Frequency sum and wave-vector mismatch
In second-harmonic generation, the two lower-frequency photons are identical fundamental photons. Difference-frequency generation starts from wave three plus a coherent lower-frequency seed.
L26 · Phase matching and energy exchange
Does a longer crystal always make more new light? No. Phase mismatch can make light generated at different depths cancel. Even at matched angles, sum-frequency mixing can send energy back into the input waves. In matched second-harmonic generation from a single input, conversion approaches a limit; finite-beam walk-off can stop extra length from helping.
Watch input light fade as a new frequency grows inside the crystal. Compare the automatically acquired depth trace and angle scan, then try sum-frequency back-conversion or seeded difference mixing.
Physics tutorial
BackgroundIn a nonlinear crystal, light waves of different frequencies exchange energy. The crystal couples the fields; it does not add an independent source of optical energy.
Why it mattersLight made deeper in the crystal can reinforce what came before or cancel part of it. In sum-frequency mixing, the same coupling can also return energy to the inputs.
Start with the essentials
In second-harmonic generation, the two lower-frequency photons are identical fundamental photons. Difference-frequency generation starts from wave three plus a coherent lower-frequency seed.
The high-frequency wave travels as an extraordinary wave and the two lower-frequency waves as ordinary waves. The reference angle comes from the Sellmeier fit for BBO.
Every wave can be depleted. For second harmonic, the two low-frequency waves become a single wave, and the equation for the high-frequency wave takes half the coupling coefficient.
The two Manley–Rowe invariants hold when the waves are distinct. For second harmonic, the conserved quantity is the fundamental photon flow plus twice the harmonic photon flow.
As the extraordinary beam walks off sideways, a prescribed Gaussian overlap factor reduces the coupling. This is a scalar approximation for finite beams; it does not solve for diffracting or distorted transverse fields.
For lossless, phase-matched plane waves, this closed form gives an independent check on the numerical propagation. With weak conversion and nonzero mismatch, the familiar sinc-squared curve appears.
Typical misconceptionEach beam really has the color shown on screen.
Better mental modelThe colors only label the model's channels, and some of those channels are infrared. The wavelength readouts tell you what each beam physically is.
Typical misconceptionAn ideal phase-matching curve is as good as detector data.
Better mental modelEach recorded point reruns the model with depleting fields. The values are simulated powers, not measurements from real hardware.
Choose Matched second harmonic. A depth trace and angle scan are acquired automatically; open Advanced controls to move the depth diagnostic.
What to observe: The diagnostic reads a different point on the same propagated solution. The stored trace and scan retain their original values.Drag the internal-axis dial or choose Angle mismatch. Temperature mismatch is in Advanced controls and additional demonstrations.
What to observe: The generated output falls and the depth trace can oscillate. The optical frequencies still conserve energy; the fields no longer add in step along the crystal.Choose Sum frequency and increase Crystal length from two to four millimetres. Then try Seeded difference frequency.
What to observe: Sum-frequency output can fall as energy returns to the lower-frequency waves. Seeded difference mixing instead drains the higher-frequency pump and amplifies the seed as it generates its partner.Probes and measurement · Reading path
Articles on this path that use this experiment, followed by the other experiments they suggest.