argon-40
Quick Summary
Argon-40 (⁴⁰Ar) is a stable isotope of the noble gas argon. While argon-36 and argon-38 are more common in the universe, argon-40 constitutes 99.60% of argon found on Earth. This abundance is primarily due to the radioactive decay of potassium-40 (⁴⁰K) into argon-40. This process, which has been occurring since Earth's formation, allows argon-40 to slowly escape from rocks into the atmosphere. The decay of potassium-40 to argon-40 is a key principle used in potassium-argon dating to determine the age of rocks and minerals.123
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argonThe production of argon-40 from potassium-40 decay is utilized as a means of determining Earth’s age (potassium-argon dating).
Read MoreThe production of argon-40 from potassium-40 decay is utilized as a means of determining Earth’s age (potassium-argon dating).
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datingPotassium–argon methods…of mass 40 (40K) to argon gas of mass 40 (40Ar) formed the basis of the first widely used isotopic dating method. Since radiogenic argon-40 was first detected in 1938 by the American geophysicist Lyman T. Aldrich and A.O. Nier, the method has evolved into one of the most versatile…
Read More…of mass 40 (40K) to argon gas of mass 40 (40Ar) formed the basis of the first widely used isotopic dating method. Since radiogenic argon-40 was first detected in 1938 by the American geophysicist Lyman T. Aldrich and A.O. Nier, the method has evolved into one of the most versatile…
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