of the form: 1 r 1 r rdm Analogous to Vr Tot d in electrostatics m v v 4 r 4 0 r with rrr
(n.b. these two relations are both valid assuming that m rr and ToT vanish when r !)
So then if m rAr , and m rAr vanishes as r , then the magnetic scalar potential m r is given by:
11 rAr rdm d m 44vvrr
{Note that if Arm r does not go to zero at infinity, then we’ll have to use some other means in order to obtain an appropriate m r , e.g. in an analogous manner to that which we’ve had to do for the (electric) scalar potential Vrassociated with problems that have electric charge distributions extending out to infinity.}
Thus, this choice of m r ensures that indeed we can always make the magnetic vector potential Ardivergenceless, i.e. the conditionAr 0 (Coulomb Gauge) can always be met, for the case of magnetostatics. Note that if m r 0 then m rAr 0 .
4 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
With the choice of the magnetic scalar potential: 1 r rdm and Ar Ar A Ar r, and Ar 0 m 4 v r om
Then Ampere’s Law (in differential form) becomes:
B rArArArJr 2 0 free 0 2 Which gives: Ar0 Jfree r Vector form of Poisson’s equation for magnetostatics.
2 Arxoxfree J r The three separate/independent scalar forms 2 i.e.: Aryoyfree J r of Poisson's equation are connected by: 2 JrJ rxJryJrzˆˆ ˆ Arzozfree J r free x free y free z free
22 2 2 n.b. in Cartesian coordinates: Ar Arxyz xˆˆ A r y Ar zˆ
However, in curvilinear coordinates (i.e. spherical-polar or cylindrical coordinates)
rxyzˆˆˆsin cos sin sin cos ˆ e.g. spherical-polar coordinates: ˆ cos cosxˆˆ cos sinyz sin ˆ ˆ ˆˆ sinxy cos
Note that the unit vectors rˆ,ˆ ˆ for spherical-polar coordinates are in fact explicit functions of the vector position, r i.e. rrrˆˆ, ˆˆ r and ˆˆ r and therefore rˆ,ˆ ˆ must also be explicitly differentiated in calculating the Laplacian 2 of a vector function (here, Ar) in curvilinear (i.e. either spherical-polar and/or cylindrical) coordinates!!! This is extremely important to keep in mind, for the future…
The safest way to calculate the Laplacian of a vector function 2 Ar in terms of curvilinear coordinates, is to NOT use curvilinear coordinates!!! Failing that, then one should use:
2 Ar Ar Ar Ar 0 in the Coulomb Gauge If m r 0 then (automatically) m rAr 0 and we can use Ardirectly. 2 Hence, if Ar0 Jfree r (vector Poisson equation for magnetostatics), Jrfree then if Jr 0 as r , then Ar 0 d where rr rr free 4 v r
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 5 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Generalizing this for a moving point charge as well as for line, surface and volume current densities (with BrAr ), we summarize these results in the following table:
vr vr rˆ Ar o q Br o q 4 free r 4 free r 2 Ir ˆ o free Irdfree r Ar d Br o C C 2 4 r 4 r o d dr rˆ I o free C 4 r I free 4 C r 2 Kr ˆ 0 free Krfree r Ar da B rda o S 2 4 r 4 S r Jr ˆ o free Jrfree r Ar d B rd o v 2 4 r 4 v r
Note that:AvIdKJ , , , , i.e. A is always parallel to the direction of motion of current, with relative velocityv , whereas B AvIdKJ ,, , , .
Note also that B and A both vanish when v 0 (e.g. in the rest frame of a current (e.g. a proton or an electron beam)).
A Tale of Two Reference Frames:
For a pure point electric charge/point electric monopole moment, q we know that if it is moving in the lab frame with speed v << c {c = speed of light in vacuum} that the magnetic field Bq r observed in the lab frame is:
1 q rrˆˆo Brqq Ar 2222 vEr q v qv cc440 rr
Thus in the lab frame where this charged particle is moving, the magnetic vector potential Arq associated with this moving charged particle (as observed in the lab frame) has a non-zero curl.
