| John Hamilton Reynolds | |
| Birth Date: | 3 April 1923 |
| Birth Place: | Cambridge, Massachusetts, United States |
| Death Place: | Berkeley, California, United States |
| Field: | Geophysics |
| Work Institution: | University of Chicago, University of California, Berkeley |
| Alma Mater: | Harvard University, University of Chicago |
| Doctoral Advisor: | Mark Inghram |
| Known For: | Discovery of excess meteoritic 129Xe |
| Prizes: | John Price Wetherill Medal (1965) J. Lawrence Smith Medal (1967) Leonard Medal (1973)[1] |
John Hamilton Reynolds[2] (April 3, 1923 – November 4, 2000) was an American physicist and a specialist in mass spectrometry.
John H. Reynolds was born 3 April 1923 in Cambridge, Massachusetts, United States. He studied first at Harvard University and, after serving in the Navy during World War II, at the University of Chicago. There, he was influenced by his Ph.D. thesis advisor Mark Inghram and by two other famous physicists, Harold Urey and Enrico Fermi. He specialized in mass spectrometry and utilized this method to determine isotope ratios needed for the radiometric dating of geologically and cosmologically relevant samples. In 1950 he was appointed as professor to the University of California, Berkeley where he continued his research on isotope ratios in meteorites, leading to the discovery in 1960 that the Richardton meteorite and other meteorites had an excess of xenon-129,[3] [4] [5] thought to be a result of the beta decay of iodine-129 in the early Solar System.[6] His improvement of potassium-argon dating was adopted by several institutions.[7] [8]
Reynolds was a Guggenheim Fellow for the academic years 1956–1957 and 1986–1987.[9] He was elected to the National Academy of Sciences in 1968.[1] He died of pneumonia on November 4, 2000, in Berkeley, California, United States.