15  Deep dive: does an electromagnetic wave carry energy?

Poynting’s theorem, and why it still works where there is no current. A companion to slides 70–78 and Chapter 3.

NoteAbout this chapter

This is a self-contained derivation, meant for students who want to see why \(\mathbf S=\mathbf E\times\mathbf H\) is an energy flux, not just use it. Unlike the rest of the book, its plane-wave section uses the physics convention \(e^{i(\mathbf k\cdot\mathbf r-\omega t)}\) (see the note there); every physical result is the same.

15.1 The question

We say that light from the Sun heats the Earth, that a radio transmitter “sends power” to a receiver, and that a laser can cut steel. All of these statements assume that energy travels through empty space carried by the electromagnetic field.

That is not obvious. In the gap between the Sun and the Earth there are no charges and no currents. So what exactly is carrying the energy, and how can we prove it rather than just assert it?

The plan is:

  1. Define energy through what it does to matter (work on charges).
  2. Derive, from Maxwell’s equations alone, a conservation law: Poynting’s theorem.
  3. Look at the vacuum case, where \(\mathbf{J}=0\), and see what the theorem does and does not tell us there.
  4. Close the argument with a thought experiment: a pulse travelling between a transmitter and a receiver.
NoteWhat you need

Maxwell’s equations in differential form, the Lorentz force, the divergence theorem, and one vector identity (given below).

15.2 Starting point: how fields exchange energy with matter

Energy, in mechanics, is defined through work. So we first ask: at what rate do electromagnetic fields do work on charges?

A charge \(q\) moving with velocity \(\mathbf{v}\) feels the Lorentz force

\[ \mathbf{F} = q\left(\mathbf{E} + \mathbf{v}\times\mathbf{B}\right). \]

The power delivered to the charge is

\[ P = \mathbf{F}\cdot\mathbf{v} = q\,\mathbf{E}\cdot\mathbf{v} + q\,(\mathbf{v}\times\mathbf{B})\cdot\mathbf{v} = q\,\mathbf{E}\cdot\mathbf{v}, \]

because \(\mathbf{v}\times\mathbf{B}\) is perpendicular to \(\mathbf{v}\): the magnetic force does no work.

For a continuous distribution of charge with density \(\rho\) moving with velocity \(\mathbf{v}\), the current density is \(\mathbf{J}=\rho\mathbf{v}\), and the power delivered per unit volume is

\[ p = \rho\,\mathbf{v}\cdot\mathbf{E} = \mathbf{J}\cdot\mathbf{E}. \tag{15.1}\]

ImportantKey point 1

\(\mathbf{J}\cdot\mathbf{E}\) is the only place where the fields hand energy to matter (kinetic energy, heat in a resistor, charging a battery) or take it back (a generator driving an antenna). It is the bridge between “field” and “mechanical energy”.

15.3 Deriving Poynting’s theorem

15.3.1 The two curl equations

\[ \nabla\times\mathbf{E} = -\frac{\partial\mathbf{B}}{\partial t} \tag{15.2}\]

\[ \nabla\times\mathbf{H} = \mathbf{J} + \frac{\partial\mathbf{D}}{\partial t} \tag{15.3}\]

15.3.2 Build a scalar equation

Take the dot product of Equation 15.2 with \(\mathbf{H}\) and of Equation 15.3 with \(\mathbf{E}\):

\[ \mathbf{H}\cdot(\nabla\times\mathbf{E}) = -\mathbf{H}\cdot\frac{\partial\mathbf{B}}{\partial t} \]

\[ \mathbf{E}\cdot(\nabla\times\mathbf{H}) = \mathbf{E}\cdot\mathbf{J} + \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t} \]

Subtract the second from the first:

\[ \mathbf{H}\cdot(\nabla\times\mathbf{E}) - \mathbf{E}\cdot(\nabla\times\mathbf{H}) = -\mathbf{H}\cdot\frac{\partial\mathbf{B}}{\partial t} - \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t} - \mathbf{J}\cdot\mathbf{E}. \]

15.3.3 Use the vector identity

\[ \nabla\cdot(\mathbf{E}\times\mathbf{H}) = \mathbf{H}\cdot(\nabla\times\mathbf{E}) - \mathbf{E}\cdot(\nabla\times\mathbf{H}) \]

The left-hand side is therefore a divergence:

\[ -\nabla\cdot(\mathbf{E}\times\mathbf{H}) = \mathbf{H}\cdot\frac{\partial\mathbf{B}}{\partial t} + \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t} + \mathbf{J}\cdot\mathbf{E}. \tag{15.4}\]

15.3.4 Recognise a time derivative

In a linear, isotropic, non-dispersive medium, \(\mathbf{D}=\varepsilon\mathbf{E}\) and \(\mathbf{B}=\mu\mathbf{H}\) with constant \(\varepsilon,\mu\). Then

\[ \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t} = \varepsilon\,\mathbf{E}\cdot\frac{\partial\mathbf{E}}{\partial t} = \frac{\partial}{\partial t}\left(\tfrac12\varepsilon E^2\right), \qquad \mathbf{H}\cdot\frac{\partial\mathbf{B}}{\partial t} = \frac{\partial}{\partial t}\left(\tfrac12\mu H^2\right). \]

Define

\[ u = \tfrac12\left(\mathbf{E}\cdot\mathbf{D} + \mathbf{H}\cdot\mathbf{B}\right), \qquad \mathbf{S} = \mathbf{E}\times\mathbf{H}. \tag{15.5}\]

NoteAssumption to keep in mind

The step \(\mathbf{E}\cdot\partial_t\mathbf{D} = \partial_t(\tfrac12\varepsilon E^2)\) assumes a non-dispersive medium. We come back to this in Section 15.9, where it changes the answer to “how fast does energy travel?”.

