Intuition What this page is for
The parent note gave you the machinery: the ordinary index n o , the direction-dependent extraordinary index n e ( θ ) , and the phase-lag Δ ϕ that builds wave plates. Here we stress-test that machinery against every case it can throw at you — angle = 0 , angle = 9 0 ∘ , in-between angles, positive vs negative crystals, degenerate inputs, and a word problem. If you can do all ten below, no exam question on this topic can surprise you.
Everything here uses only what the parent built. The one formula we lean on constantly:
Cell
Case class
What is special
Example
A
θ = 0 ∘ (along optic axis)
degenerate: no splitting, n e ( θ ) = n o
Ex 1
B
θ = 9 0 ∘ (across optic axis)
limiting: maximum splitting, n e ( θ ) = n e
Ex 2
C
general 0 < θ < 9 0 ∘
index interpolates between n o and n e
Ex 3
D
negative crystal (n e < n o )
n e ( θ ) rises with θ … wait, falls — sign check
Ex 3, Ex 4
E
positive crystal (n e > n o )
n e ( θ ) increases with θ ; opposite trend
Ex 4
F
degenerate crystal (n e = n o )
isotropic: birefringence vanishes for all θ
Ex 5
G
phase / wave-plate design (Δ ϕ )
pick thickness d for a target retardation
Ex 6, Ex 7
H
walk-off angle (e-ray bends off k ^ )
the "extraordinary" bending itself
Ex 8
I
real-world word problem
Nicol-prism style separation choice
Ex 9
J
exam twist (solve backwards for θ )
given the index, find the angle
Ex 10
Read the matrix as a checklist. Each example below names the cell(s) it clears.
Worked example Example 1 — Cell A: propagation
along the optic axis (θ = 0 ∘ )
Calcite: n o = 1.658 , n e = 1.486 . What index does the e-ray feel when it travels straight down the optic axis?
Forecast: Along the optic axis the crystal is defined to have no birefringence. So guess: both rays feel the same index. Which one?
Step 1. Put θ = 0 into the workhorse:
n e ( 0 ) 2 1 = n o 2 c o s 2 0 ∘ + n e 2 s i n 2 0 ∘ = n o 2 1 + 0.
Why this step? cos 0 ∘ = 1 and sin 0 ∘ = 0 — travelling straight down the axis means "all along, none across", so the n e term switches completely off.
Step 2. Therefore n e ( 0 ) = n o = 1.658 .
Why this step? Inverting 1/ n e ( 0 ) 2 = 1/ n o 2 gives n e ( 0 ) = n o directly.
Verify: The e-ray index equals the o-ray index, so the two rays travel at the same speed and never separate — precisely the definition of the optic axis. ✅
Worked example Example 2 — Cell B: propagation
across the optic axis (θ = 9 0 ∘ )
Same calcite. What index does the e-ray feel travelling perpendicular to the optic axis?
Forecast: This is the "most anisotropic" direction. Guess: the index reaches its extreme principal value n e .
Step 1. Put θ = 9 0 ∘ :
n e ( 9 0 ∘ ) 2 1 = n o 2 c o s 2 9 0 ∘ + n e 2 s i n 2 9 0 ∘ = 0 + n e 2 1 .
Why this step? cos 9 0 ∘ = 0 , sin 9 0 ∘ = 1 — now it's "all across, none along", so the n o term vanishes.
Step 2. n e ( 9 0 ∘ ) = n e = 1.486 .
Verify: The gap between the two rays is now ∣ n o − n e ∣ = ∣1.658 − 1.486∣ = 0.172 — the largest possible. Maximum splitting, as promised. ✅
Worked example Example 3 — Cell C & D: a general angle in a
negative crystal (θ = 3 0 ∘ )
Calcite (n e < n o , negative). Find n e ( 3 0 ∘ ) .
Forecast: The answer must sit between 1.486 and 1.658 . Because calcite is negative, as θ grows from 0 to 9 0 ∘ the index should slide down from 1.658 toward 1.486 . So at 3 0 ∘ expect a value nearer the top of that range.
Step 1. cos 2 3 0 ∘ = 0.75 , sin 2 3 0 ∘ = 0.25 .
Why this step? cos 3 0 ∘ = 2 3 so cos 2 = 4 3 ; the two must add to 1 , giving sin 2 = 4 1 .
Step 2. n o 2 = 1.65 8 2 = 2.749 , n e 2 = 1.48 6 2 = 2.208 .
Step 3.
n e ( 3 0 ∘ ) 2 1 = 2.749 0.75 + 2.208 0.25 = 0.2728 + 0.1132 = 0.3860.
Why this step? Straight substitution of the two ratios.
Step 4. n e ( 3 0 ∘ ) = 1/ 0.3860 = 1.609 .