Contrast this with the situation in the rest frame of this pure point electric charge particle, where the magnetic field vanishes, i.e. the magnetic vector potential Arq associated with this charged particle has no curl!!!
1 Vrt, We will find out (next semester, in P436) that: Art, in electrodynamics. ct2 connection between the Art , field and electric scalar potential V rt , - they are in fact the 3 spatial & 1 temporal components of the relativistic 4-potential in electrodynamics !!!
6 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede Uses of the Magnetic Scalar Potential m r :
In certain (limited) circumstances for magnetostatics, it is actually possible to have the magnetic field Br directly related to the (negative) gradient of a magnetic scalar potential m r , i.e. Brrom , in direct analogy to that for electrostatics Er Vr . 2 2 However, whileBrom r om r 0 is satisfied, i.e. m r 0 is Laplace’s equation for the magnetic scalar potential,m r (n.b. implying that m r 0 ), Ampere’s law B rrJr is not satisfied/is violated (!!!) unless omo 0Always !!! Jr 0 everywhere in the region(s) of interest. These current-free regions must also be simply- connected. {A region D (e.g. in a plane) is connected if any two points in the region can be connected by a piecewise smooth curve lying entirely within D. A region D is a simply connected region if every closed curve in D encloses only points that are in D.}
The use of Brrm is in fact helpful for determining the magnetic fields associated with e.g. current-carrying filamentary wires, current loops/magnetic dipoles, and e.g. the magnetic fields associated with magnetized materials/magnetized objects.
The SI Units of the magnetic vector potential A are Tesla-meters (= magnetic field strength per unit length), which is also equal to Newtons/Ampere (force per unit current) = kg-meter/Ampere-sec2 = kg-meter/Coulomb-sec = (kg-meter/sec)/Coulomb = momentum per unit charge, since (kg-meter/sec) are the physical units associated with momentum p ""mv . Thus, for the A -field: force momentum 1 Tesla-meter = 1 unit of = 1 unit of Ampere of current Coulomb of charge and for the B -field, from BrAr : forceN momentum 1 Tesla = 1 unit of meter meter Ampere of currentAm Coulomb of charge Physically, the A -field has units of force per Ampere of current (or momentum per Coulomb of electric charge), and thus physically, the magnetic field BrAr is the curl of the force per unit current (or momentum per unit charge) field. Note also that force, F dP dt and current, I dQ dt such that the magnetic vector potential A physically also has units of ForceFdpdtdpdt / / p and thus B is the curl of this physical quantity. CurrentIdqdt / dq/ dt q
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 7 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
The Magnetic Vector Potential of a Long Straight Wire Carrying a Steady Current
For a filamentary wire carrying steady current I, the magnetic vector potential and magnetic field d rˆ o d o are: Ar I and Br Ar I 2 4 C r 4 C r Let the length of wire = 2L, and I Izˆ and thus ddzdzzˆˆ
r r rr R22
The infinitesimal magnetic vector potential, dA r Ryˆ due to the current-carrying line segment d carrying current I is: oodr dr dA r Ryˆ I I 44r R22
The corresponding infinitesimal magnetic field increment is: oodr dzzˆ dB r Ryˆˆ dA r Ry I I 44r R22 zL dzzˆ L d Ar Ryˆˆ dAr Ryoo I 2 CzL 22 0 22 44RR Now: L oo22 22 2I lnRzˆ 2 ILRLR ln ln 440
More generally, for a distance R away from a long straight wire of length 2L carrying a steady current I: L 2 Ar Ryˆ 2ln11o I R zˆ L 4 R
o 2L If L >> R, then: Ar Ryˆ 2ln I zˆ {Since 11 for 1.} 4 R
Note that if L → ∞ (or R → 0), then Ar Ryˆ diverges (logarithmically)! This is OK (unphysical anyway!) because even if A → ∞, BA !!! (necessarily!!!)
