Anisotropic Dielectrics and the Permittivity Tensor
Set a clear calcite crystal on a printed page and you see two copies of every letter. Rotate the crystal and one copy circles the other. Nothing in the last eighteen articles can explain this: we have treated every dielectric as if it responded to a field the same way in every direction, one number per material. Calcite refuses. Its carbonate groups all lie in parallel planes, so bound charge slides easily within those planes and reluctantly across them. Push with a field at an angle and the medium pushes back in a different direction — the polarization, and with it , tilts away from . This article closes the dielectrics chapter by making that direction-dependence precise. The single number grows into a matrix — the permittivity tensor — and everything we know follows it: why energy conservation forces the tensor to be symmetric, how diagonalization hands every crystal a natural frame of principal axes with just three numbers, and how lattice symmetry prunes those numbers down (cubic crystals, remarkably, back to one). The microscopic ingredients are already on our shelf: the molecular polarizability tensor promised in Induced Dipoles and Atomic Polarizability, and the fragile lattice sum of Local Field and the Lorentz Cavity, whose failure under a 5% tetragonal stretch was anisotropy announcing itself. Master the tensor and you hold the static foundation of crystal optics — birefringence, wave plates, the liquid-crystal pixel you are probably reading this on — and the vocabulary (principal axes, eigenvalues, quadratic forms) the rest of physics reuses for inertia, stress, and conductivity.
- In a crystal the dielectric response depends on direction: with a permittivity tensor, and is generally not parallel to .
- Energy bookkeeping forces the tensor to be symmetric, , for any lossless, non-gyrotropic medium — otherwise you could harvest energy by cycling the field.
- A real symmetric tensor can always be rotated to diagonal form: the eigenvectors are the crystal's principal axes, the eigenvalues its three principal permittivities .
- Crystal symmetry prunes the count: triclinic keeps 6 independent components, orthorhombic 3 (biaxial), tetragonal/hexagonal/trigonal 2 (uniaxial), cubic exactly 1 — a cubic crystal is optically isotropic, by theorem not by accident.
- In calcite (, at optical frequency) a field at to the optic axis produces a tilted away from — the static seed of double refraction.
- The energy density is still ; its constant-energy surfaces are ellipsoids whose semi-axes encode the principal indices .
- Key idea: in an anisotropic dielectric the linear response is a tensor relation ; symmetry lets you rotate to principal axes where three numbers — and the geometry of an ellipsoid — carry all the physics.
In an anisotropic dielectric the linear response is a tensor relation ; the symmetry lets you rotate to principal axes where the tensor is diagonal, reducing the physics to three principal permittivities and their refractive indices.
Where this lives today
The permittivity tensor is the most commercially deployed object in this chapter. Every liquid-crystal display pixel is a vat of rod-like molecules forming a tunable uniaxial dielectric: the nematic director (the local optic axis) reorients in an applied field because the molecules' makes alignment energetically favorable, and the reoriented tensor then rotates the polarization of transmitted light between crossed polarizers. A billion screens steer their tensors, pixel by pixel, sixty times a second. At the engineering frontier the game is designing rather than accepting what nature grows. Metamaterials assemble sub-wavelength cells whose effective tensors take values no crystal offers, including principal values of opposite sign (hyperbolic media); transformation optics runs our chapter backwards — choose the field pattern you want and solve for the spatially varying tensor that produces it. Even the humble circuit board participates: woven fiberglass laminate is measurably biaxial, and high-speed designers route differential pairs at an angle to the weave to dodge the resulting skew.
The physical picture
Picture a bound electron in a crystal as a mass caged by springs — stiff springs along one crystallographic direction, soft springs along another. A field applied exactly along a spring direction stretches only those springs, and the induced dipole points along the field. But push at and the charge cheats: it slides farther along the soft direction than the stiff one, so the dipole moment — and, summed over the lattice, the polarization — leans away from toward the compliant axis. The permittivity tensor is nothing more than the bookkeeping matrix of these direction-dependent stiffnesses.
