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1: Blackbody Radiation
Definition and Key Problem
Blackbody radiation refers to the electromagnetic radiation emitted by an idealized object (a "blackbody") that absorbs all incident radiation and re-emits energy solely based on its temperature. Real-world approximations include heated metals or stars. By the late 19th century, experiments revealed a universal emission spectrum: intensity versus wavelength curves depended only on temperature, peaking at specific wavelengths (e.g., red glow at 500°C vs. blue-white at 6000°C).
Classical physics, combining thermodynamics and electromagnetism, failed to explain this spectrum. The Rayleigh-Jeans law, derived from classical wave theory, predicted that radiation intensity should increase indefinitely as wavelength decreased (proportional to ). This implied infinite energy at ultraviolet wavelengths—a nonsensical result termed the ultraviolet catastrophe.
Planck’s Quantum Hypothesis
In 1900, Max Planck resolved the catastrophe by introducing a radical assumption: the oscillating charges in the blackbody’s walls emit or absorb energy in discrete packets called quanta, not continuously. He proposed that energy for a frequency is:
where is Planck’s constant () and is an integer. This quantization meant energy exchange could only occur in multiples of .
Planck’s Radiation Law
Using this hypothesis, Planck derived the blackbody spectrum formula:
where:
Key Implications
Significance
Planck’s work marked the birth of quantum theory by demonstrating that energy quantization was necessary to describe nature. Though initially a mathematical trick, it laid the foundation for quantum mechanics, directly influencing Einstein’s explanation of the photoelectric effect (1905).