Radioactive isotope diffusion refers to the process by which radioactive isotopes move through a medium, such as rock or sediment, driven by concentration gradients and thermal energy. This movement can significantly impact the distribution and concentration of isotopes in geological materials, influencing age dating and geochemical processes. Understanding this diffusion is crucial in fields like geochronology and environmental studies, as it helps unravel the history of geological formations and the behavior of contaminants in the environment.
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