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Alexis Claude Clairaut (French pronunciation: [alɛksi klod klɛʁo]; 13 May 1713 – 17 May 1765) was a French mathematician, astronomer, and geophysicist. He was a prominent Newtonian whose work helped to establish the validity of the principles and results that Sir Isaac Newton had outlined in the Principia of 1687.
May 7, 2012 · 17 May 1765. Paris, France. Summary. Alexis Clairaut was a French mathematician who worked to confirm the Newton-Huygens belief that the Earth was flattened at the poles. View two larger pictures. Biography. Alexis Clairaut's father, Jean-Baptiste Clairaut, taught mathematics in Paris and showed his quality by being elected to the Berlin Academy.
Learn about the life and work of Alexis Clairaut, a child prodigy who presented his research on four families of algebraic curves to the Royal Academy of Sciences at age 13. Explore the history and geometry of these curves, which are related to mean proportionals and Descartes' geometrie.
…1747 French mathematician and physicist Alexis-Claude Clairaut proposed a modification of Newton’s law of gravity. Instead of a pure inverse-square law, Clairaut proposed adding a small term, proportional to the inverse fourth power of the distance, in order to get the motion of the Moon’s perigee to come out correctly.…
May 13, 2017 · On May 13, 1713, French mathematician, astronomer, and geophysicist Alexis Claude Clairaut was born. Clairaut was one of the key figures in the expedition to Lapland that helped to confirm Newton’s theory for the figure of the Earth. In that context, Clairaut worked out a mathematical result now known as “Clairaut’s theorem“.
A dual language edition of Clairaut's 1734 paper on four new families of curves and their properties. Learn about the historical and mathematical contexts of Clairaut's work and his use of the term genre.
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Overview. Alexis Claude Clairaut. (1713—1765) Quick Reference. (1713–65) Frenchmathematician and physicist. In 1736 he took part in an expedition to Lapland to measure the length of a degree of latitude; the result proved that the Earth is an oblate spheroid.