8 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
So, for a distance R away from a long straight wire of length 2L carrying a steady current I:
L 2 A r Ryˆˆ2ln11o I R zˆˆ A r Ry z L z 4 R
Then BrAr Let’s do this in cylindrical coordinates: (note: x22yR here):
0 0 0 0 0 1 Az A A Az 1 A Az BR ˆ ˆ A zˆ ˆ z z R R R R
ˆˆzˆ In Cylindrical Coordinates: 1 A Or: BR0 z ˆ zˆ Rz R 00A z R
yˆ B 0 1 Az Az ˆ Thus: B R ˆˆ R RR B 0 ˆ z xˆ
Az o 22 Then: BR ˆˆ R 2lnln I LLRR 4 R
Now if: UR L L22 R 1 dU R R Then: ln UR RURdRLLR22 LR 22 dU R R 1 Since: and: ln R dR LR22 R R
B-field associated with filamentary o R 1 Then finally: BR I ˆ wire of length 2L 2 22R L2 111RR carrying steady LL current I. o I Note that as L → ∞, then BR ˆ i.e. exactly the same as we obtained for 2 R ∞-long straight filamentary wire carrying steady current I (see previous P435 Lecture Notes)!!!
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 9 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
The Magnetic Vector Potential Ar and Magnetic Field BrAr Associated with
a Pair of Long, Parallel Wires Carrying Steady Currents I1 Izˆ and I2 Izˆ , Separated by a Perpendicular Separation Distance, d
Plane to wires and containing separation distance d
ddzdzz1 ˆˆ r 111rrrr 1 ddzdzz2 ˆˆ r 222rrrr 2 rrr12
For simplicity’s sake, assume L >> R1, R2.
o 2L o 2L Then: AR11 Iln zˆ and AR22 Iln zˆ 2 R1 2 R1
Then, using the principle of linear superposition: oo22LL ArArArIzIzTOT 12 lnˆˆ ln 22RR12 2 ooRR22 Or: ArTOT Iln zˆˆ I ln z for L >> R1, R2. 24RR11
10 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Now let us re-locate the local origin to be at the LHS wire, where it intersects the -plane:
Top View
I1 (out of page) d I2 (into page) 222 y d-y R1 xy 22 22 R1 x R2 R2 xdy
2 2 2 ooR2 xdy Then: ArTOT Iln zˆˆ I ln z for L >> R1, R2. 44Rxy 22 1
AyTOT 0 diverges (x = 0) Ar Ayd 0 for I IIz ˆ TOT TOT 2 12
(for x = 0 i.e. observation point on yˆ -axis) y = 0 y = d/2 y = d y
AydTOT diverges (x = 0)
Note that AAz ˆ i.e. AATOT TOT 0 (since currents only in zˆ -direction) !!! TOT z xy Note also that AAzTOT z ˆ changes sign – its direction is parallel to the closest current!!!
Then: BTOTrAr TOT , in Cartesian xˆˆyzˆ coordinates:
TOT TOT Az o dy y 222 BIx 22 R1 xy y 2 RR21 TOT TOT Az o x x 22 22 BIy 22 R2 xdy x 2 RR21 TOT Bz 0
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 11 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
At the point x = 0 and y = d/2 (i.e. at the center point, midway between the two conductors): {where R1 = R2 = R = d/2}:
dd 2 TOT 11 4 2 I BIooo22 I I o x 22 22dd dd 2 dd 22 22 TOT By 0 TOT Bz 0 Top View: d 2o I BTOT xy0, , z 0 xˆ 2 d
The Magnetic Vector Potential Ar and Magnetic Field BrAr Associated with a Magnetic Dipole Loop (For Large Source-Observer Separation Distances)
For simplicity’s sake, let us choose the observation / field point Pr to lie in the x-z plane:
Observation / field Point Pr Px ,0, z Magnetic Dipole Loop has radius R
R r
I Iˆ
12 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
dRd ˆ cos rrˆˆ = opening angle between rˆ and rˆ rr rr rr dRd cos where: rrR rr rr rR {from the arc length formula “ SR ”}
ooIdr dr Now: Ar I 44CCrr
Ar (here) is a function of xˆˆ and y only (actually only ˆ ) and not zˆ since IdId lies in the x-y plane and I Iˆ (here). Since we evaluate A in the x-z plane, the only component of d that will contribute to A (there) will be in the yˆ direction (n.b. A is parallel to the closest current from the observation point P(r)).
