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SCIENCE · INVESTIGATE AND EXPLAIN

Derive local intensity from complex field addition

A complex amplitude records two real pieces of information: magnitude and phase relative to a reference. For equally polarized waves of the same frequency in the same medium, the detector intensity is proportional to the squared magnitude of the summed field. The common proportionality constant is absorbed into the original normalized units here.

Learning outcome: Reconstruct real and imaginary components before intensity. Compare a complete phase scan with a fixed reading, then change the beam ratio and derive visibility from the observed extrema.

Starting recap

Retain complex amplitude before intensity, definite-integral boundaries, normalization, calibration covariance and unused evidence.

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Try

For r=4 and φ=90°, E=1+2i and I=5. The phase scan ranges from 1 to 9, so V=8/10=0.8. The intensity at this one phase happens to equal the incoherent average, but the remaining phase scan distinguishes them.

Open the experiment

Predict

Can the same local intensity arise from a coherent and an incoherent record?

Experiment

Reconstruct real and imaginary components before intensity. Compare a complete phase scan with a fixed reading, then change the beam ratio and derive visibility from the observed extrema.

Sum fields before squaring

Worked teaching model · synthetic values · Original equal-frequency, equally polarized coherent fields E1=1 and E2=sqrt(a) exp(iφ), in one reference impedance. Phase-averaged incoherent intensity is a separate comparison; interference redistributes flux across the complete apparatus.

Reset keeps your prediction, captures and practice history.

The cross term survives only when the phase relation is retained.

Original equal-frequency, equally polarized coherent fields E1=1 and E2=sqrt(a) exp(iφ), in one reference impedance. Phase-averaged incoherent intensity is a separate comparison; interference redistributes flux across the complete apparatus.

036090relative phase (degrees)relative intensity

The vertical axis is rescaled to this case’s actual range; equal display height does not imply equal optical power. The finite curve is illustrative; the ledger preserves the exact case values and stated numerical quadrature.

Original conditional optical ledger
QuantityValueUnit
Real field component1.00000amplitude
Imaginary field component2amplitude
Coherent local intensity5relative intensity
Incoherent phase-averaged comparison5relative intensity
Maximum over phase9relative intensity
Minimum over phase1relative intensity
Fringe visibility0.800000ratio

Virtual original records only. No laser, intense-light source, instrument alignment, physical apparatus operation or completed practical competence is supplied.

The cross term survives only when the phase relation is retained.

Original equal-frequency, equally polarized coherent fields E1=1 and E2=sqrt(a) exp(iφ), in one reference impedance. Phase-averaged incoherent intensity is a separate comparison; interference redistributes flux across the complete apparatus.

Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.

Understand

1. Establish the optical mechanism

A complex amplitude records two real pieces of information: magnitude and phase relative to a reference. For equally polarized waves of the same frequency in the same medium, the detector intensity is proportional to the squared magnitude of the summed field. The common proportionality constant is absorbed into the original normalized units here.

Write E1=1 and E2=sqrt(r) exp(iφ). Multiplying E1+E2 by its complex conjugate gives I=1+r+2sqrt(r)cosφ. The last term is not extra emitted energy: interference redistributes local flux, and a complete energy account must include the other positions or output channels of the optical system.

As phase varies, Imax=(1+sqrt(r))² and Imin=(1−sqrt(r))². Their difference divided by their sum yields visibility V=2sqrt(r)/(1+r). Equal intensity gives complete ideal contrast, whereas unequal amplitudes leave a nonzero minimum even with perfect coherence.

If the relative phase samples a full uniform cycle during observation, the average cosine is zero and the intensity becomes 1+r. This is an incoherent or phase-averaged comparison, not the field at a particular phase. Orthogonal polarizations also require vector treatment; the scalar formula cannot silently be used for arbitrary polarization.

2. Work the original evidence

For r=4 and φ=90°, E=1+2i and I=5. The phase scan ranges from 1 to 9, so V=8/10=0.8. The intensity at this one phase happens to equal the incoherent average, but the remaining phase scan distinguishes them.

3. Predict and investigate

Can the same local intensity arise from a coherent and an incoherent record?

Reconstruct real and imaginary components before intensity. Compare a complete phase scan with a fixed reading, then change the beam ratio and derive visibility from the observed extrema.

Transfer the derivation to a changed case

Change to equal beams r=1. Find intensities at 0° and 180°, visibility and the phase average.

Retain your prediction, intermediate reasoning and assumptions before opening public feedback.

Compare a worked response

The extrema are 4 and 0, visibility 1 and phase average 2. Local cancellation does not eliminate emitted energy from the complete optical field.

Primary mechanism context. Checked 31 October 2026. Original prose, records and diagrams; no copied source exercises or physical light-source operation. Retain first reasoning and public-feedback exposure in the course evidence workspace when registered.

Apply

For coherent intensity ratio 4, what does a nonzero minimum of 1 establish?

Public practice checks a specific claim. It does not establish independent mastery.

Change to equal beams r=1. Find intensities at 0° and 180°, visibility and the phase average.

Continue

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