CampusDownWiki
Total citations 10,489한국어KO 2,688EnglishEN 5,585日本語JA 745中文ZH 1,471
CampusDown ↗
English

Half-life

🔬 Natural Sciences By CampusDown Wiki Editorial Team Last updated
A half-life is the time it takes for half of the radioactive nuclei in a sample to decay, leaving half the original amount; each isotope has its own, and it is virtually unaffected by temperature or pressure.
Contents
  1. 1. Discovery and meaning
  2. 2. Half-lives of common isotopes
  3. 3. Dating and drug half-life
  4. 4. FAQ
  5. 5. References

Discovery and meaning

In 1903 Ernest Rutherford and Frederick Soddy at McGill University showed that radioactive elements transform into other elements (decay) and that their activity falls at a fixed rate; by around 1907 Rutherford was calling this period the half-life. No one can predict when a single atom will decay, but across huge numbers of atoms the amount drops by exactly half in each interval. After two half-lives a quarter remains, after three an eighth and after ten about a thousandth. Iodine-131, with an 8-day half-life, falls to one-eighth after 24 days.

Half-lives of common isotopes

Half-lives range from fractions of a second to longer than the age of the universe. Short ones suit medical tests where nothing should linger in the body; long ones serve as clocks for deep time.

IsotopeHalf-lifeMain use
Technetium-99mAbout 6 hoursNuclear medicine imaging
Iodine-131About 8 daysThyroid treatment
Cesium-137About 30 yearsMarker of reactor-accident fallout
Carbon-14About 5,730 yearsRadiocarbon dating
Uranium-238About 4.5 billion yearsDating the age of Earth

Cesium-137 became the key measure of soil and food contamination after the 2011 Fukushima accident. A longer half-life means weaker radiation that lingers; a shorter one means stronger radiation that fades fast.

Dating and drug half-life

In 1949 Willard Libby developed radiocarbon dating, based on carbon-14 that stays constant in living things and decays with a 5,730-year half-life after death, winning the 1960 Nobel Prize in Chemistry. It works for material up to about 50,000 years old; older rocks are dated with long-lived isotopes such as uranium and potassium. In 1956 Clair Patterson used lead isotopes in meteorites to put Earth's age at about 4.55 billion years. In medicine, a drug's half-life is the time for its blood level to halve; it guides dosing intervals, and a drug is usually considered cleared after four to five half-lives.

FAQ

Is a radioactive substance gone after two half-lives?
No. It halves each time, so a quarter remains after two. In theory it never reaches zero; after ten half-lives (about 1/1000) it is usually considered greatly reduced.
Does heating a substance shorten its half-life?
Radioactive decay happens inside the nucleus, so temperature, pressure and chemistry have essentially no effect. That stability is what makes it a reliable dating clock.

Sources reviewed: 2026-10-26

References

  1. Rutherford, E., & Soddy, F. (1903). Radioactive change. Philosophical Magazine, 5(29), 576–591.
  2. Libby, W. F. (1955). Radiocarbon Dating (2nd ed.). University of Chicago Press.
  3. Patterson, C. (1956). Age of meteorites and the earth. Geochimica et Cosmochimica Acta, 10(4), 230–237.

Reports and materials that use this theory (Korean)

There are no materials dedicated to this theory yet, but you can search related reports in the CampusDown library (Korean).

Find more reports · Search '반감기' on CampusDown →

You may also like

Latest ArticlesView all ›

New guides for college study and assignments (Korean)

This article was last updated on October 26, 2026. It is based on widely recognized original works and textbooks; when citing it in a paper, please check the original sources listed in the references.