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In physics, radiation is the emission or transmission of energy through space or a material medium in the form of waves or particles. It includes electromagnetic radiation (photons such as radio waves, microwaves, infrared, visible light, ultraviolet, X-rays, and gamma rays), particle radiation (subatomic particles with non-zero rest energy such as alpha, beta, proton, and neutron radiation), and other wave phenomena like acoustic and gravitational radiation. A key way radiation is classified is by whether it is ionizing or non-ionizing, which depends largely on the energy of the radiation. Ionizing radiation has enough energy to ionize atoms and molecules—typically more than about 10 eV—breaking chemical bonds and potentially damaging biological tissue (especially DNA). Common ionizing forms include gamma rays and X-rays (higher-energy parts of the electromagnetic spectrum), ultraviolet radiation at sufficiently energetic wavelengths, and particle types such as alpha particles, beta particles, and neutrons. Non-ionizing radiation has lower energies that generally cannot ionize atoms; instead, it may cause molecular excitation or vibrations that are experienced as heat (e.g., infrared, microwaves, radio waves). The boundary between ionizing and non-ionizing effects is not perfectly sharp, and some overlap in biological effects can occur. Ionizing radiation is further described by its mechanisms and penetration: alpha particles are strongly ionizing but weakly penetrating (stopped by thin materials), beta particles penetrate more than alpha but less than gamma, and gamma rays penetrate deeply because they are uncharged photons. Neutrons are “indirectly ionizing” because they ionize mainly through nuclear interactions such as absorption that make nuclei unstable. Radiation also occurs naturally (e.g., from radioactive materials in rocks and cosmic rays) and can be detected with specialized instruments like Geiger counters.
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