Verify: 1.486 < 1.609 < 1.658 ✅, and 1.609 is closer to 1.658 than the 4 5 ∘ answer (1.565 from the parent note) — the index really does slide downward as θ increases in a negative crystal. ✅
Worked example Example 4 — Cell E: a
positive crystal, opposite trend (θ = 3 0 ∘ , quartz)
Quartz: n o = 1.544 , n e = 1.553 (positive, n e > n o ). Find n e ( 3 0 ∘ ) and state which way the index trends.
Forecast: Now n e > n o , so as θ grows the index should climb up from 1.544 toward 1.553 . Expect a value just above 1.544 .
Step 1. cos 2 3 0 ∘ = 0.75 , sin 2 3 0 ∘ = 0.25 (same trig as Ex 3).
Step 2. n o 2 = 1.54 4 2 = 2.3839 , n e 2 = 1.55 3 2 = 2.4118 .
Step 3.
n e ( 3 0 ∘ ) 2 1 = 2.3839 0.75 + 2.4118 0.25 = 0.31462 + 0.10366 = 0.41828.
Step 4. n e ( 3 0 ∘ ) = 1/ 0.41828 = 1.5462 .
Verify: 1.544 < 1.5462 < 1.553 ✅. So for a positive crystal the e-index rises with θ — the mirror image of calcite. The sign of Δ n = n e − n o tells you the direction of travel of the curve. ✅
Worked example Example 5 — Cell F: the degenerate crystal (
n e = n o )
Suppose a crystal has n o = n e = 1.60 (an accidentally isotropic case). Find n e ( θ ) for any θ .
Forecast: If both principal indices are equal, the "lopsidedness" is gone. Guess: one index for every direction, no splitting anywhere.
Step 1. With n o = n e = n :
n e ( θ ) 2 1 = n 2 c o s 2 θ + n 2 s i n 2 θ = n 2 c o s 2 θ + s i n 2 θ = n 2 1 .
Why this step? cos 2 θ + sin 2 θ = 1 is always true (Pythagoras on the unit circle), so the θ -dependence collapses.
Step 2. n e ( θ ) = n = 1.60 for all θ .
Verify: No angle gives splitting — this is just ordinary glass. The formula correctly reduces to the isotropic case, which is exactly what "birefringence needs two distinct indices" demanded. ✅ (See Dielectric tensor and anisotropic media for why equal diagonal entries mean isotropy.)
Worked example Example 6 — Cell G: half-wave plate thickness for calcite
At λ = 589 nm, using principal indices (θ = 9 0 ∘ , so ∣Δ n ∣ = 0.172 ), find the thinnest thickness d giving a half-wave retardation, Δ ϕ = π .
Forecast: A half-wave plate flips polarization; it needs twice the retardation of a quarter-wave plate (parent Ex 3 gave 856 nm for π /2 ). Guess: about 2 × 856 ≈ 1712 nm.
Step 1. The phase difference after thickness d is Δ ϕ = λ 2 π ∣Δ n ∣ d .
Why this step? The two rays travel the same physical distance d but at different speeds; the optical-path gap is ∣Δ n ∣ d , and each wavelength of gap is 2 π of phase.
Step 2. Set Δ ϕ = π and solve: d = 2∣Δ n ∣ λ .
Step 3. d = 2 ( 0.172 ) 589 × 1 0 − 9 = 1.712 × 1 0 − 6 m = 1712 nm.
Verify: Units: (dimensionless) m = m ✅. And it is exactly twice the quarter-wave value — consistent with Wave plates (quarter and half wave) . ✅
Worked example Example 7 — Cell G twist: retardation of a
given plate
A calcite plate is d = 2.0 μ m thick, principal indices, λ = 589 nm. What is Δ ϕ , and is it a "clean" wave plate?
Forecast: 2.0 μ m is a bit more than the half-wave value (1712 nm). So Δ ϕ should be a bit more than π . Guess: around 1.1 π to 1.2 π .
Step 1. Δ ϕ = λ 2 π ∣Δ n ∣ d = 589 × 1 0 − 9 2 π ( 0.172 ) ( 2.0 × 1 0 − 6 ) .
Why this step? Same phase formula, now solving forward for Δ ϕ .
Step 2. Numerator inside: 0.172 × 2.0 × 1 0 − 6 = 3.44 × 1 0 − 7 . Divide by 589 × 1 0 − 9 = 5.89 × 1 0 − 7 : ratio = 0.5840 .
Step 3. Δ ϕ = 2 π × 0.5840 = 3.669 rad = 1.168 π .
Verify: 1.168 π is just above π — matches the forecast. It is not a clean half-wave plate (π ) nor quarter-wave (π /2 ); the extra 0.168 π means the output is elliptically polarized. ✅ (See Polarization of light .)
Worked example Example 8 — Cell H: the e-ray
walk-off angle
For calcite at θ = 4 5 ∘ between k ^ and the optic axis, the e-ray's energy travels at an angle α off k ^ given by
tan ( θ + α ) = ( n e n o ) 2 tan θ .
Find α . (This α is literally why the e-ray is "extraordinary".)