Both microscopic ingredients of this cage are already on our shelf. Induced Dipoles and Atomic Polarizability warned that for anything less symmetric than a sphere, is itself a tensor — a CO molecule polarizes about twice as easily along its O=C=O axis as across it, a debt we pay in full below. And Local Field and the Lorentz Cavity showed that even perfectly isotropic molecules acquire an anisotropic response from an anisotropic lattice: the near-field sum that vanishes identically on a cubic lattice revives at the 14% level under a mere 5% tetragonal stretch, turning the local-field correction — and hence the susceptibility — into a direction-dependent object. Molecular shape and lattice geometry are the two roads into the tensor; most real crystals travel both. The theme of this article is that the tensor is far tamer than nine arbitrary numbers. Energy conservation makes it symmetric; symmetry makes it diagonalizable; and the crystal's own point symmetry then squeezes the three surviving eigenvalues, sometimes all the way back to one.
From molecule to crystal: the tensor law
For an isotropic linear dielectric we wrote , one scalar multiplying the total macroscopic field. To let the medium respond differently in different directions, we keep linearity — still valid for the small-field Taylor reasons of Linear Dielectrics, Susceptibility and Permittivity — but promote the single coefficient to a matrix,
where: — components of the polarization density (C/m²); — components of the total macroscopic field, the repeated index summed over ; — the electric susceptibility tensor, nine dimensionless numbers. Read it as a machine: feed in a field along and the column tells you the polarization it produces, off-axis components included. Diagonal recovers the isotropic case exactly. The displacement keeps its universal definition — that equation, from The Electric Displacement D, is bookkeeping and holds in any medium whatsoever. Only the constitutive link closing the equations changes:
where: — the permittivity tensor (F/m); — the Kronecker delta carrying the vacuum part. Because need not be proportional to , and point in different directions unless lies along one of the special directions we construct below. Gauss's law in dielectrics is untouched: cares only about 's divergence, not about which way it leans relative to . Where do the nine come from? Sum the microscopic responses, as in the isotropic chapter but keeping directions. If each molecule carries a polarizability tensor (so ) and sits in a lattice whose local-field correction is itself directional, inherits anisotropy from both factors. For CO: along the molecular axis versus across it (polarizability volumes and ) — two-to-one anisotropy in a single molecule. In the gas this washes out: tumbling molecules present the average and the bulk stays isotropic, as we verify numerically in the worked examples. Freeze the same molecules into an ordered lattice and the anisotropy survives to the macroscale — that is the crystal.
Why the tensor must be symmetric
Nine components suggest nine material constants. Thermodynamics immediately strikes three: for any medium that stores field energy without loss, . This is not a convenience assumption — its violation would let you build a perpetual-motion machine out of a capacitor, and the derivation shows exactly how.
We want to show that for any lossless dielectric, using nothing but the energy ledger of Energy Stored in Dielectric Systems. The strategy is the same exact-differential argument that proves conservative forces have curl zero: charge the crystal to the same final field along two different paths in "field space," demand that the work invested be the same, and see what that forces on the tensor. Watch for where losslessness enters — a medium that dissipates is under no such obligation, which is why absorbing and gyrotropic media escape the theorem.
Step 1. The work delivered per unit volume by the sources while the displacement grows by is — this is the same increment we integrated to get in the isotropic chapter, and its derivation (trickling free charge onto conductors) nowhere assumed . With linear, . Why field space? The state of the dielectric is specified by the three numbers . Charging the crystal is a path from the origin to the final field in this abstract space, and is the line integral of along that path.
Step 2. Charge to the final state two ways. Path A: raise from to first (cost ), then raise from to while sits fixed (cost , the cross term because the -field rides along while shifts). Path B: same moves in the opposite order, giving the cross term instead.