We only want the component of dr along the yˆ -axis, dr cos (Note: If we wanted to evaluate A e.g. in the y-z plane, then we would want only the component of dr along the xˆ -axis, dr sin )
2 o Rdcos Then: Ar Ax ,0, z Iˆˆ yˆ in the x-z plane for rxz ,0, . 4 0 r Now: r 22rR 2 2cos rR (from the Law of Cosines) and r rr
1 2 rRrR2 212 RR And: 122 cos 1 cos if R r , r and r r . rrr2 rr And: r r rrcos xxˆˆˆ zzˆ R cos x R sin y xR cos (if the observation / field point Pr Px ,0, z lies in the x-z plane) rRxR1cos2 Thus: 1 2 for r >> R and rrr r r 2 rr 2 IRxR2 1 Then: Ar Ax ,0, z o R cos 1 cos d yˆ 0 2 42 rrr IR 2 o ˆ Or: Ar Ax ,0, z 3 xy for r >> R and rrr r 4 r
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 13 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
But notice that in the x-z plane: zˆ Pr Px ,0, z x sin r r z
xˆ x yˆ out of page
IR 2 o ˆ Ar Ax ,0, z 2 sin y for r >> R and rrr r 4 r But in the x-z plane, ˆ yˆ , and since the direction of Aris always parallel to the current:
IR 2 o ˆ Ar 2 sin for r >> R and rrr r {n.b. Ar I ˆ } 4 r The magnetic dipole moment associated with this current-carrying loop is mmz ˆ mIaIazˆ (for this planar loop) where (here): aRz 2 ˆ (by the right-hand rule) mIRz 2 ˆ and: mmIaIR22 RI Note that: zrˆˆˆcos r sinˆˆ r ˆ sin r ˆ sin ˆˆ sin Thus, the quantity: mrˆˆ IazrIRˆˆ 22 zr ˆ IRsin ˆ
oomrˆ mr Ar 23 for r >> R and rrr r 44rr
Now BrAr in spherical coordinates for the magnetic dipole (with magnetic dipole moment mIaIRz 2 ˆ ) is:
o 2m Brr 3 cos 4 r
o m Br 3 sin valid for r >> R and rrr r 4 r Br 0 BrBrrBrBrr ˆ ˆ
m Bro 2cos rˆ sinˆ mIaIRz 2 ˆ Thus: 3 for r >> R and rrr r and . 4 r cf w/ the E -field associated with a physical electric dipole with dipole moment p qd : 1 p Er2cos rˆ sinˆ p qd 3 for r >> d and rrr r and . 4 o r
14 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
We already know what this Br looks like it – it is “solenoidal” around the current loop:
Cross-Sectional View of a Magnetic Dipole Loop:
2 mr mIaIRz ˆ o Thus if = a constant vector, Ar 3 for r >> R and rrr r 4 r mr o Br Ar 3 for r >> R and rrr r 4 r rr r Bro m m 0 3 3 3 4 r r r 0
rrmxˆ rm33mr r mrˆˆ r m e.g. mmxx 3 m xx33 533 5 3 x rr r rr r r 2 rrrr33333 3 r 33 and: 33 r 53 5 3 5 3 3 0 rr rr r r r r r
Magnetic Field oomr 3mr ˆˆ r m Br Ar 33 of a Magnetic 44rr Dipole Loop for r >> R (far away) and rrr r
The magnetic field of a distant circuit (r >> R) does not depend on its detailed geometry, but only its magnetic dipole moment, m !!! Important (conceptual) result!!!
