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Portions of this entry contributed by Michel Barran
American physical chemist, geophysicist and cosmochemist who was a student at the University of Montana (1914-1917),
then at University of California at Berkeley (where he received his Ph.D. in physical chemistry 1923) and Copenhagen
from 1923-1924, where he studied atomic physics with Niels Bohr. He begin his teaching career
at Johns Hopkins University as an instructor in the chemistry department (1924-1929), and became a pioneer in the
application of quantum mechanics to chemistry. In 1929, he moved to Colombia University and was appointed associate
professor (1929-1934), then full professor (1934-1945). From 1933 to 1940, he was editor of the Journal of
Chemical Physics. In 1931, with F. Brickwedde and G. Murphy, Urey evaporated four liters of hydrogen down to one
millimeter and then measured the spectrum of the remainder. The result was a set of lines displaced slightly from the
hydrogen lines, amounting to the discovery of deuterium, or heavy hydrogen, for which Urey was awarded
in 1934 Nobel Prize in chemistry and had a significant influence on chemistry, physics and medicine. During the 1930s,
Urey's group separated isotopes of oxygen, carbon, nitrogen and sulphur, and worked on medical and biological
applications of isotopes.
During World War II, in spite of his profound pacifism, he directed isotope separation studies of the Manhattan
Project. After the war, he became a professor at the Institute for Nuclear Studies, University of Chicago (1945-1958)
at the same time as Fermi. He was subsequently a professor-at-large at the University of California, San Diego
(1958-1972). Urey was also an advocate of nuclear arms control, working actively with other scientists to promote
global cooperation and to prevent nuclear proliferation and conflict.
In his postwar career, Urey turned almost fully to geochemistry and cosmochemistry. His work with the heavy isotope
oxygen-18 led him to devise methods for estimating the temperature of the ocean during times as far back as 180 million
years ago. This led him into the study of the relative abundance of the elements on Earth and the development of a
theory of the origin of the elements and of their abundances in the Sun and other stars. He also investigated properties
of the Earth's early atmosphere. In this context, he studied the composition of
meteorites. His interests in biology, elemental abundances, and the origin of the solar
system led him to propose his student Stanley Miller to perform the so-called "Miller-Urey's Electric
Discharge Experiment" and to take seriously the experimental results (1953).
After 1958, Urey became a scientific counselor and adviser to the space program, campaigning and arguing for the most
economical and scientifically sound method of conducting space research. Several hundred papers by Urey are listed in
Poggendorff volumes VI and VIIb.
Miller

Urey, H. Papers. http://orpheus.ucsd.edu/speccoll/testing/html/mss0044e.html.
Urey, H. "The Distribution of Electrons in the Various Orbits of the Hydrogen Atom." Astrophys. J. 59, 1924.
Urey, H. "A Hydrogen Isotope of Mass 2 and its Concentration." Phys. Rev. 40, 1932.
Urey, H. "Some Thermodynamic Properties of Hydrogen and Deuterium." Nobel Prize lecture. Stockholm, 1935.
Urey, H. "The Origin and Development of the Earth and Other Terrestrial Planets." Geochim. Cosmochim. Acta 1, 1951.
Urey, H. and Moller, S. L. "Organic Compound Synthesis on the Primitive Earth." Science 130, 245-251, 1959.
Urey, H. The Planets, their Origin and Development. New Haven, CT: Yale University Press, 1952.
Urey, H.; Craig, H.; Miller, G. L.; and Wasserburg, G. J. Isotopic and Cosmic Chemistry. Amsterdam, Netherlands, 1964.
Urey, H. and Ruark, A. Atoms, Molecules, and Quanta, 2 vols., 2nd ed. New York: McGraw-Hill, 1964.
© 1996-2007 Eric W. Weisstein
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