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Max Planck introduced the Planck constant h in 1900 to solve the black-body radiation problem: the observed spectral distribution of electromagnetic radiation emitted by a body did not match existing theories across all wavelengths. Classical ideas and later approximations worked only in limited regimes—Wien’s law for short wavelengths/high temperatures and the Rayleigh–Jeans law for long wavelengths—leaving a major discrepancy (especially at short wavelengths). Planck modeled radiation as arising from many harmonic oscillators (one per frequency) and sought a formula that matched both the short- and long-wavelength behavior. Planck’s key step was to modify the assumptions about how oscillator energy is exchanged. He found that reproducing the full spectrum required treating the energy of oscillators as discrete rather than continuously divisible, with energy elements proportional to frequency. This led to the Planck radiation law and the energy–frequency relation E = h f (first version of the Planck–Einstein relation). Using experimental black-body data, Planck could estimate h (close to the modern value), showing that the constant was not merely a fitting parameter but encoded the quantization needed to explain black-body spectra.
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