Continuity Equation in Electromagnetism For Current Density

Last edited: 2021-07-11 16:26:31

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The continuity equation is an important tool that one can use whether it is in a fluid dynamics problem or an electromagnetic problem. The continuity equation in electrodynamics relates the charge density to the current density in a volume.

Derivation of Continuity Equation For Charge and Current Density

Lets derive the continuity equation for electric charges. If you are just searching for it, this is what it looks like:

ρt=j, \frac{\partial \rho}{\partial t} = - \nabla \cdot \vec{j},

where ρ\rho is the charge density and j\vec{j} is the current density (current divided by an area). Lets get a few things straight first. When we say the charge is conserved we are talking about the charge in an arbitrary volume. Additional charge can not be created from some sort of source inside the volume. The only way to change the charge is a flow of new charges from outside the volume, that would be our j\vec{j}. So lets observe an infinitesimal surface element dSd \vec{S} on the surface of our volume. The surface element is vector that is normal to the surface. So the infinitesimal charge dqd q that passes through the surface element can be written as:

dq=jdSdt. dq = \vec{j} \cdot d \vec{S} dt.

We'll use this expression later. The total charge qq for the whole volume VV can be written as:

q=VρdV, q = \int_V \rho dV,

where earlier mentioned ρ\rho is the charge density for the volume. We can now use the conservation of charge and look at the change of the charge through time and flux of charge through the volume's surface V\partial V. So we have two expressions, firstly:

dqdt=VρtdV, \frac{dq}{dt} = \int_V \frac{\partial \rho}{\partial t} dV,

which is just the derivative of the total charge for the volume. Secondly, we have:

dqdt=VjdS, \frac{dq}{dt} = - \int_{\partial V} \vec{j} \cdot d \vec{S},

which uses the expression for the charge through a surface element. The reason for the minus sign is because we are calculating the inflow of charges but the surface element vector is pointing outwards from the volume and we have to counteract that. We are almost at our sought after expression but we'll have to use one more trick, the divergence theorem aka Guass's theorem which states:

VFdV=VFdS, \int_V \nabla \cdot \vec{F} dV = \int_{\partial V} \vec{F} \cdot d \vec{S},

which fits perfectly with our charge flux expression:

VjdS=VjdV. - \int_{\partial V} \vec{j} \cdot d \vec{S} = - \int_V \nabla \cdot \vec{j} dV.

So now we have:

dqdt=VρtdV=VjdV. \frac{dq}{dt} = \int_V \frac{\partial \rho}{\partial t} dV = - \int_V \nabla \cdot \vec{j} dV.

As you can see we have two expression with a volume integral for the volume VV. So we can remove the integral and we finally get our continuity equation for electric charges:

ρt=j. \frac{\partial \rho}{\partial t} = - \nabla \cdot \vec{j}.

Now lets see how the continuity equation looks in different coordinate systems.

Continuity Equation in Cartesian Coordinates

The continuity equation for charges in Cartesian coordinates is given by:

ρt+jxx+jyy+jzz=0. \frac{\partial \rho}{\partial t} + \frac{\partial j_x}{\partial x} + \frac{\partial j_y}{\partial y} + \frac{\partial j_z}{\partial z} = 0.

Continuity Equation in Cylindrical Coordinates

The continuity equation for charges in cylindrical coordinates is given by:

ρt+1rr(rjr)+1rθ(jθ)+z(jz)=0. \frac{\partial \rho}{\partial t} + \frac{1}{r} \frac{\partial}{\partial r}(r j_r) + \frac{1}{r} \frac{\partial}{\partial \theta}(j_\theta) + \frac{\partial}{\partial z}(j_z) = 0.

Continuity Equation in Spherical Coordinates

The continuity equation for charges in spherical coordinates is given by:

ρt+1r2r(r2jr)+1rsinθθ(jθsinθ)+1rsinθφ(jφ)=0. \frac{\partial \rho}{\partial t} + \frac{1}{r^2} \frac{\partial}{\partial r}(r^2 j_r) + \frac{1}{r \sin{\theta}} \frac{\partial}{\partial \theta}(j_\theta \sin{\theta}) + \frac{1}{r \sin{\theta}} \frac{\partial}{\partial \varphi}(j_\varphi) = 0.

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