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How Does Radioactive Decay Work?

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How Does Radioactive Decay Work?

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Generally, there are four main concepts that students struggle with when thinking about radioactive decay: • the spontaneity (or randomness) of radioactive decay, • the reason isotopes are important, • the concept of half-life, and • knowing which system is appropriate

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If an isotope (forms of chemical elements that differ in the number of neutrons in their atomic nuclei) is radioacitve, it will break down naturally into a lighter element called a decay product. This process occurs at a predictable rate and can be used to determine how old an object is. What is a Half-life? A half-life is the time required for half of an element’s atoms in a sample to change to the decay product. In each half-life only half of the remaining radioactive atoms decay, no matter how large the sample is. Look at the diagram below which represents the radioactive decay of uranium-238. The shaded area represents the decay product which is lead-206. The half-life of uranuim-238 is 4.5 billion years, since this object has gone through two half-lives it is 9 billion years old.

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