Equation 15.4 becomes Poynting’s theorem in differential form:

\[ \boxed{\;\frac{\partial u}{\partial t} + \nabla\cdot\mathbf{S} = -\,\mathbf{J}\cdot\mathbf{E}\;} \tag{15.6}\]

15.3.5 Integral form

Integrate over a volume \(V\) with closed surface \(\partial V\) and apply the divergence theorem:

\[ \boxed{\;-\frac{d}{dt}\int_V u\,dV = \oint_{\partial V}\mathbf{S}\cdot d\mathbf{a} + \int_V \mathbf{J}\cdot\mathbf{E}\,dV\;} \tag{15.7}\]

WarningSo far, this is only mathematics

Equation 15.6 is an identity that follows from Maxwell’s equations. We named the quantities \(u\) and \(\mathbf{S}\), but naming is not proving. The physics enters only when we interpret each term.

15.3.6 Interpreting the terms

Read Equation 15.7 as a budget for the volume \(V\):

Term Meaning Justified by
\(\int_V \mathbf{J}\cdot\mathbf{E}\,dV\) rate at which mechanical energy of charges in \(V\) increases Lorentz force, Equation 15.1
\(\dfrac{d}{dt}\int_V u\,dV\) rate of change of something stored in \(V\) must be energy, for the budget to balance
\(\oint_{\partial V}\mathbf{S}\cdot d\mathbf{a}\) rate at which that something leaves through the surface must be energy flux, for the budget to balance

Because the first term is certainly energy per unit time, and all terms in one equation must have the same physical nature, the other two are energy too: \(u\) is the energy density of the field (J/m³) and \(\mathbf{S}\) is the energy flux density (W/m²), the Poynting vector.

15.4 The objection: in vacuum there is no current

TipThe students’ question

“In a wave travelling through empty space there are no electrons. So \(\mathbf{J}=0\). How can a term that needs moving charges tell us anything about the wave?”

The objection is correct. In vacuum, \(\mathbf{J}=0\), \(\mathbf{D}=\varepsilon_0\mathbf{E}\), \(\mathbf{B}=\mu_0\mathbf{H}\), and Equation 15.6 reduces to

\[ \frac{\partial u}{\partial t} + \nabla\cdot\mathbf{S} = 0, \qquad u = \tfrac12\varepsilon_0 E^2 + \frac{B^2}{2\mu_0}. \tag{15.8}\]

The resolution is to separate two different questions that are easy to mix up.

15.4.1 Question A: in vacuum, is something conserved and moving?

Yes. Equation 15.8 has exactly the form of the continuity equation for charge,

\[ \frac{\partial\rho}{\partial t} + \nabla\cdot\mathbf{J} = 0 . \]

It says: \(u\) cannot be created or destroyed at a point; it can only flow, and \(\mathbf{S}\) is its flux. If \(u\) decreases somewhere, it is because \(\mathbf{S}\) carries it to the neighbouring region.

15.4.2 Question B: is that “something” energy?

The vacuum equation alone cannot answer this. A continuity equation only tells you that some quantity is conserved. In fact the free Maxwell equations have other locally conserved quantities built from the fields (for example the optical helicity), each with its own continuity equation. Nothing in Equation 15.8 singles out \(u\) as energy.

Besides energy, momentum and angular momentum, the source-free Maxwell equations admit further conserved densities: the optical helicity, and an infinite family discovered by Lipkin (1964) that he called “zilch”. They are all conserved in vacuum and obey continuity equations, yet none of them is energy. This is precisely why the vacuum equation alone is not enough.

15.4.3 Answer: matter tells us which conserved quantity is energy

“Energy” is defined by what it can do to matter: heat an absorber, accelerate a charge, drive a current. The only term in the theorem that talks to matter is \(\mathbf{J}\cdot\mathbf{E}\), and it only appears where there are charges.

So we apply Equation 15.7 to a volume that contains charges: the transmitting antenna or the absorbing receiver. There, mechanical energy lost or gained by the charges is balanced by \(\mathbf{S}\) and \(u\). That calibrates \(u\) and \(\mathbf{S}\) as energy.

Crucially, \(u\) and \(\mathbf{S}\) are defined by the same expressions Equation 15.5 everywhere, in the antenna and in the empty space around it. Once they are identified as energy where matter is present, they are energy everywhere.

ImportantKey point 2

\(\mathbf{J}\cdot\mathbf{E}\) is not needed where the wave is. It is needed where we identify what the wave carries: at the source and at the receiver. The vacuum region only has to show that the quantity is conserved and moves, which Equation 15.8 does.

TipAn analogy

A ball flying through the air has no force doing work on it (ignore gravity and drag). Nothing during the flight tells you that \(\tfrac12 mv^2\) is energy. You know it because of the throw (your muscles did work) and the impact (it can break a window). The flight only shows that the quantity is conserved and travels with the ball.

15.5 The decisive thought experiment: a pulse in flight

This argument shows that the energy must be in the field, not as a matter of interpretation, but because otherwise energy conservation would fail.

15.5.1 Set-up

  • A transmitting antenna T at the origin.
  • A receiver R at distance \(d\).
  • Empty space in between: no charges, \(\mathbf{J}=0\).

At \(t=0\) the generator drives T for a short time \(\tau\), then switches off. We choose \(\tau \ll d/c\).

We track three volumes: \(V_T\) around the transmitter, \(V_R\) around the receiver, and the vacuum between them.

15.5.2 The energy budget over time

Let \(W_\text{rad}\) be the energy the generator supplied and that did not end up as heat in the antenna wires (it is measurable: it is the work done against the radiation resistance, \(\int R_\text{rad}\,I^2\,dt\)).

Time interval Mechanical energy lost by charges in T Mechanical energy gained by charges in R Charges between T and R Where is \(W_\text{rad}\)?
\(t<0\) 0 0 none still in the generator
\(0<t<\tau\) increasing up to \(W_\text{rad}\) 0 none leaving \(V_T\) through \(\oint\mathbf{S}\cdot d\mathbf{a}\)
\(\tau < t < d/c\) \(W_\text{rad}\) (final) 0 (signal has not arrived) none ?
\(t > d/c\) \(W_\text{rad}\) \(> 0\) none partly absorbed in R, the rest travels on

15.5.3 The contradiction, and its only resolution

Look at the third row. The transmitter has already lost \(W_\text{rad}\): the generator is switched off and the work has been done. The receiver has not yet gained anything, because no signal travels faster than \(c\). Between them there is no matter at all.