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 15 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Compare this result for Br for the magnetic dipole loop, with magnetic dipole moment mIa , with result for the electric dipole field Er associated with a physical electric dipole moment p qd :
o 3mrˆˆ r m Br 3 mIa , for rR (far away) and rrr r 4 r 1 3prrˆˆ p Er 3 p qd , for rd (far away) and rrr r 4 o r +q When r ≈ R (or less) for magnetic dipole loop Or r ≈ d (or less) for electric dipole, then will be able to “see” / observe / detect higher- d p qd order moments - e.g. quadrupole, octupole, sextupole, etc. . .moments of the BE fields. −q
The statement that the magnetic field of a distant circuit (r >> R) does not depend on its detailed geometry, but only its magnetic dipole moment, mIa (n.b. this is also true for the electrostatic case, with p qd ) are very useful!!!
If one can compute mIa then one can obtain Ar and hence BrAr (or if have p qd then can obtain Er) for r >> R (or d) and rrr r . EASY!!!
Magnetic Flux Conservation
If BrAr then Br Ar 0 is automatically satisfied everywhere r If Br 0 for each/every point, r in a volume v bounded by its surface S Then: Br d B r ndAˆ (by the Divergence Theorem) vS What is Br ndAˆ ?? B r ndAˆ 0 S S Recall Gauss’ Law for E (and/or D ) were: D ndAˆ Qenclosed = net electric displacement flux through closed surface S . DfreeS E r ndAˆ Qenclosed = net electric flux through closed surface S . ETotoS
Thus: B r ndAˆ 0 = net magnetic flux through closed surface S 0 !!! m S Magnetic flux is conserved → magnetic field lines have no beginning / no end points (because no magnetic charge(s)!) 2 The SI units of magnetic flux m are Tesla-m = Webers
16 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede Again: Do not confuse magnetic flux, m with the magnetic scalar potential m r (they even have the same units!!! Webers / Tesla-m2) WAA-HEE !!!
They are not the same thing!!! Ar Ar m r Br ndAˆ BrArArr m S m
Magnetic Flux Magnetic Vector Potential Magnetic Scalar Potential Area element
Don’t confuse these either!!!
1 Ar Ar 2 r r rd gives Ar 0 mm m 4 v r
The magnetic flux through a surface S (not necessarily closed!!!): Br ndSˆˆ A r ndS A r d by Stoke’s Theorem m SS C
n.b. not a closed surface!
Magnetic flux enclosed by contour C : Ard m C
n.b. This d is NOT a line segment associated with a line current I !!!
B r ndSˆˆ A r ndS A r d r d m SS CC mm
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 17 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Griffiths Example 5.11:
A spherical shell of radius R carries a uniform surface charge density and rotates with constant angular velocity , Determine the magnetic vector potential it produces at point r .
A rotating surface charge density produces a surface/sheet current density Kr vr Kr The magnetic vector potential is thus: Ar o da 4 S r
For ease of integration, choose the observation/field point Pr Pzz ˆ (i.e. rzz ˆ ) along the zˆ -axis and to lie in the x-z plane. Choose the origin to be at the center of the sphere, as shown in the figure below:
r rr R22 r 2cos Rr from the law of cosines
Kr vr and: vr r sinxˆ cos zˆ (here) rRsin cos xRˆˆ sin sin yR cos zˆ vr r xyzˆˆˆ vr sin 0 cos RRRsin cos sin sin cos
