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The Planck constant h originated from Max Planck’s attempt to solve the black-body radiation problem at the turn of the 20th century. Classical physics could not reproduce the observed spectral distribution: Wien’s law worked for short wavelengths/high temperatures, while the Rayleigh–Jeans law matched long wavelengths but failed badly at short wavelengths (leading to the “ultraviolet catastrophe”). Planck modeled electromagnetic radiation as many harmonic oscillators (one for each frequency) and sought a formula that matched the spectrum across all wavelengths. Planck introduced a crucial modification: he assumed the oscillators’ energy could be exchanged only in discrete amounts rather than continuously. By treating the energy of N oscillators as consisting of integral multiples of finite equal “energy elements,” he derived Planck’s law for spectral radiance, which contains h in the exponential term. This quantization led to the relation that the energy element must be proportional to frequency, yielding the first form of the Planck–Einstein relation E = h f. Using experimental black-body data, Planck estimated h (close to the modern value), establishing h as the proportionality constant governing energy quantization in radiation.
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