If energy is only a property of matter, then during the interval \(\tau < t < d/c\) the total energy of the universe is smaller by \(W_\text{rad}\). Energy conservation would be violated for a finite time, and then mysteriously restored when the pulse arrives.

The only way to keep energy conserved at every instant is that the energy is located in the fields between T and R. Poynting’s theorem tells us exactly where and how much. At time \(t\) the pulse occupies the spherical shell \(c(t-\tau) < r < ct\), and

\[ \int_\text{shell} u\,dV = W_\text{rad}. \]

ImportantKey point 3

The absence of current in the vacuum is not a weakness of the argument. It is the argument. Because nothing material sits between transmitter and receiver while the pulse is in flight, the energy has nowhere else to be but in the field.

15.6 A common trap: the “displacement current”

In vacuum Equation 15.3 reads

\[ \nabla\times\mathbf{H} = \varepsilon_0\frac{\partial\mathbf{E}}{\partial t}. \]

The right-hand side is historically called the displacement current. Some students conclude: “So there is a current in vacuum, and that is what \(\mathbf{J}\) refers to.” This is wrong, for two reasons.

  1. It involves no moving charge. It is simply a time-varying electric field. The name comes from Maxwell’s mechanical models of the ether and is misleading.
  2. In the derivation it does not end up in \(\mathbf{J}\cdot\mathbf{E}\). It ends up in \(\mathbf{E}\cdot\partial\mathbf{D}/\partial t\), which is part of \(\partial u/\partial t\): it describes a change of stored field energy, not work done on matter.

\(\mathbf{J}\) in Poynting’s theorem is always the current of real charges.

15.7 Plane waves from Maxwell’s equations

Up to now we have stated the plane-wave fields. Here we derive them, and in particular the relation \(E = vB\), which is what makes the electric and magnetic energies equal.

NoteConvention

We use the physics convention \(e^{i(\mathbf{k}\cdot\mathbf{r}-\omega t)}\). With the engineering convention \(e^{j(\omega t-\mathbf{k}\cdot\mathbf{r})}\) the signs of some intermediate expressions change (for example \(\varepsilon - j\sigma/\omega\) instead of \(\varepsilon + i\sigma/\omega\)), but every physical result is identical. Physical fields are always the real parts of the complex expressions.

15.7.1 Ansatz

Consider a linear, homogeneous, isotropic, source-free medium (\(\rho=0\), \(\mathbf{J}=0\)) with constant \(\varepsilon\) and \(\mu\). We look for solutions of the form

\[ \mathbf{E}(\mathbf{r},t) = \mathbf{E}_0\,e^{i(\mathbf{k}\cdot\mathbf{r}-\omega t)}, \qquad \mathbf{B}(\mathbf{r},t) = \mathbf{B}_0\,e^{i(\mathbf{k}\cdot\mathbf{r}-\omega t)}, \tag{15.9}\]

where \(\mathbf{E}_0\) and \(\mathbf{B}_0\) are constant vectors, possibly complex (this includes every polarization).

For such fields, derivatives become multiplications:

\[ \nabla \;\to\; i\mathbf{k}, \qquad \frac{\partial}{\partial t} \;\to\; -i\omega . \]

Maxwell’s four differential equations therefore become four algebraic vector equations.

15.7.2 The divergence equations: the wave is transverse

\[ \nabla\cdot\mathbf{E}=0 \;\Rightarrow\; \mathbf{k}\cdot\mathbf{E}_0 = 0, \qquad \nabla\cdot\mathbf{B}=0 \;\Rightarrow\; \mathbf{k}\cdot\mathbf{B}_0 = 0 . \]

Both fields are perpendicular to the direction of propagation.

15.7.3 Faraday’s law: the ratio \(E/B\)

\[ \nabla\times\mathbf{E} = -\frac{\partial\mathbf{B}}{\partial t} \;\Rightarrow\; i\,\mathbf{k}\times\mathbf{E}_0 = i\omega\,\mathbf{B}_0 \;\Rightarrow\; \boxed{\;\mathbf{B}_0 = \frac{\mathbf{k}\times\mathbf{E}_0}{\omega}\;} \tag{15.10}\]

This single line contains three results.

  • Direction. \(\mathbf{B}_0\) is perpendicular to both \(\mathbf{E}_0\) and \(\mathbf{k}\): the vectors \((\mathbf{E},\mathbf{B},\mathbf{k})\) form a right-handed triad.
  • Magnitude. Since \(\mathbf{k}\perp\mathbf{E}_0\), \(|\mathbf{k}\times\mathbf{E}_0| = k\,|\mathbf{E}_0|\), hence \[ \frac{|\mathbf{E}_0|}{|\mathbf{B}_0|} = \frac{\omega}{k} \equiv v_\varphi , \] the phase velocity. This is the precise meaning of \(v\) in “\(E = vB\)”.
  • Phase. If \(k\) is real, \(\mathbf{B}\) is exactly in phase with \(\mathbf{E}\): they vanish and peak at the same points and instants.
ImportantKey point 4

Faraday’s law alone relates \(E\) and \(B\), but it does not tell us how fast the wave travels: \(v_\varphi\) is still unknown.