vr R cos sin sin xˆˆ cos sin cos sin cos y sin sin sin zˆ
22 Now since sindd cos 0 00 Then terms involving only sin or cos in the integral for Ar contribute nothing.
18 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Kr r A roo da da 44SSrr with Kr r and da R2 sin d d and r Rr222cos Rr
3 R sin cos sin Then: Ar o d yˆ 0 22 2 Rr2cos Rr
Let: u cos 0 u 1 du sin d u 1
cos sin 1 udu d 0122 22 R rRr2cos RrRru 2 u1 RrRru22 Rr22 2 Rru 3Rr22 u1 1 22 22 22 R rRrRrRrRrRr 3Rr 2r If rR (i.e. inside sphere) then this integral =2 3R 2R If rR (i.e. outside sphere) then this integral = 2 3r Now: rrysin ˆ
R Then: Arro for rR (inside sphere) 3 R4 Aro r for rR (outside sphere) 3r3
If we now rotate the problem so that zˆ and rr ,, then rrysin ˆ r sinˆ , thus with rotated to zˆ and field point now located at rr ,, , the magnetic vector potential Ar inside/outside the rotating sphere becomes: o R ArR Ar,, r sin ˆ ( rR , inside sphere) Ar max 3 1 R2sin ~ r 3 o R4 sin 2 o ˆ ~1 r Ar,, 2 ( rR , outside sphere) 3 r r rR
zˆ 2R 22 Then: BrAr o cos rˆ sin RzR ˆ !!! ( zˆ ) 333oo
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 19 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Griffiths Example 5.12:
Determine the magnetic vector potential Ar of an infinitely long solenoid with n turns / unit length, radius R and steady current I I n.b. The current extends to infinity, so we cannot use Ar o d because it diverges! 4 C r But we do know that:
Magnetic flux Ar d Ar da Bda m CS S
Flux-enclosing loop / contour
Brda m S
But we know from Ampere’s Circuital Law that: BinsiderR o nIzˆ = uniform & constant
inside 22 mo nI R o nI R
But: inside Ar R d where dRd ˆ m C inside m Ar R2 R Now Asolenoid must be parallel to I Iˆ for the “ideal solenoid” (i.e. no pitch angle) Ar Ar ˆ
inside nI R 2 1 Then: Ar R mo ˆˆ nIR 2 R 2 R 2 o
2 A rR 1 R Ar max ArRnI ˆ 1 If r > R, then more generally, we have: outside o 2 onIR 2 r ~ r ~1 r 1 For r < R, then: ArRnIrinside o ˆ r 2 rR
Note that: Ar A rˆ (only) for the infinitely long ideal solenoid.
20 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Does BrAr ? 1 BrArrArz ˆ in cylindrical coordinates rr 0 2 11 R 11 2 BrRnIroutside o znIRˆ o zˆ 0 2 rr r 2 rr 11 2 11 Binside r R o nI r zˆˆˆ o nI 2 r z o nIz 22rr r
Does Ar 0 ?? (Coulomb Gauge) Ar A rˆ
In Cylindrical Coordinates: 1 Ar Ar 0 because Ar has NO explicit -dependence! r
1 R2 ArRnIoutside o ˆ 2 r 1 ArR nIrˆ inside2 o
Magnetostatic Boundary Conditions
In the case of electrostatics, we learned (via use of Gauss’ Law - E r ndaˆ Qenclosed ) that the normal component of Er suffers a discontinuity ETotoS whenever there is a surface charge density (free or bound) present on a surface / interface:
above below above below Tot free bound VV21 EE21 oonnsurface surface above above 21 ( is continuous across interface) n.b. = perpendicular component relative to surface, = parallel component relative to surface:
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 21 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Consider a thin conducting sheet of material carrying a surface current density of KKxKxˆˆ Amperes/meter
Now imagine that this current sheet KKxKxˆˆ is “placed” in an external magnetic field, e.g. created / emanating from some other current-carrying circuit below this current sheet.
Call this external magnetic field that is below the original current sheet Bbelow . 1ext
What we discover is that the magnetic field above the current sheet Babove is not parallel to Bbelow 2ext 1ext - it has been refracted by the current sheet (in the tangential direction - with respect to the surface)!
