advanced28 min studyLesson 226 in Physics

A reference beam makes phase observable

Recover a complex field from calibrated reference interference and distinguish recording from reconstruction.

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What you’ll understand

  • Identify the object–reference cross terms in an intensity record.
  • Explain off-axis separation and reconstruction orders.
  • Recover a complex field with four reference-phase exposures.

An ordinary camera cannot directly follow an optical field oscillating hundreds of trillions of times per second. It records an averaged intensity and discards the local absolute phase. Holography introduces a known reference field so that relative object phase appears in measurable interference. The record remains an intensity image; its additional information comes from a controlled comparison. Reconstruction then extracts a complex field relative to that reference, subject to sampling and calibration.

The reference creates information-bearing cross terms

Write the object and reference complex amplitudes at the recording plane as O and R. Their intensity contains the object intensity, the reference intensity, and two conjugate cross terms. These last terms encode the phase difference. Mutual coherence, compatible polarizations, and mechanical stability are necessary during the exposure. A bright reference by itself does not recover phase if the relative phase wanders through many cycles before the detector finishes averaging.

In off-axis holography, tilt a plane-wave reference slightly relative to the object beam. Its known transverse phase ramp shifts the two cross-term spectra to opposite carrier frequencies. A Fourier-domain window can isolate one cross term if the carrier, object bandwidth, and sampling rate leave them separated from each other and the central intensity terms. Too little tilt causes overlap; too much tilt produces fringes finer than the pixels can sample. Neither problem is solved just by increasing reference power.

I=∣O+R∣2=∣O∣2+∣R∣2+OR∗+O∗R,R(x)=rei2πfrxI=|O+R|^2=|O|^2+|R|^2+OR^*+O^*R,\qquad R(x)=r e^{i2\pi f_r x}
O and R are calibrated scalar amplitudes with intensity |O|² and |R|². r is a real reference amplitude, x is in metres, and off-axis carrier f_r is in cycles per metre.↔ Scroll wide equations horizontally.

Reconstruction is a separate optical operation

For a simple thin amplitude hologram, suppose developed transmittance varies linearly with recorded intensity over a limited exposure range. Illuminating that pattern with the original reference gives several field terms. One is proportional to the object field multiplied by reference intensity; another involves the conjugate object and produces a twin image. Other terms form an undiffracted background. Off-axis geometry separates these orders in angle. Real recording materials can be nonlinear, so this elementary transmittance law is a deliberate model.

A digital hologram instead stores camera samples and extracts the complex cross term numerically, then propagates it with a calibrated diffraction model. The recovered field is defined relative to the reference, not an independently measurable absolute phase of the universe. Refocusing can move a reconstruction plane within the information supported by the measurement. It does not restore unrecorded spatial frequencies, remove speckle automatically, or supply complete three-dimensional material properties from one arbitrary scattering scene.

Phase stepping offers another controlled comparison

Rather than separate orders spatially, record several exposures while stepping a uniform reference phase. For a stable object and known real reference amplitude r, phases zero, π/2, π, and 3π/2 separately probe the real and imaginary parts of the object field. Subtracting opposite exposures removes both separate intensities. The four measurements therefore yield two quadratures without needing an off-axis carrier, although motion between frames or phase-step calibration errors can corrupt the result.

Use the waves lab as a fully coherent object–reference pair. Reset and set both controls to phase zero degrees and amplitude ratio 0.5; predict amplitude 1.5. Reset again and set phase 180 degrees and ratio 0.5; predict amplitude 0.5. The squared amplitudes differ by two in its arbitrary intensity units. The lab shows signed waveforms rather than camera exposure values and has no hologram, Fourier filtering, or diffraction reconstruction. Its purpose is to test the interference algebra before interpreting a recorded pattern.

Re⁡O=I0−Iπ4r,Im⁡O=Iπ/2−I3π/24r,Iϕ=∣O+reiϕ∣2\operatorname{Re}O=\frac{I_0-I_\pi}{4r},\qquad \operatorname{Im}O=\frac{I_{\pi/2}-I_{3\pi/2}}{4r},\qquad I_\phi=|O+r e^{i\phi}|^2
All four intensities use one linear detector calibration and the same stable O and r>0. The phase convention places the controlled phase on the added reference field.↔ Scroll wide equations horizontally.

Recover two field quadratures

A unit-amplitude reference is stepped through phases 0,π/2,π,3π/2. The calibrated intensities at one pixel are 8,10,4,2 in that order. Recover the object amplitude and its intensity, and check consistency of the separate-intensity background.

  1. Subtract the opposite real-quadrature frames: 8−4=4. Divide by four times the reference amplitude, giving real object amplitude one.

  2. Subtract the other opposite frames: 10−2=8. Dividing by four gives imaginary object amplitude two, so the recovered complex field is 1+2i.

  3. Its intensity is 1²+2²=5. Adding reference intensity one gives background six; both opposite-frame averages, (8+4)/2 and (10+2)/2, equal six, as required.

The result

The field relative to the reference is 1+2i, with object intensity 5 and separate-intensity background 6.

Explore the model

Interactive lab

Interactive lab · waves

Reference phase changes the record

Reset and set BOTH controls to phase 0° and ratio 0.5, predicting amplitude 1.5. Reset and set phase 180° and ratio 0.5 for a separate run, predicting amplitude 0.5. Compare their squared amplitudes.

Reference phase changes the recordTwo waves share the same frequency and wave number. Playback advances t in sin(2x − t) + a sin(2x − t + phase). Current readings: Sum at x = 0: 0.866; Resultant amplitude: 1.732; Phase difference: 60°. All parameters are adjustable with the labeled controls below.−3.14−1.5701.573.14−3.4−1.701.73.4x · radiansAmplitude
SumFirst componentSecond component
Sum at x = 0
0.866
Resultant amplitude
1.732
Phase difference
60°
t = 0 s

Two waves share the same frequency and wave number. Playback advances t in sin(2x − t) + a sin(2x − t + phase). Parameter changes pause playback and recompute the model at the current elapsed time. Reset restores both parameters and returns time to zero. Playback starts paused. Adjust either parameter, then choose Play or Step.

Look forA known reference converts relative phase into intensity changes; this lab does not record or reconstruct a hologram.

Check your understanding

What allows an off-axis hologram to encode and then separate object phase information?

Try it yourself

At one stable pixel O=1+i and the reference amplitude is two. Predict the four intensities for reference phases 0,π/2,π,3π/2, then verify the recovered quadratures.

Take a moment to make a prediction or work it out on paper. Open a hint when you need one.

Give me a hint

The separate-intensity background is |O|²+4. The cross terms are four times the real or imaginary quadrature with the appropriate sign.

Compare with the solution

The background is 2+4=6. The four intensities are 6+4=10, 6+4=10, 6−4=2, and 6−4=2. Their opposite differences divided by 4r=8 both equal one. The recovered field is 1+i as required; the equal real and imaginary parts happen to make pairs of exposures equal.

Take it with you

  • A hologram records object–reference interference intensity.
  • Off-axis carriers and phase stepping are different ways to extract cross terms.
  • Reconstruction recovers a reference-relative field within recorded bandwidth.

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