15.7.4 Ampère–Maxwell law: a second relation

\[ \nabla\times\mathbf{H} = \frac{\partial\mathbf{D}}{\partial t} \;\Rightarrow\; i\,\mathbf{k}\times\frac{\mathbf{B}_0}{\mu} = -i\omega\varepsilon\,\mathbf{E}_0 \;\Rightarrow\; \mathbf{E}_0 = -\frac{\mathbf{k}\times\mathbf{B}_0}{\omega\mu\varepsilon} . \tag{15.11}\]

15.7.5 Consistency: the dispersion relation

Insert Equation 15.10 into Equation 15.11:

\[ \mathbf{E}_0 = -\frac{\mathbf{k}\times(\mathbf{k}\times\mathbf{E}_0)}{\omega^2\mu\varepsilon} . \]

With \(\mathbf{a}\times(\mathbf{b}\times\mathbf{c}) = \mathbf{b}(\mathbf{a}\cdot\mathbf{c}) - \mathbf{c}(\mathbf{a}\cdot\mathbf{b})\) and \(\mathbf{k}\cdot\mathbf{E}_0 = 0\),

\[ \mathbf{k}\times(\mathbf{k}\times\mathbf{E}_0) = \mathbf{k}\,(\mathbf{k}\cdot\mathbf{E}_0) - k^2\,\mathbf{E}_0 = -k^2\,\mathbf{E}_0 , \]

so

\[ \mathbf{E}_0 = \frac{k^2}{\omega^2\mu\varepsilon}\,\mathbf{E}_0 \quad\Rightarrow\quad \boxed{\;k^2 = \omega^2\mu\varepsilon\;} \quad\Rightarrow\quad v_\varphi = \frac{\omega}{k} = \frac{1}{\sqrt{\mu\varepsilon}} . \tag{15.12}\]

In vacuum \(v_\varphi = 1/\sqrt{\mu_0\varepsilon_0} = c\), and therefore \(E = cB\).

ImportantKey point 5

Faraday says \(E/B = \omega/k\). Ampère–Maxwell says \(E/B = k/(\omega\mu\varepsilon)\). Both can be true only if the wave travels at \(1/\sqrt{\mu\varepsilon}\). Neither equation alone predicts light; their mutual consistency does.

15.7.6 Back to real fields

Take \(\mathbf{k} = k\,\hat{\mathbf{z}}\) and \(\mathbf{E}_0 = E_0\,\hat{\mathbf{x}}\) with \(E_0\) real. Then \(\mathbf{k}\times\mathbf{E}_0 = kE_0\,\hat{\mathbf{y}}\), and the real parts are

\[ \mathbf{E} = E_0\cos(kz-\omega t)\,\hat{\mathbf{x}}, \qquad \mathbf{B} = \frac{E_0}{v_\varphi}\cos(kz-\omega t)\,\hat{\mathbf{y}} . \tag{15.13}\]

Because Equation 15.10 is linear, the same holds for any polarization. For circular polarization, \(\mathbf{E}_0 = E_0(\hat{\mathbf{x}} + i\hat{\mathbf{y}})/\sqrt2\): \(\mathbf{B}\) rotates together with \(\mathbf{E}\), always at \(90^\circ\) from it, with \(|\mathbf{E}| = v_\varphi|\mathbf{B}|\) at every instant.

15.7.7 Energy of the plane wave

With \(H = B/\mu\) and \(E = v_\varphi B\):

\[ u_B = \frac{B^2}{2\mu} = \frac{E^2}{2\mu v_\varphi^2} = \tfrac12\varepsilon E^2 = u_E, \qquad \frac{E}{H} = \mu v_\varphi = \sqrt{\frac{\mu}{\varepsilon}} \equiv \eta , \]

where \(\eta\) is the wave impedance (\(\eta_0 \approx 377\ \Omega\) in vacuum). The electric and magnetic energy densities are equal, and \(u = \varepsilon E^2\).

The Poynting vector points along \(\mathbf{k}\) (right-handed triad):

\[ \mathbf{S} = \mathbf{E}\times\mathbf{H} = \frac{E^2}{\eta}\,\hat{\mathbf{k}} = v_\varphi\,u\,\hat{\mathbf{k}} . \]

Time averages, using phasors and \(\langle\cos^2\rangle = \tfrac12\):

\[ \langle\mathbf{S}\rangle = \tfrac12\,\mathrm{Re}\!\left(\mathbf{E}_0\times\mathbf{H}_0^*\right) = \frac{|\mathbf{E}_0|^2}{2\eta}\,\hat{\mathbf{k}}, \qquad \langle u\rangle = \tfrac12\varepsilon\,|\mathbf{E}_0|^2, \qquad \langle S\rangle = v_\varphi\,\langle u\rangle . \tag{15.14}\]

In vacuum the energy flows at \(c\). You can check directly that Equation 15.13 satisfies Equation 15.8.

WarningHold on

In a non-dispersive medium the energy moves at the phase velocity. We will see in Section 15.9 that this is not true in dispersive media: there, energy moves at the group velocity.

15.8 Plane waves in a lossy medium

We now put charges back in: a medium with conductivity \(\sigma\), so that \(\mathbf{J} = \sigma\mathbf{E}\). This is exactly the situation of the receiver (the absorber) in the pulse thought experiment, and it is where \(\mathbf{J}\cdot\mathbf{E}\) becomes non-zero.

15.8.1 Complex permittivity and complex wave number

Ampère–Maxwell now reads

\[ i\,\mathbf{k}\times\mathbf{H}_0 = \sigma\mathbf{E}_0 - i\omega\varepsilon\,\mathbf{E}_0 = -i\omega\,\varepsilon_c\,\mathbf{E}_0, \qquad \varepsilon_c \equiv \varepsilon + i\frac{\sigma}{\omega} . \tag{15.15}\]

The conduction current is absorbed into a complex permittivity \(\varepsilon_c\). Faraday’s law is unchanged, so every step of Section 15.7 goes through with \(\varepsilon \to \varepsilon_c\):

\[ k^2 = \omega^2\mu\,\varepsilon_c . \]

The wave number is now complex. For a wave travelling along \(z\) we write

\[ k = \beta + i\alpha, \qquad \beta^2 - \alpha^2 = \omega^2\mu\varepsilon, \qquad 2\alpha\beta = \omega\mu\sigma , \tag{15.16}\]

which gives

\[ \beta = \omega\sqrt{\frac{\mu\varepsilon}{2}}\left[\sqrt{1+\left(\frac{\sigma}{\omega\varepsilon}\right)^2}+1\right]^{1/2}, \qquad \alpha = \omega\sqrt{\frac{\mu\varepsilon}{2}}\left[\sqrt{1+\left(\frac{\sigma}{\omega\varepsilon}\right)^2}-1\right]^{1/2}. \]

The dimensionless ratio \(\sigma/(\omega\varepsilon)\) (conduction current over displacement current) decides the regime.