The physical origin for this is simple to understand. Below the current sheet, the current sheet 1 itself adds to the tangential component of Bbelow a component Bbelow Kyˆ (for KKx ˆ ), ext sheet2 o above however, above the current sheet, the current sheet adds to the tangential component of Bext a 1 component Babove Kyˆ (for KKx ˆ ). sheet2 o
So if: B BxByBzˆˆ ˆ ext extxyz ext ext
belowbelow below below Then: BextBxByBz extˆˆ ext ext ˆ ║ = parallel to surface xyz And: BaboveBxByBzaboveˆˆ above above ˆ = perpendicular to surface ext extxyz ext ext
22 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede Then by the principle of linear superposition, BBBTot ext sheet . Hence, below the current sheet ( KKx ˆ ):
below Bsheet belowbelow below 1 below below below below BTOTBxB extˆˆˆˆ ext o KyBzBxByBz extˆˆ TOT TOT TOT xy2 z xyz And above the current sheet ( KKx ˆ ):
above Bsheet aboveabove above 1 above above above above BTOTBxB extˆˆˆˆ ext o KyBzBxByBz extˆˆ TOT TOT TOT xy2 z xyz
above below Thus, (comparing BBTOT vs. TOT component-by-component), we see that:
below above 1) BBTOT TOT Tangential (to sheet / surface) component of BTOT parallel xx BBbelow above to sheet current KKx ˆ is continuous. extxx ext
below above 2) BBTOT TOT Tangential (to sheet/surface) component of BTOT perpendicular y y B aboveBK below to sheet current KKx ˆ is discontinuous by an amount TOTyy TOT o
o K across sheet / surface.
3) BBbelow above Normal (to sheet/surface) component of B is continuous TOTzz TOT TOT BBbelow above across sheet / surface. extzz ext
Mathematically, these 3 statements can be compactly combined into a single expression: above below BTOTBKn TOT o ˆ where the unit normal to the surface, nzˆ ˆ (here, as drawn above).
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 23 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede As we found in electrostatics, that the scalar electric potential Vr was continuous across any boundary VrVrabove below , likewise, the magnetic vector potential Ar is also continuous across any boundary, i.e. ArArabove below provided that: Ar 0 , which above below guarantees that ArA r and also provided that: Ar Br , which, in integral form, i.e. Ar d Br da guarantees that ArArabove below . CS m
However, note that the normal derivative of Ar, since Ar K r then Ar also “inherits” the discontinuity associated with B r : B aboveBK below (see #2 on previous TOTyy TOT o page), and since BrAr , thus we have a discontinuity in the (normal) slope(s) of Aron either side of the boundary/current sheet.
We can understand the origin of this condition on the normal derivative(s) of Ar taken just above/below an “interface” e.g. for the specific case of the current sheet KKx ˆ . From B aboveBK below we know that the discontinuity in the B -field is in the yˆ -direction, TOTyy TOT o whereas since the magnetic vector potential associated with the current sheet Aris always parallel to the current, and since KKx ˆ we know that the component of ArTOT that we are concerned with here is in the yˆ -direction. But from: BTOTA TOT , then: BATOT TOT y y thus we need to worry only about the yˆ -component of the curl of ArTOT , which is: A A TOTx TOTz BATOT TOT y y zx
Then, noting that the zˆ -direction is perpendicular (i.e. normal) to the plane of the current sheet: AAaboveAAabove below below BBabove below KTOTxx TOTzz TOT TOT TOTyy TOT o zx zx surface surface above below above below above below AATOT TOT AA AATOT TOT xx TOTzz TOT xx zz x x nn surface surface surface 0 A suffers no discontinuity TOTz Neither A nor A suffer discontinuities in their slopes at the current sheet – only TOTz TOTy A above does - in the normal (i.e. zˆ ) direction. Therefore, we can most generally write this TOTx condition on the discontinuity in the normal derivative on Aras: Arabove Ar below K nno surface surface
24 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
The Magnetic Vector Potential ArAssociated with a Finite Circular Disk Sheet Current
We wish to delve a bit deeper into the nature of the magnetic vector potential, Arand also BrAr associated with current sheets. Consider a sheet current KKx o ˆ flowing on the surface of a finite circular disk of radius R, lying in the x-y plane as shown in the figure below:
zˆ
z r
yˆ
xˆˆ, KKx o z
To keep it simple, we’ll just calculate Arat an arbitrary point along the zˆ -axis above and below the x-y plane. The magnetic vector potential Arassociated with a sheet current is:
Kr Kxˆ da Arooo da 44SSrr
We deliberately chose a sheet current flowing on a finite circular disk of radius R so that we could easily carry out the integration. The area element da on the circular disk (in cylindrical coordinates) is da d d d d , and from the figure above, we see that: r 22z .
