Джордж Ветерилл: Американ физигі және планетолог

American physicist (1925–2006)

George Wetherill (August 12, 1925 Philadelphia, Pennsylvania – July 19, 2006 Washington, D. C.) was a physicist and geologist and the director emeritus of the department of terrestrial magnetism at the Carnegie Institution of Washington, DC, US. In 2000, Wetherill received the J. Lawrence Smith Medal from the National Academy of Sciences "For his unique contributions to the cosmochronology of the planets and meteorites and to the orbital dynamics and formation of solar system bodies."

After receiving his Ph. D., Wetherill became a staff member at Carnegie's Department of Terrestrial Magnetism (DTM) in Washington, D. C. There, he joined an interdepartmental group who were working to date rocks using geochemical methods that measured natural radioactive decay. This involved determining the concentration and isotopic composition of inert gases such as argon, as well as the isotopes of strontium and lead.

Wetherill left DTM in 1960 to become a professor of geophysics and geology at the University of California, Los Angeles. There, he served as chairman of the interdepartmental curriculum in geochemistry (1964 1968), and as chairman of the Department of Planetary and Space Sciences (1968 1972).

In 1975, Wetherill returned to Carnegie's Department of Terrestrial Magnetism as director. He remained director until 1991, when he became a staff member. At DTM, he began extending his research efforts into questions concerning the origin of the terrestrial planets Mercury, Venus, Earth, and Mars. He was stimulated by earlier studies by Victor Safronov (O. Yu. Schmidt Institute, Moscow), who showed that as a swarm of planetesimals coagulated into large bodies the swarm could evolve to produce a few terrestrial planets. Wetherill developed a technique to calculate numerically the orbital evolution and accumulation of planetesimal swarms, and he used the technique to reach specific predictions of the physical and orbital properties of terrestrial planets. His results agreed well with present observations. In addition to showing how the inner solar system formed, Wetherill's work provided the basis for a model of a giant impact origin for the Moon and the core of Mercury. It also led to explanations for the isotopic abundances of present day planetary atmospheres. Wetherill has shown that Jupiter plays an important role in the evolution of the Solar System; by ejecting comets from the solar system, it offers a protective presence to the inner planets.

Wetherill provided leadership in the scientific community by serving on advisory committees for NASA, the National Academy of Sciences, and the National Science Foundation. For 15 years, he was editor of the Annual Review of Earth and Planetary Sciences. He served as president of the Meteoritical Society, the Geochemical Society, the Planetology Section of the American Geophysical Union, the International Association of Geochemistry and Cosmochemistry, and was a member of the American Philosophical Society. Wetherill died at his home in Washington, D. C Wednesday, July 19, 2006, after a long illness.