15.8.2 The fields

With \(\mathbf{E}_0 = E_0\hat{\mathbf{x}}\), \(E_0\) real:

\[ \mathbf{E} = E_0\,e^{-\alpha z}\cos(\beta z - \omega t)\,\hat{\mathbf{x}} . \]

Faraday still gives \(\mathbf{B}_0 = \mathbf{k}\times\mathbf{E}_0/\omega\), but now \(k\) is complex:

\[ B_0 = \frac{\beta + i\alpha}{\omega}\,E_0 = \frac{|k|}{\omega}\,E_0\,e^{i\phi}, \qquad \phi = \arctan\frac{\alpha}{\beta}, \]

\[ \mathbf{B} = \frac{|k|}{\omega}\,E_0\,e^{-\alpha z}\cos(\beta z - \omega t + \phi)\,\hat{\mathbf{y}} . \]

Three things change with respect to the lossless case:

  1. The wave decays as \(e^{-\alpha z}\); the intensity decays as \(e^{-2\alpha z}\).
  2. \(\mathbf{B}\) lags \(\mathbf{E}\) in time by \(\phi/\omega\).
  3. The simple relation fails: \(|E|/|B| = \omega/|k|\), which is neither \(\omega/\beta\) (the phase velocity) nor \(1/\sqrt{\mu\varepsilon}\).

15.8.3 Limiting case: a good conductor

For \(\sigma \gg \omega\varepsilon\):

\[ \alpha \simeq \beta \simeq \sqrt{\frac{\omega\mu\sigma}{2}} \equiv \frac{1}{\delta}, \qquad \phi \simeq 45^\circ , \]

where \(\delta\) is the skin depth. The ratio of magnetic to electric energy is

\[ \frac{\langle u_B\rangle}{\langle u_E\rangle} = \frac{|B_0|^2/\mu}{\varepsilon|E_0|^2} = \frac{|k|^2}{\omega^2\mu\varepsilon} = \sqrt{1+\left(\frac{\sigma}{\omega\varepsilon}\right)^2} \gg 1 : \]

inside a good conductor the field energy is almost entirely magnetic, and \(|E|/|H| = \sqrt{\omega\mu/\sigma} \ll \eta_0\).

15.8.4 Poynting’s theorem with \(\mathbf{J}\ne 0\): the absorber’s energy budget

This is the case the pulse argument needs: the field hands its energy to matter. We check Equation 15.6 explicitly.

With \(\mathbf{H}_0 = \mathbf{B}_0/\mu = (\beta + i\alpha)E_0/(\omega\mu)\,\hat{\mathbf{y}}\), the time-averaged Poynting vector is

\[ \langle S_z\rangle = \tfrac12\mathrm{Re}\!\left(E_0 H_0^*\right)e^{-2\alpha z} = \frac{\beta\,E_0^2}{2\omega\mu}\,e^{-2\alpha z} . \]

In steady state \(\langle \partial u/\partial t\rangle = 0\), so the time-averaged theorem reads \(-\,d\langle S_z\rangle/dz = \langle\mathbf{J}\cdot\mathbf{E}\rangle\). Both sides:

\[ -\frac{d\langle S_z\rangle}{dz} = \frac{\alpha\beta}{\omega\mu}\,E_0^2\,e^{-2\alpha z}, \qquad \langle\mathbf{J}\cdot\mathbf{E}\rangle = \langle\sigma E^2\rangle = \tfrac12\sigma E_0^2\,e^{-2\alpha z} . \]

They are equal because \(2\alpha\beta = \omega\mu\sigma\) (Equation 15.16). ✓

Integrating the Joule heating over the whole half-space \(z>0\):

\[ \int_0^\infty \tfrac12\sigma E_0^2\,e^{-2\alpha z}\,dz = \frac{\sigma E_0^2}{4\alpha} = \frac{\beta E_0^2}{2\omega\mu} = \langle S_z(0)\rangle . \]

ImportantKey point 6

All the power that enters the surface of the absorber is converted into heat, and Poynting’s theorem accounts for it point by point. The decrease of \(\mathbf{S}\) with depth is exactly the work \(\mathbf{J}\cdot\mathbf{E}\) done on the conduction electrons. This is the “receiver” end of the pulse argument, now made quantitative.

(Here \(E_0\) is the field just inside the surface; the reflection at the interface is a separate problem.)

15.9 Energy velocity and group velocity in dispersive media

15.9.1 The problem

Real materials are dispersive: \(\varepsilon\) and \(\mu\) depend on frequency. Glass, silicon, lithium niobate: the refractive index \(n(\omega)\) is never exactly constant.

Two things then go wrong with what we did so far.

  1. In the derivation of Poynting’s theorem we wrote \(\mathbf{E}\cdot\partial\mathbf{D}/\partial t = \partial_t(\tfrac12\varepsilon E^2)\). This requires \(\mathbf{D}(t) = \varepsilon\,\mathbf{E}(t)\) at the same instant. In a dispersive medium \(\mathbf{D}(t)\) depends on \(\mathbf{E}\) at earlier times, so \(u = \tfrac12(\mathbf{E}\cdot\mathbf{D} + \mathbf{H}\cdot\mathbf{B})\) is no longer the stored energy.
  2. A pulse does not travel at the phase velocity \(\omega/k\) but at the group velocity

\[ v_g = \frac{d\omega}{dk} = \frac{c}{n + \omega\,\dfrac{dn}{d\omega}} \equiv \frac{c}{n_g}, \]

where \(n_g\) is the group index. In silicon waveguides, for example, \(n_g\) is typically much larger than the effective index.

We define the energy velocity as the ratio of time-averaged energy flux to time-averaged energy density:

\[ v_E \equiv \frac{\langle S\rangle}{\langle u\rangle} . \tag{15.17}\]

In Equation 15.14 we found \(v_E = v_\varphi\), but that used the non-dispersive \(u\). The goal of this section is to find the correct \(\langle u\rangle\) and prove that

\[ \boxed{\;v_E = v_g\;} \]

for any lossless (or weakly lossy) dispersive medium.

