For electrostatic fields, we found from Coulomb’s law that there is a scalar function such that E=−∇V. For charge distributions that are finite in extent (e.g., not an infinite line or plane), we can compute E by first computing
V(r)=4πϵo1(∫ԉρ(r′)dτ′+∫ԉσ(r′)dA′+∫ԉλ(r′)dl′)
and then use E=−∇V. (In most problems, only one of the charge densities in the above equation was not zero; the equation above is the most general equation.) Given that the integrands are scalars, it is often easier to use this approach rather than computing E directly using Coulomb’s Law:
(I’ve written the integrands in a slightly different way so that it looks more like the integrands for E.)
From the Biot–Savart law, it can be shown that ∇×B=μoJ. Because ∇×B=0, we cannot in general find a scalar function Vm such that B=−∇Vm. (Vm has some use; it can be used for solving boundary value problems in current–free regions and also when fitting measurements from current–free regions.)
However, we can find a vector function A for which B=∇×A. This vector is called the “vector potential,” and it applies to magnetic fields only.
A natural question is why we introduce this vector potential (see also 15-4 in the Feynman Lectures on Physics). One of the reasons that V is useful is that it is a scalar, and so instead of discussing the vector function E, we can discuss the scalar function V. Also, V has a physical interpretation and use – for example, it can be used to find the work required to assemble a charge distribution. Neither of these is true for the vector potential A. There are, however, several uses for A. One is that the equations for finding it look similar to that for V:
A(r)=4πμo(∫ԉJ(r′)dτ′+∫ԉK(r′)da′+∫ԉI(r′)dl′).
As a result, some of the techniques used in computing V can be used in computing A. In addition, some of the integrals found for V can be re–used when they appear in integrals required to compute A. Recall that the expansion of 1/ԉ was used to find the multipole expansion of V in Chapter 3.4 of Griffiths (so as to avoid having to integrate to find V at points for which r>r′). The integrals for A have a 1/ԉ, and so we can use the multipole expansion to find an equation for A that allows us to avoid having to integrate to find A (and also B because it can be computed from A).
A second reason that A is useful is that we can write ∇2A=−μoJ, which is the analog to the Poisson equation ∇2V=−ρ/ϵo. Sometimes we can use the boundary value techniques for solving Poisson’s equation for solving ∇2A=−μoJ (which is actually three equations, each which have the form of Poisson’s equation: ∇2Ax=−μoJx, ∇2Ay=−μoJy, ∇2Az=−μoJz.)
Finally, the vector potential appears as a natural quantity in the Lagrangian in classical mechanics and in many equations in quantum mechanics. This is discussed in detail in 15-4 in the Feynman Lectures on Physics.
This B has the same form as a magnetic dipole in spherical coordinates and unit vectors; we can conclude that this vector potential is that for a magnetic dipole for which the current system is a small loop of area A centered on the origin in the x–y plane if α=μoIA/4π.
Inserting zeros for terms involving partial derivative of Ax and Ay gives
∇×A=(∂y∂Az−0)x^+(0−∂x∂Az)y^+(0+0)z^
Evaluation gives
B=∇×A=∓αx^
This is the field of a sheet of current in the x–y plane with current flowing in the +z^ direction. (To see this, draw out the bound current sheets and see HW #11.1.
The general equation for the vector potential for a magnetic dipole is
A=4πμor2m×r^
If m=mox^, find B in cartesian coordinates with cartesian unit vectors. Note that you can check your answer using equation 5.89 of Griffiths 4th edition:
B=4πμor31[3(m⋅r^)r^−m]
Answer
Method 1
In Magnetic Dipoles, the equation for a with dipole m=Iπb2z^ was given as
B=4πμor5Iπb2(3xzx^+3yzy^+(3z2−r2)z^)
Swapping z and x and replacing Iπb2 with mo gives the answer to this problem:
There are two general types of problems related to computing A
if B is known, and
if B is not known
If B is known, we can sometimes (a.) find A by guessing what A will give B=∇×A, (b.) use B=∇×A, and (c.) and additional information, or using ∮A⋅dl=∫B⋅dl. As an example of (c.), see Example 5.12 of Griffiths.
If B is not known, we can always use direct integration to find A. Often the integral encountered will be one that was previously used to find V using direct integration. Most generally, the integral will not have a closed–form solution, and we will write the integrant of A as a power series as was done in the monopole expansion for V.
Suppose that we know B for an infinitely long wire along the z–axis with I=Iz^. It can be argued using symmetry that for a certain choice of integration path for the line integral that
∮A⋅dl=∫B⋅da
simplifies to
Az(s)L−A(so)L=L∫sosBϕds′
Using Bϕ=2πμosI gives
Az(s)=Az(so)−2πμoIlnsos
Suppose B was not known. We can solve for A by analogy. For a finite wire along the z axis that is centered on the origin and has a length L, the vector potential is
A=∫ԉI(r′)dl′
Here, dl′=dz′ (the dl′ here is the differential length along the wire; in ∮A⋅dl used above, dl is a path of integration). Using I=Iz^, we have
Az=4πμo∫−L/2L/2ԉIdz′
We have encountered an integral like this before. If, instead of a wire, we have a uniformly charged line of charge density λ, then
V=4πϵo1∫−L/2L/2ԉλdz′
From this, we can conclude that we can take the answer for V and replace λ/ϵo with μoI to get Az.
For an infinitly long wire, we can’t actually use the above equation to find V. We can only compute the potential difference V(s)−V(so)=−∫sosE⋅ds^. For an infinite wire, E=(λ/2πϵo)s^/s and integration gives V(s)−V(so)=−(λ/2πϵo)ln(s/so). Using the replacement of λ/ϵo with μoI gives
set up the integral that must be solved to find A(x,y,z) due to a loop with current I of radius b that lies in the x–y plane and is centered on the origin.
Answer
I=Iϕ^
dl′=bdϕ′
r′=bs^
r=xx^+yy^+zz^
To do the integration, we need to convert non-cartesian unit vectors to cartesian unit vectors.