Step 3. Subtract: . If this is nonzero, run path A forward and path B backward: the field returns to zero, the dielectric is exactly as it started, yet the cycle has handed the external circuit the energy — a machine that mints energy from nothing, every cycle. Why losslessness is the premise. In an absorbing medium the state at the end of a cycle is not the initial state (heat has been generated), so path-independence is not required and the argument stops. Formally becomes complex; a static magnetic field (Faraday-active media) adds an antisymmetric part while remaining lossless because breaks time-reversal — both escape the theorem honestly.
Step 4. Forbidding the free lunch forces , and the identical argument in the other two coordinate planes gives : six independent components, not nine. Equivalently, is an exact differential and exists as a state function, with symmetric because mixed partials commute. Verified numerically: charging to V/m through a symmetric test tensor () costs J/m³ along both paths (equal to 6 digits); repeating with an asymmetric tensor of the same symmetric part (, ) gives vs J/m³ — a cycle would harvest J/m³ per lap, the advertised perpetual-motion machine.
With symmetry in hand, the energy density itself comes along for free. Since is exact precisely when the tensor is symmetric, it integrates to
where: — electrostatic energy density (J/m³), a positive-definite quadratic form for any passive dielectric. The familiar of the isotropic chapter survives verbatim — with the scalar product now doing real work, because the two vectors are no longer parallel. The which-energy honesty of Energy Stored in Dielectric Systems also carries over unchanged: this is the free-charge ledger, springs included.
Principal axes: the crystal's own frame
A real symmetric matrix is the friendliest object in linear algebra: it can always be diagonalized by a pure rotation. Physically, every crystal — however low its symmetry — hides three mutually perpendicular directions along which the response is parallel to the push.
Go deeper · Derivation B · 2 minPrincipal axes and the energy ellipsoid
We want to show that there exists an orthogonal frame in which is diagonal, and to extract the geometry that frame carries: constant-energy surfaces that are ellipsoids whose axes encode the three principal permittivities. The route is the spectral theorem, but we walk it concretely — via the quadratic form — because that is the version that generalizes to the inertia tensor and the stress tensor later in the curriculum. Watch for why symmetry is indispensable: an asymmetric matrix need not be diagonalizable by any rotation.
Step 1. Consider the energy on the sphere . A continuous function on a sphere attains a maximum; call the maximizing direction . At a constrained maximum the gradient of must be parallel to the constraint normal: . The maximizing direction is therefore an eigenvector — a direction where exactly, response parallel to push.
Step 2. Here symmetry earns its keep: for symmetric , the subspace perpendicular to is mapped into itself. Take any ; then — the first equality is exactly . So we can repeat Step 1 inside the perpendicular plane to find , and follows as the remaining normal. Three mutually orthogonal eigenvectors exist. Why an asymmetric tensor fails. Without the perpendicular subspace leaks — acquires a component along — and the construction stalls after one step. Orthogonal principal axes are a privilege of symmetric tensors.
Step 3. In the frame the tensor is : the three eigenvalues are the principal permittivities, all positive for a passive dielectric (each is along its axis). The whole machine reduces to component-by-component multiplication: , , . Every anisotropic problem strategy in this subject is now visible: rotate in, scale, rotate out.
Step 4. The geometry: in the principal frame the constant-energy condition reads , an ellipsoid in -space with semi-axes . Re-expressed in (using ), — an ellipsoid whose semi-axes are , i.e. proportional to the principal refractive indices . Normalized, this -space ellipsoid is the index ellipsoid of crystal optics; here it is simply the level surface of our energy ledger. Verified: for (calcite) and at 45 deg with V/m, the three routes to the energy — the quadratic form , the dot product , and — all give J/m³.