15.9.2 Step 1: the stored energy in a dispersive medium (Brillouin)

15.9.2.1 Quasi-monochromatic field

Energy density only makes sense for a field that is switched on and evolves, so consider a carrier at frequency \(\omega\) with a slowly varying complex envelope \(\tilde{\mathbf{E}}(t)\):

\[ \mathbf{E}(t) = \mathrm{Re}\!\left[\tilde{\mathbf{E}}(t)\,e^{-i\omega t}\right], \qquad \left|\frac{d\tilde{\mathbf{E}}}{dt}\right| \ll \omega\,|\tilde{\mathbf{E}}| . \]

“Slowly varying” means the envelope changes little during one optical period, i.e. the spectrum of \(\tilde{\mathbf{E}}\) is concentrated in a narrow band \(\Omega \ll \omega\) around the carrier.

15.9.2.2 The response of the medium

Write the envelope as a superposition of small frequency offsets, \(\tilde{\mathbf{E}}(t) = \int \tilde{\mathbf{E}}(\Omega)\,e^{-i\Omega t}\,d\Omega\). Each component at \(\omega+\Omega\) is multiplied by \(\varepsilon(\omega+\Omega)\). Expanding to first order,

\[ \varepsilon(\omega+\Omega) \simeq \varepsilon(\omega) + \Omega\,\frac{d\varepsilon}{d\omega} . \]

Since \(\Omega\,e^{-i\Omega t} = i\,\dfrac{d}{dt}e^{-i\Omega t}\), the factor \(\Omega\) becomes \(i\,d/dt\) acting on the envelope:

\[ \tilde{\mathbf{D}}(t) \simeq \varepsilon\,\tilde{\mathbf{E}} + i\,\frac{d\varepsilon}{d\omega}\,\frac{d\tilde{\mathbf{E}}}{dt} , \qquad \mathbf{D}(t) = \mathrm{Re}\!\left[\tilde{\mathbf{D}}(t)\,e^{-i\omega t}\right]. \tag{15.18}\]

15.9.2.3 Averaging over one period

\[ \frac{\partial\mathbf{D}}{\partial t} = \mathrm{Re}\!\left[\left(\frac{d\tilde{\mathbf{D}}}{dt} - i\omega\tilde{\mathbf{D}}\right)e^{-i\omega t}\right]. \]

For two slowly varying phasors, \(\langle \mathrm{Re}[\mathbf{a}\,e^{-i\omega t}]\cdot\mathrm{Re}[\mathbf{b}\,e^{-i\omega t}]\rangle = \tfrac12\mathrm{Re}(\mathbf{a}^*\cdot\mathbf{b})\). Keeping terms to first order in \(d/dt\), using Equation 15.18:

\[ \frac{d\tilde{\mathbf{D}}}{dt} - i\omega\tilde{\mathbf{D}} \simeq -i\omega\varepsilon\,\tilde{\mathbf{E}} + \left(\varepsilon + \omega\frac{d\varepsilon}{d\omega}\right)\frac{d\tilde{\mathbf{E}}}{dt} . \]

Therefore

\[ \left\langle \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t}\right\rangle = \tfrac12\,\mathrm{Re}\!\left[-i\omega\varepsilon\,|\tilde{\mathbf{E}}|^2\right] + \tfrac12\,\frac{d(\omega\varepsilon)}{d\omega}\,\mathrm{Re}\!\left[\tilde{\mathbf{E}}^*\cdot\frac{d\tilde{\mathbf{E}}}{dt}\right]. \]

  • If \(\varepsilon\) is real (lossless), the first term vanishes.
  • In the second term, \(\mathrm{Re}[\tilde{\mathbf{E}}^*\cdot d\tilde{\mathbf{E}}/dt] = \tfrac12\,d|\tilde{\mathbf{E}}|^2/dt\).

So

\[ \left\langle \mathbf{E}\cdot\frac{\partial\mathbf{D}}{\partial t}\right\rangle = \frac{d}{dt}\left[\frac14\,\frac{d(\omega\varepsilon)}{d\omega}\,|\tilde{\mathbf{E}}|^2\right], \]

and identically for the magnetic term. The time-averaged stored energy density is the Brillouin formula:

\[ \boxed{\;\langle u\rangle = \frac14\left[\frac{d(\omega\varepsilon)}{d\omega}\,|\tilde{\mathbf{E}}|^2 + \frac{d(\omega\mu)}{d\omega}\,|\tilde{\mathbf{H}}|^2\right]\;} \tag{15.19}\]

For a non-dispersive medium, \(d(\omega\varepsilon)/d\omega = \varepsilon\) and we recover \(\langle u\rangle = \tfrac14(\varepsilon|E|^2 + \mu|H|^2)\), consistent with Equation 15.14.

NoteWhat about losses?

If \(\varepsilon = \varepsilon_R + i\varepsilon_I\), the first term no longer vanishes and gives \(\tfrac12\omega\varepsilon_I|\tilde{\mathbf{E}}|^2\), which is not a time derivative. It is a dissipation term, identical to \(\langle\mathbf{J}\cdot\mathbf{E}\rangle\) with an effective conductivity \(\sigma = \omega\varepsilon_I\), exactly as in Equation 15.15. The Brillouin formula is meaningful when \(\varepsilon_I \ll \varepsilon_R\), i.e. away from absorption lines.

15.9.3 Step 2: what the extra energy is (a check with the Lorentz model)

Why should the stored energy contain \(d\varepsilon/d\omega\)? Because in a material, part of the energy is mechanical energy of the bound charges. The polarization current \(\partial\mathbf{P}/\partial t\) is a current of real (bound) charges, so it does work \(\mathbf{E}\cdot\partial\mathbf{P}/\partial t\): this is the \(\mathbf{J}\cdot\mathbf{E}\) idea again, now hidden inside \(\mathbf{D}\).

