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Geoffrey Ingram Taylor. Sir Geoffrey Ingram Taylor ( Londres, 7 de março de 1886 — Cambridge, 27 de junho de 1975) era um físico e matemático britânico, e uma figura importante na dinâmica de fluidos e na teoria das ondas.
Sir Geoffrey Ingram Taylor OM FRS FRSE (7 March 1886 – 27 June 1975) was a British physicist and mathematician, who made contributions to fluid dynamics and wave theory. Early life and education. Taylor was born in St. John's Wood, London.
1922. The penetration of a fluid into a porous medium or Hele-Shaw cell containing a more viscous liquid. PG Saffman, GI Taylor. Proceedings of the Royal Society of London. Series A. Mathematical and …. , 1958. 4338. 1958. The instability of liquid surfaces when accelerated in a direction perpendicular to their planes.
Summary. Geoffrey Taylor was a British physicist and mathematician who worked in fluid dynamics and wave theory. View four larger pictures. Biography. Geoffrey Taylor's father was Edward Ingram Taylor (born Paddington, London, 1855) who was an artist who designed and decorated the public rooms in ocean liners.
1 de mai. de 2024 · Sir Geoffrey Ingram Taylor was a British physicist. He taught at Cambridge University from 1911 to 1952. He made important discoveries in fluid mechanics, as well as significant contributions to the theory of the elastostatic stress and displacement fields created by dislocating solids, the quantum.
- The Editors of Encyclopaedia Britannica
1 de jan. de 2020 · A biography of the physicist and mathematician who made significant contributions to fluid dynamics and wave theory. Learn about his life, education, career, achievements, honors, and cross-references in the field of continuum mechanics.
24 de dez. de 2016 · Geoffrey Ingram Taylor is recognized within astronomy for the description of Taylor columns (rotating, rising fluid structures, of which the Great Red Spot on Jupiter may be an example) and for the development of the theory of the Rayleigh-Taylor instability, in which a dense fluid, held up by the pressure of a less dense one underneath, rather ...
