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Willard Libby

Chemistry

Willard Frank Libby was an American physical chemist who lived from 1908 to 1980. He is noted for his role in developing radiocarbon dating in 1949, a process that revolutionized archaeology and paleontology, for which he was awarded the Nobel Prize in Chemistry in 1960. A 1931 chemistry graduate of the University of California, Berkeley, where he also earned his doctorate in 1933, he studied radioactive elements and developed sensitive Geiger counters to measure weak radioactivity. During World War II he worked on the Manhattan Project's gaseous diffusion process for uranium enrichment at Columbia University. After the war he joined the University of Chicago's Institute for Nuclear Studies, where he developed the technique for dating organic compounds using carbon-14, and later served on the Atomic Energy Commission before becoming a professor of chemistry at UCLA.

Facts
Birth Year
1908 1
Death Date
1980-09-08 1
Death Year
1980 1
Death Place
Los Angeles, United States 1
Nationality
United States 1
Birthplace
Grand Valley, United States 1
Field
Field (category)
Physics 1
Field (category)
Chemistry 1
Connections

Member Of

Source Willard Libby (Wikipedia)

Works In

Chemistry, Disciplines
Source Willard Libby (Wikipedia)
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Sources
1. Willard Libby (Wikidata)
  • P570 (date of death): year
    +1980-09-08T00:00:00Z
  • P570 (date of death): full date
    +1980-09-08T00:00:00Z
  • P27 (country of citizenship): United States
    Q30
  • P20 (place of death): Los Angeles, United States
    Q65
  • P19 (place of birth): Grand Valley, United States
    Q5595214
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Willard Libby (Wikipedia)
  • Member Of: Columbia University, Infobox, workplaces
    Infobox workplaces: University of California, Berkeley SAM Laboratories Columbia University University of Chicago University of California, Los Angeles
  • Works In: Chemistry, Lead sentence
    Willard Frank Libby (December 17, 1908, September 8, 1980) was an American physical chemist noted for his role in the 1949 development of radiocarbon dating, a process which revolutionized archaeology and palaeontology.
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