Take the lossless Lorentz model: \(N\) oscillators per unit volume, charge \(q\), mass \(m\), resonance \(\omega_r\),

\[ m\ddot{x} = -m\omega_r^2 x + qE \quad\Rightarrow\quad x_0 = \frac{q E_0}{m(\omega_r^2-\omega^2)}, \qquad \varepsilon(\omega) = \varepsilon_0\left[1 + \frac{\omega_p^2}{\omega_r^2-\omega^2}\right], \qquad \omega_p^2 = \frac{Nq^2}{m\varepsilon_0}. \]

Mechanical energy of the oscillators, time-averaged:

\[ \langle u_\text{mech}\rangle = N\left\langle \tfrac12 m\dot{x}^2 + \tfrac12 m\omega_r^2 x^2\right\rangle = \frac14 N m(\omega^2+\omega_r^2)\,|x_0|^2 = \frac14\,\varepsilon_0\,\omega_p^2\,\frac{\omega_r^2+\omega^2}{(\omega_r^2-\omega^2)^2}\,|E_0|^2 . \]

Brillouin electric term:

\[ \frac{d(\omega\varepsilon)}{d\omega} = \varepsilon_0\left[1 + \omega_p^2\,\frac{\omega_r^2+\omega^2}{(\omega_r^2-\omega^2)^2}\right] \quad\Rightarrow\quad \frac14\,\frac{d(\omega\varepsilon)}{d\omega}\,|E_0|^2 = \underbrace{\frac14\varepsilon_0|E_0|^2}_{\text{vacuum field}} + \underbrace{\langle u_\text{mech}\rangle}_{\text{bound charges}} . \]

ImportantKey point 7

The Brillouin energy density is vacuum field energy plus the kinetic and potential energy of the bound charges that the wave sets in motion. The naive expression \(\tfrac14\varepsilon|E|^2\) misses the latter; it can even become negative where \(\varepsilon<0\), which is physically meaningless. For a passive lossless medium \(d(\omega\varepsilon)/d\omega > 0\) always (the electromagnetic analogue of Foster’s reactance theorem), so the Brillouin energy is always positive.

15.9.4 Step 3: proof that \(v_E = v_g\)

Take a plane wave in a lossless medium with real \(\varepsilon(\omega)\) and \(\mu(\omega)\). We use the prime for \(d/d\omega\) in this subsection only.

Energy flux. With \(|H_0| = |E_0|/\eta\) and \(\eta = \sqrt{\mu/\varepsilon}\):

\[ \langle S\rangle = \frac{|E_0|^2}{2\eta} = \frac12\sqrt{\frac{\varepsilon}{\mu}}\,|E_0|^2 . \]

Energy density. From Equation 15.19, with \(|H_0|^2 = (\varepsilon/\mu)|E_0|^2\):

\[ \langle u\rangle = \frac14|E_0|^2\left[(\varepsilon + \omega\varepsilon') + \frac{\varepsilon}{\mu}(\mu + \omega\mu')\right] = \frac{\varepsilon}{4}|E_0|^2\left[2 + \omega\frac{\varepsilon'}{\varepsilon} + \omega\frac{\mu'}{\mu}\right]. \]

Inverse group velocity. From \(k = \omega\sqrt{\mu\varepsilon}\):

\[ \frac{dk}{d\omega} = \sqrt{\mu\varepsilon} + \omega\,\frac{\mu\varepsilon' + \varepsilon\mu'}{2\sqrt{\mu\varepsilon}} = \frac{\sqrt{\mu\varepsilon}}{2}\left[2 + \omega\frac{\varepsilon'}{\varepsilon} + \omega\frac{\mu'}{\mu}\right]. \]

Compare. The same bracket appears in both. Eliminating it:

\[ \langle u\rangle = \frac{\varepsilon}{4}|E_0|^2\cdot\frac{2}{\sqrt{\mu\varepsilon}}\,\frac{dk}{d\omega} = \frac12\sqrt{\frac{\varepsilon}{\mu}}\,|E_0|^2\,\frac{dk}{d\omega} = \langle S\rangle\,\frac{dk}{d\omega} . \]

Hence

\[ \boxed{\;v_E = \frac{\langle S\rangle}{\langle u\rangle} = \frac{d\omega}{dk} = v_g\;} \tag{15.20}\]

ImportantKey point 8

In a dispersive, lossless medium, energy is transported at the group velocity, not at the phase velocity. The extra term \(\omega\,d\varepsilon/d\omega\) in the stored energy (the energy parked in the bound charges) is exactly what slows the energy down from \(v_\varphi\) to \(v_g\). In a non-dispersive medium the two coincide, which is why Equation 15.14 gave \(v_\varphi\).

15.9.5 How general is this?

The result is not limited to isotropic plane waves. For lossless systems it also holds for:

  • Anisotropic media. The energy velocity is the vector \(\mathbf{v}_E = \nabla_{\mathbf{k}}\,\omega(\mathbf{k})\), which in general is not parallel to \(\mathbf{k}\). This is why the ray direction and the wave-vector direction differ in birefringent crystals.
  • Waveguides. With \(\beta(\omega)\) the propagation constant of a mode, the ratio of guided power to energy per unit length equals \(d\omega/d\beta\), both in metallic waveguides and in dielectric (photonic) waveguides, where the dispersion comes from both material and geometry.
  • Periodic structures (photonic crystals, gratings). For Bloch modes, with flux and energy averaged over one unit cell, the energy velocity equals \(\nabla_{\mathbf{k}}\,\omega\) of the band. Near a band edge \(v_g\to 0\), which is the basis of slow-light devices.
  • Negative-index media. \(v_g\) is antiparallel to \(\mathbf{k}\), but \(\langle\mathbf{S}\rangle\) is antiparallel too: the equality still holds.

15.9.6 When it fails: the “weird cases”

The identification \(v_E = v_g\) rests on two assumptions: negligible loss and a first-order Taylor expansion of \(\varepsilon(\omega)\) over the pulse bandwidth. It breaks down when either fails.