One geometric consequence is worth carrying in your head: since , points along the normal to the constant- ellipsoid at the tip of — and an ellipse's normal is parallel to its radius only on the axes. That is the picture behind every walk-off angle we compute:
What crystal symmetry does to the tensor
Six independent components is the worst case — triclinic, no symmetry beyond the lattice itself. Every symmetry operation the crystal possesses is a constraint, by Neumann's principle: a macroscopic property tensor must be invariant under every point-symmetry operation of its crystal, for each symmetry rotation or reflection — the property cannot be choosier than the crystal that hosts it. The payoff is a complete classification, and one genuinely surprising theorem.
Go deeper · Derivation C · 2 minHow symmetry prunes the tensor and why cubic crystals are exactly isotropic
We want the count of independent permittivity components for each crystal family, and in particular the cubic surprise: a crystal with manifestly special directions (a cube's edges are nothing like its diagonals) whose dielectric response is nonetheless perfectly isotropic. The strategy is to apply Neumann's principle operation by operation, starting from the general symmetric tensor with entries . The thing to watch is what each symmetry kills: reflections and 2-fold axes kill off-diagonals; higher-fold axes go further and equate diagonals.
Step 1. Orthorhombic (three perpendicular 2-fold axes): a 180° rotation about sends , so and ; invariance forces both to vanish. The -axis rotation kills . The tensor is diagonal in the crystallographic frame with three distinct entries — the crystal axes are the principal axes, and the crystal is biaxial: 3 independent components.
Step 2. Tetragonal, hexagonal, trigonal (one axis of order , along ): invariance under rotation by about requires the block in the -plane to commute with a non-trivial rotation. A symmetric matrix invariant under rotation by anything other than must be proportional to the identity — its two eigenvalues would otherwise pick out two special perpendicular directions in the plane, which the -fold axis forbids. Hence , off-diagonals zero, free: 2 independent components, the uniaxial family, with the -fold axis as the optic axis. Why order 3 already suffices. A 3-fold axis rotates by 120°; the only symmetric tensors unmoved by 120° in a plane are isotropic in that plane. This is why trigonal calcite is uniaxial even though its symmetry looks "lower" than tetragonal.
Step 3. Cubic: the -axis 4-fold makes the block isotropic as in Step 2, so ; but a cube has equivalent 4-fold axes along and too, forcing by the same argument. All three eigenvalues coincide: , one independent component. Rock salt, diamond, and silicon are dielectrically indistinguishable from glass — every direction, not just the symmetry directions, sees the same , because a symmetric tensor with three equal eigenvalues is a multiple of the identity, full stop. Why the cube's "special directions" leave no trace. The permittivity tensor is a quadratic-form probe — it can only distinguish directions by assigning them different eigenvalues, and the cube's symmetry leaves no room for unequal eigenvalues. Cubic anisotropy is real but invisible at rank 2; it resurfaces in rank-4 properties like elasticity, where single-crystal silicon is measurably direction-dependent.
Step 4. The census: triclinic 6, monoclinic 4 (its single 2-fold kills two off-diagonals), orthorhombic 3 (biaxial: mica, topaz), tetragonal/hexagonal/trigonal 2 (uniaxial: quartz, calcite, rutile), cubic 1 (isotropic: NaCl, diamond). Melt or powder any of them and orientational averaging returns the scalar — which is why this entire chapter could ignore the tensor until its final article. Verified: the counts 6/4/3/2/1 match Nye's standard crystallographic tables (Physical Properties of Crystals, Table 3), and the uniaxial assignments match the handbook data quoted below.
Anchor numbers, at 589 nm where the anisotropic tensor is best tabulated: calcite is negative uniaxial with , (, ); quartz is weakly positive (, ); rutile dramatically so (, ). One honesty note from Linear Dielectrics: is the optical-frequency tensor. At DC the ionic lattice adds its own stretch response — calcite's static values sit near and — and the full frequency story is dispersion, deferred to the waves chapter.
