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John Perry (engineer)

John Perry
Born (1850-02-14)14 February 1850
Garvagh, County Londonderry, Ireland
Died 4 August 1920(1920-08-04) (aged 70)
Nationality British
Parent(s) Samuel Perry
Engineering career
Discipline Mechanical

John Perry (14 February 1850 – 4 August 1920) was a pioneering engineer and mathematician from Ireland.

He was born on 14 February 1850 at Garvagh, County Londonderry, the second son of Samuel Perry and a Scottish-born wife.

Perry worked as Lord Kelvin's assistant at the University of Glasgow, and later became professor of mechanical engineering at Finsbury Technical College. He was a colleague of William Edward Ayrton and John Milne at the Imperial College of Engineering in Tokyo, 1875–79, and was also a Fellow of the Royal Society. In 1900 he was elected president of the Institution of Electrical Engineers, and from 1906–08 served as president of the Physical Society of London.

Perry was a great admirer of his employer, Lord Kelvin. In the printing of his 1890 lecture on spinning tops, Perry inscribed the following acknowledgement: "This report of an experimental lecture is inscribed to Sir William Thomson, by his affectionate pupil, the lecturer, who hereby takes a convenient method of acknowledging the real author of whatever is worth publication in the following pages." The book was later reprinted by Dover Publications in 1957 as Spinning Tops and Gyroscopic Motions.

Perry received an honorary doctorate (LL.D) from the University of Glasgow in June 1901.

In 1895, Perry published a paper challenging Kelvin's assumption of low thermal conductivity inside the Earth, and thus disputing Kelvin's estimate that the Earth was only 20–400 million years old, but this had little impact. It was not until the discovery in 1903 that radioactive decay releases heat and the development a few years later of radiometric dating of rocks that it was accepted that the age of the earth was many times older, as Perry had argued. Perry's reasoning held that if the interior of the Earth was fluid, or partly fluid, it would transfer heat much more effectively than the conductivity which Kelvin assumed, and he stated that "much internal fluidity would practically mean infinite conductivity for our purpose."


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