  1. Near an absorption line (anomalous dispersion). There \(dn/d\omega < 0\), and \(v_g = c/n_g\) can exceed \(c\), become infinite or even negative. This does not violate causality: the medium reshapes the pulse by absorbing more of its trailing part, so the peak appears to advance, but no energy or information travels faster than \(c\). A proper energy velocity that includes the energy stored in and dissipated by the oscillators stays below \(c\) (Loudon, 1970). The front of a signal always travels at \(c\) (Sommerfeld and Brillouin).
  2. Strong higher-order dispersion. If \(\varepsilon(\omega)\) curves significantly over the pulse bandwidth, the pulse distorts and “the velocity of the pulse” is no longer well defined. The equality \(v_E = v_g\) still holds frequency by frequency, but \(v_g\) at the carrier no longer describes where the energy of the whole pulse is.
  3. Evanescent waves and tunnelling. When \(k\) is imaginary, \(d\omega/dk\) loses its meaning as a velocity; apparent superluminal tunnelling times (the Hartman effect) are another manifestation.
TipFor a classroom

A good conceptual summary: phase velocity is how fast the crests move, group velocity is how fast the envelope moves, and in a transparent medium the energy rides with the envelope. The “weird cases” are all situations where the medium is not transparent, or where the envelope itself stops being a well-defined object.

15.10 Radiation: energy that never comes back

For a localised oscillating source (an antenna), the fields far away decrease as \(1/r\). Then \(|\mathbf{S}|\propto 1/r^2\), and the power through a sphere of radius \(r\),

\[ P = \oint_{r}\mathbf{S}\cdot d\mathbf{a} \;\propto\; \frac{1}{r^2}\cdot r^2 = \text{constant}, \]

does not depend on \(r\). The same power crosses every sphere, however large: energy leaves the source and never returns. This is what distinguishes a radiated wave from the near-field terms, which decrease faster than \(1/r\) and only exchange energy back and forth with the source.

15.11 Experimental confirmation

The argument above is theoretical. Experiments confirm it in two independent ways.

  • Heating. An absorber (bolometer, thermopile, optical power meter) placed in a beam warms up. Its temperature rise gives the absorbed power, and it matches \(\oint\mathbf{S}\cdot d\mathbf{a}\).
  • Radiation pressure. The field also carries momentum, with density \(\mathbf{S}/c^2\). A beam of power \(P\) exerts a force \(P/c\) on an absorber and \(2P/c\) on a mirror. This was measured by Lebedev (1900) and by Nichols and Hull (1901 to 1903).

15.12 Summary

ImportantThe logic in seven steps
  1. Energy is defined by work on matter. The fields do work on charges at the rate \(\mathbf{J}\cdot\mathbf{E}\) per unit volume.
  2. Maxwell’s equations imply Poynting’s theorem, \(\partial_t u + \nabla\cdot\mathbf{S} = -\mathbf{J}\cdot\mathbf{E}\). Where charges are present, the budget identifies \(u\) and \(\mathbf{S}\) as energy density and energy flux.
  3. In vacuum, \(\mathbf{J}=0\) and the theorem becomes a continuity equation: the same quantity \(u\) is conserved and flows with flux \(\mathbf{S}\). It is energy because it is the same \(u\) that was identified at the source.
  4. Pulse argument. While a pulse is between transmitter and receiver, the transmitter has lost energy and the receiver has gained none. Energy conservation at every instant requires the energy to be in the field.
  5. Plane waves. Faraday gives \(E/B = \omega/k\) and Ampère–Maxwell fixes \(\omega/k = 1/\sqrt{\mu\varepsilon}\); electric and magnetic energies are equal.
  6. Absorbers. In a lossy medium, the decrease of \(\mathbf{S}\) with depth equals the Joule heating \(\mathbf{J}\cdot\mathbf{E}\): the field’s energy is handed over to matter.
  7. Dispersive media. The stored energy includes the energy of the bound charges (Brillouin), and energy travels at the group velocity, \(v_E = d\omega/dk\), except near absorption lines and in other strongly non-transparent situations.

15.13 Questions for discussion

Because \(q(\mathbf{v}\times\mathbf{B})\cdot\mathbf{v}=0\): the magnetic force is always perpendicular to the velocity. The magnetic field still stores energy (\(B^2/2\mu_0\)) and contributes to \(\mathbf{S}\), but it transfers energy to matter only indirectly, through the electric field it induces.

No. It becomes a continuity equation, which shows that \(u\) is conserved locally and flows with flux \(\mathbf{S}\). What it cannot do by itself is tell us that \(u\) is energy; that identification comes from regions with charges.

No. It contains no moving charges and contributes to \(\partial u/\partial t\) (change of stored field energy), not to \(\mathbf{J}\cdot\mathbf{E}\) (work on matter).

So that there is a finite time interval in which the transmitter has completely stopped and the receiver has not yet been reached. During that interval no matter anywhere holds the missing energy, which makes the contradiction unavoidable.

See Section 15.7. The ratio of flux to density has dimensions of velocity: it is the speed at which energy is transported, here \(c\).

Mainly magnetic: \(\langle u_B\rangle/\langle u_E\rangle = \sqrt{1+(\sigma/\omega\varepsilon)^2} \gg 1\). The conduction current \(\sigma E\) is much larger than the displacement current, so a small \(E\) sustains a large \(H\) through Ampère’s law.

Because \(\mathbf{D}(t)\) depends on the past values of \(\mathbf{E}\), so \(\mathbf{E}\cdot\partial_t\mathbf{D}\) is not the time derivative of \(\tfrac12\varepsilon E^2\). Physically, the formula ignores the kinetic and potential energy of the bound charges driven by the wave (Section 15.9).

\(v_\varphi = \omega/\beta = c/\sqrt{1-\omega_c^2/\omega^2} > c\) and \(v_g = d\omega/d\beta = c\sqrt{1-\omega_c^2/\omega^2} < c\), with \(v_\varphi v_g = c^2\). The energy travels at \(v_g\); the phase velocity exceeding \(c\) carries no energy or information.

No. The medium absorbs the trailing part of the pulse more strongly, which moves the peak forward without any energy getting ahead of the front. The assumptions behind \(v_E = v_g\) (negligible loss, slowly varying \(\varepsilon\) over the bandwidth) fail there.