Forecast: Since calcite is negative (n o > n e ), ( n o / n e ) 2 > 1 , so the ray direction tilts further than k ^ — expect a small positive walk-off of a few degrees.
Step 1. ( n o / n e ) 2 = ( 1.658/1.486 ) 2 = ( 1.11575 ) 2 = 1.24489 .
Why this step? This ratio is the "anisotropy strength"; > 1 means the e-ray leans away from k ^ .
Step 2. tan 4 5 ∘ = 1 , so tan ( 4 5 ∘ + α ) = 1.24489 .
Step 3. 4 5 ∘ + α = arctan ( 1.24489 ) = 51.22 9 ∘ , hence α = 6.22 9 ∘ .
Why this step? arctan answers "which angle has this tangent?" — it undoes the tan on the left.
Verify: α ≈ 6. 2 ∘ , a small positive tilt — matches the forecast and the famous "double image shift" you see through a calcite crystal. If we had used a positive crystal (n o < n e ) the ratio would be < 1 and α would be negative (tilts the other way). ✅
Worked example Example 9 — Cell I: real-world word problem (which crystal splits more?)
You need to physically separate two polarizations for a Nicol prism over a 1.0 mm path, and you may pick calcite (Δ n = − 0.172 ) or quartz (Δ n = + 0.009 ). Which gives the larger optical-path separation between the rays, and how big is it?
Forecast: Separation grows with ∣Δ n ∣ . Calcite's 0.172 dwarfs quartz's 0.009 , so calcite wins by roughly 0.172/0.009 ≈ 19 × . Guess: calcite gives a path gap of order 0.17 mm.
Step 1. Optical-path gap = ∣Δ n ∣ d .
Why this step? Same optical-path idea as the wave plate, but now we care about the physical separation the two rays accumulate.
Step 2. Calcite: 0.172 × 1.0 × 1 0 − 3 = 1.72 × 1 0 − 4 m = 0.172 mm.
Step 3. Quartz: 0.009 × 1.0 × 1 0 − 3 = 9.0 × 1 0 − 6 m = 0.009 mm.
Verify: Ratio = 0.172/0.009 = 19.1 ✅. Calcite separates ~19× more — exactly why real Nicol prisms are cut from calcite, not quartz. ✅
Worked example Example 10 — Cell J: exam twist (solve
backwards for the angle)
In calcite you measure the e-ray feeling index n e ( θ ) = 1.600 . At what angle θ to the optic axis is it travelling?
Forecast: 1.600 sits between 1.486 and 1.658 , so a valid θ exists. It is closer to n o = 1.658 , and in a negative crystal high index means small θ — expect something under 4 5 ∘ .
Step 1. Rearrange the workhorse. Using cos 2 θ = 1 − sin 2 θ :
n e ( θ ) 2 1 = n o 2 1 + sin 2 θ ( n e 2 1 − n o 2 1 ) .
Why this step? Collecting everything onto sin 2 θ lets us isolate the one unknown.
Step 2. Plug numbers: n e ( θ ) 2 1 = 1/2.56 = 0.390625 ; n o 2 1 = 0.363805 ; n e 2 1 − n o 2 1 = 0.452899 − 0.363805 = 0.089094 .
Step 3. sin 2 θ = 0.089094 0.390625 − 0.363805 = 0.089094 0.026820 = 0.30103 .
Step 4. sin θ = 0.30103 = 0.54866 , so θ = arcsin ( 0.54866 ) = 33.2 7 ∘ .
Why this step? arcsin answers "which angle has this sine?" — the inverse we need after isolating sin θ .
Verify: Re-substitute θ = 33.2 7 ∘ into the forward formula: cos 2 = 0.699 , sin 2 = 0.301 , giving 1/ n e 2 = 0.699/2.749 + 0.301/2.208 = 0.2543 + 0.1363 = 0.3906 , so n e = 1.600 ✅. And 33.2 7 ∘ < 4 5 ∘ , matching the forecast. ✅
Recall Quick self-test on the matrix
At θ = 0 the e-ray index equals what? ::: n o (no splitting along the optic axis)
In a negative crystal, does n e ( θ ) rise or fall as θ goes 0 → 9 0 ∘ ? ::: It falls (from n o down to n e )
If n o = n e , what is n e ( θ ) ? ::: A single constant n for all θ — the crystal is isotropic
What controls how thick a wave plate must be? ::: ∣Δ n ∣ and the target Δ ϕ : d = λ Δ ϕ / ( 2 π ∣Δ n ∣ )
Why does the e-ray "walk off"? ::: Its energy flow tilts by α from k ^ because ( n o / n e ) 2 = 1
Mnemonic Matrix in one breath
"Ends pin, middle slides, sign steers, equal kills."
Ends (0 ∘ , 9 0 ∘ ) pin the index to n o /n e ; the middle slides between them; the sign of Δ n steers which way it slides (and the walk-off); equal indices kill birefringence entirely.