Limiting cases
| Case | Result | Meaning |
|---|---|---|
| Isotropic / cubic | , always | The whole chapter until now; also any melt, glass, gas, or powder by orientational averaging. |
| along a principal axis | , walk-off | Anisotropy hides: each axis behaves as an ordinary scalar dielectric with its own . |
| Uniaxial () | one optic axis; | Calcite at : leans from ; maximum at . |
| Weak anisotropy () | rad | Quartz's index split gives walk-off of only — why calcite, not quartz, shows double images to the naked eye. |
| Lossy or magneto-active medium | complex / non-symmetric | The energy theorem's premise fails; Hermitian and gyrotropic parts appear (Faraday effect) — beyond statics. |
Worked examples
Example 1 — calcite: how far does D lean? A slab of calcite carries a uniform field V/m at to the optic axis (optical-frequency tensor: , ). Find , the walk-off angle, and the stored energy density.
Step 1. Set up in the principal frame, optic axis along , field in the -plane: V/m, V/m.
Step 2. Apply the diagonal tensor component by component: C/m², and C/m². The magnitude is C/m².
Step 3. Direction of : , so — the displacement leans toward the easy plane. The walk-off angle is 6.2°. (Sweeping shows the lean maximizes at for , the analytic maximum with .)
Step 4. Energy density: 0.439 J/m³. Cross-checks: the quadratic form and the projection give the same J/m³ — the is the anisotropy tax on the naive .
Example 2 — CO2, from one molecule to a gas. The CO polarizability tensor has C·m²/V along the molecular axis and C·m²/V across it. (a) A field V/m is applied at to a molecule's axis — where does point? (b) Predict the dielectric constant of CO gas at 20 °C, 1 atm, and compare with the measured .
Step 1. Single molecule, principal frame along the O=C=O axis: C·m, C·m. Direction: , so sits from the axis — tilted away from , toward the easy axis. A single molecule is a miniature calcite.
Step 2. In the gas the molecules tumble, and the orientation average of the tensor is the scalar C·m²/V — one soft axis, two stiff ones, weighted equally. The macroscopic response is isotropic even though no single molecule is.
Step 3. Number density at 20 °C, 1 atm: m⁻³. The gas is dilute enough () that the Clausius–Mossotti denominator is negligible and .
Step 4. Prediction: 1.000916, against the measured — agreement to better than 1% of the susceptibility. The anisotropy has not vanished, only hidden: light scattered from the gas is measurably depolarized because individual molecules still respond off-axis, which is exactly how is measured. Freeze the gas into an oriented crystal and the tilt of Step 1 would survive to the macroscale.
A crystal's history
Origins · 1 minAugustin-Jean Fresnel and how this was discovered
Fresnel built the physics of anisotropic media a full generation before anyone could write a tensor. Working from Bartholin's double images and Huygens's two wavefronts in calcite, he made the decisive leap in 1821: light is a transverse vibration, so a crystal can assign different speeds to different vibration directions. From that single idea he reduced every known crystal-optical effect to three principal velocities along three perpendicular axes — principal-axis decomposition of a symmetric tensor, discovered as geometry seventy-seven years before Voigt coined the word "tensor" for exactly this kind of object. A road engineer who did optics between postings and died at 39, Fresnel is why the index ellipsoid, the walk-off construction, and the uniaxial index formula all carry his fingerprints.
Going further
References. Griffiths, Introduction to Electrodynamics, 4th ed., §4.4 (linear dielectrics; anisotropic remark) · Jackson, Classical Electrodynamics, 3rd ed., §4.5 and §7.10 (crystal optics) · Zangwill, Modern Electrodynamics, §6.5 (dielectric tensor) · Born & Wolf, Principles of Optics, Ch. 15 (crystal optics, index ellipsoid) · Landau & Lifshitz, Electrodynamics of Continuous Media, §13, §97-98 · Nye, Physical Properties of Crystals, Ch. 1-3 (Neumann's principle, tensor census)
Provenance. Tensor constitutive relation, symmetry from energy, diagonalization, index ellipsoid, and the uniaxial Fresnel equation follow Jackson §4.5 & §7.10, Born & Wolf Ch. 15, and Landau-Lifshitz ECM §13,97. Verifier should recompute: (1) symmetry of from exactness of ; (2) the uniaxial index formula from the plane-wave wave equation; (3) calcite values , at 589 nm (standard handbook values); (4) the component counts (cubic 1, uniaxial 2, biaxial 3) against Nye's crystal-symmetry tables.