R Kxˆ R 2 dd 2 Kxˆ R d 1 Azoo oo Kxˆ 22 z 4 00 22 4 0 222 oo Thus: z z 0 11 Kxˆˆ R22 z z 2 K R 22 z z 2 x 22oo oo
Now there is a subtlety here that we need to notice before proceeding further – since we are interested in knowing Azat an arbitrary point along the zˆ -axis - above and/or below the x-y plane, thus z can be either positive or negative. Note that both the R22 z and z2 terms are always 0 for both positive and/or negative z (in particular: zzz2 !). Thus, in order to preserve this fact, we explicitly keep expression for the magnetic vector potential Az as:
1 Az K R22 z z 2 xˆ 2 oo
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 25 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede A plot of the magnetic vector potential Azvs. z is shown in the figure below for a circular disk of radius R = 10 m and sheet current KKxo ˆˆ1.0 x Amperes/meter.
Note that Azis a maximum when z = 0, right on the sheet current. Note also the discontinuity in the slope(s) of Az on either side of z = 0, which arises due to the presence of the sheet current in the x-y plane, since: Arabove Ar below K nno surface surface Azabove00 Az below or: K zzo zz00
Care/thought must also be taken when carrying out the normal derivatives (slopes) above and below the x-y plane – look carefully at the slopes for z > 0 and z < 0 in the above figure, and compare this information to what we calculate:
above Az 0 zz z 111K Rz22 zx 2ˆˆˆ K x K1 x 222oo oo22 2 oo 22 zz Rz z Rz below Az 0 zz z 111K Rz22 zx 2ˆˆˆ K x K1 x 222oo oo22 2 oo 22 zz Rz z Rz
26 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
Thus we see that indeed: Azabove00 Az below =11 Kxˆˆ Kx Kx ˆ K zz22oo oo oo o zz00 The magnetic field Bz at an arbitrary point along the along the zˆ -axis – either above and/or below the x-y plane is calculated using BzAz in Cartesian coordinates. Since Azx Az A zxˆ (only), then: BzAzAzxy x ˆˆ x z Thus: above above above above Azx 0 1 z B zAzAzxyK000 xoo ˆˆ 2 1y ˆ z Rz22 below below below below Azx 0 1 z B zAzAzxyK000 xoo ˆˆ 2 1y ˆ z Rz22
The figure below shows the magnetic field Bz vs. z along the zˆ -axis with a sheet current KKx o ˆ flowing on the surface of the finite disk of radius R, lying in the x-y plane:
© Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 27 2005-2008. All Rights Reserved. UIUC Physics 435 EM Fields & Sources I Fall Semester, 2007 Lecture Notes 16 Prof. Steven Errede
We now investigate what happens in the limit that the radius of the sheet current-carrying circular disc, R , i.e. it becomes an infinite planar sheet current. We discover that the magnetic vector potential Arassociated with the sheet current KKx o ˆ becomes infinite (i.e. Ardiverges):
11 lim A z K R22 z zx 2ˆˆ K 22 z zx 2 oo oo R 22
whereas the boundary condition on the discontinuity in the normal derivative of Aracross the sheet current lying in the x-y plane at z = 0 still exists, and is well-behaved (i.e. finite):
Azabove00 Az below =11 Kxˆˆ Kx Kx ˆ K zz22oo oo oo o zz00
We also discover that the magnetic field Br is also well-behaved (i.e. finite) – and constant – independent of the height/depth z above/below the x-y plane (!!):
z limBabove zK 011 1 yKyˆˆ 22oo22 oo R z z limBbelow zK 011 1 yKyˆˆ 22oo22 oo R z
28 © Professor Steven Errede, Department of Physics, University of Illinois at Urbana-Champaign, Illinois 2005-2008. All Rights Reserved.