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Potassium-40 (40K) is a radioactive isotope of potassium, a chemical element essential for plant and animal life. While natural potassium consists mainly of stable isotopes potassium-39 and potassium-41, about 0.01 percent is potassium-40.1

Potassium-40 has a long half-life of approximately 1.25 billion years. It decays into two daughter products: argon-40 and calcium-40. This decay process is the basis for potassium-argon dating, a method used to determine the age of rocks and minerals. The ratio of argon-40 to potassium-40 in a sample can indicate how long ago the rock or mineral formed. This dating technique is valuable for understanding Earth's history, with applications ranging from dating meteorites to recent volcanic rocks.123

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