Builds on: Linear Dielectrics, Susceptibility and Permittivity · The Electric Displacement D · Polarization Density P · Induced Dipoles and Atomic Polarizability · Gauss's Law in Dielectrics · Local Field and the Lorentz Cavity Leads to: Boundary Conditions for D and E · Magnetostatics (the chapter that opens next) · Birefringence and Crystal Optics · Electro-optic Effect (Pockels and Kerr)
Is D still defined as eps0 E + P in a crystal, or does the tensor replace that definition?
The definition never changes: is pure bookkeeping and holds in every medium. What the tensor replaces is only the constitutive link — the material's answer to "what P does this E produce?", which was and is now . Everything built on the definition alone — , the pillbox condition on , bound-charge formulas — survives untouched.
If D and E point in different directions, which one do I trust for Gauss's law and field lines?
Both, for their own jobs. still holds exactly, so -lines begin and end only on free charge; still holds in statics, so remains the gradient of a potential. The novelty is that these are now genuinely different vector fields whose line maps do not coincide. The Gauss's Law in Dielectrics ritual still works for , but its last step becomes the matrix solve .
How can a cubic crystal be isotropic when a cube obviously has special directions?
The cube's specialness is real but invisible to a rank-2 tensor, which can only express anisotropy by giving different eigenvalues to different directions — and the cube's rotations force all three equal. After that, every direction (edge, face diagonal, body diagonal) gives identically. Higher-rank properties have more room: the rank-4 elastic tensor of cubic silicon keeps three independent constants and is measurably anisotropic, which is why wafer flats mark crystal orientation even though silicon's permittivity is a scalar.
My handbook lists refractive indices, not permittivities. How do I get the tensor from n_o and n_e?
At optical frequencies along each principal axis, so calcite's , give , — the values used throughout this article. The honesty clause: that is the electronic response only. At low frequency the ionic lattice also stretches, and calcite's static tensor is near — three times the optical values. Which tensor you need depends on which field you apply; the frequency dependence (and why only at matching frequencies) is the dispersion story of the waves chapter.
Does an anisotropic crystal have a permanent polarization?
Not by virtue of anisotropy alone. The susceptibility tensor describes response: switch the field off and returns to zero, however anisotropic may be. Spontaneous polarization is a stronger condition — it needs a polar crystal class, the subject of Ferroelectrics and Spontaneous Polarization. The properties do interact: all ferroelectrics are strongly anisotropic, but most anisotropic crystals (calcite, quartz) are not ferroelectric.
Where does the number six come from for the general tensor?
Count the entries of a symmetric matrix: three diagonal plus three independent off-diagonal (each equal to its mirror partner) — six. The energy argument cut nine to six; crystal symmetry then cuts to 3 (orthorhombic), 2 (uniaxial), or 1 (cubic). Six is also why a triclinic crystal needs its principal axes found by diagonalization: nothing in the lattice hands them to you.
Is the 6-degree walk-off in the worked example the same thing as birefringence?
Same root, different phenomena. We computed the static misalignment of and . Birefringence is the wave consequence: a wave in a uniaxial crystal splits into two polarizations with different indices ( and ), and the extraordinary ray's energy walks off from its wavefront normal by an angle governed by exactly our . The calcite double image is the wave phenomenon; its size is set by the static tensor computed here. The full machinery — index-ellipsoid slicing, the Fresnel equation, wave plates — is crystal optics in the electromagnetic-waves chapter, where we hand this off.