List of elements by half-life

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List of Elements by Half-Life

The half-life of a radioactive element is the time required for half of the quantity of the element to undergo radioactive decay. Understanding the half-life of elements is crucial in various fields, including nuclear physics, environmental science, radiometric dating, and medicine. This article provides a comprehensive list of elements categorized by their half-lives, from the shortest to the longest.

Short Half-Life Elements[edit | edit source]

Elements with short half-lives decay rapidly. They are often used in medical imaging and treatments, as well as in scientific experiments that require quick decay rates.

  • Polonium (Po-214): With a half-life of 164 microseconds, Polonium-214 is one of the shortest-lived isotopes used in scientific research.
  • Radon (Rn-222): Radon-222 has a half-life of 3.8 days, making it significant in studies related to atmospheric and environmental sciences.
  • Technetium (Tc-99m): Technetium-99m, with a half-life of 6 hours, is widely used in medical diagnostic procedures, especially in nuclear medicine for imaging.

Intermediate Half-Life Elements[edit | edit source]

These elements have half-lives that range from several days to thousands of years. They are important in industrial applications, geological dating, and long-term medical therapies.

  • Iodine (I-131): Iodine-131 has a half-life of 8 days and is used in the treatment of thyroid cancer and in nuclear medicine imaging.
  • Cesium (Cs-137): With a half-life of about 30 years, Cesium-137 is a byproduct of nuclear fission and is used in medical radiation therapy and industrial gauges.
  • Carbon (C-14): Carbon-14, with a half-life of 5,730 years, is essential in radiocarbon dating for determining the age of archaeological and geological samples.

Long Half-Life Elements[edit | edit source]

Elements in this category have half-lives ranging from millions to billions of years. They are significant in understanding the age of the Earth and the universe, as well as in studying long-term nuclear waste management.

  • Uranium (U-238): Uranium-238 has a half-life of 4.468 billion years and is used in dating the age of the Earth, as well as in nuclear reactors and weapons.
  • Thorium (Th-232): With a half-life of 14.05 billion years, Thorium-232 is used in thorium-based nuclear power generation.
  • Potassium (K-40): Potassium-40 has a half-life of 1.248 billion years and is important in geological dating and studies of the Earth's crust.

See Also[edit | edit source]

References[edit | edit source]



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Contributors: Prab R. Tumpati, MD