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Encyclopedia > Edward V. Appleton

Sir Edward Victor Appleton (September 6, 1892April 21, 1965) was an English physicist. After returning from active service in World War I, he became assistant demonstrator in experimental physics at the Cavendish Laboratory in 1920. He was professor of physics at the Univ. of London (1924–36) and professor of natural philosophy at Cambridge Univ. (1936–39). From 1939 to 1949 he was secretary of the Dept. of Scientific and Industrial Research. Knighted in 1941, he received the 1947 Nobel Prize in Physics for his contributions to the knowledge of the ionosphere, which led to the development of radar.


For many years it had been postulated that there was a conducting layer in the upper reaches of the atmosphere. Marconi had been able to make his historic tranatlantic transmissions and to achieve this the signals had to be "bent if they were to reach their destination. In 1902 Oliver Heaviside and A E Kennelly independently proposed the idea of their being a conducting layer that reflected radio signals.


In his work, Appleton had observed that the strength of the radio signal from a transmitter a on a frequency such as the medium wave band and over a path of a hundred miles or so was constant during the day but that it varied during the night. This lead to him to believe that it was possible that two radio signals were being received. One was traveling along the ground, and another was reflected by a layer in the upper atmosphere. The fading or variation in strength of the overall radio signal received resulted from the interference pattern of the two signals.


To prove his theory, Appleton used the British Broadcasting Corporation (BBC) radio broadcast transmitter at Bournemouth England. This transmitted a signal towards the upper reaches of the atmosphere. He received the radio signals near Cambridge, proving they were being reflected. By making a periodic change to the frequency of the broadcast radio signal he was able to measure the time taken for the signals to travel to the layers in the upper atmosphere and back. In this way he was able to calculate that the height of the reflecting layer was 60 miles above the ground.


External links

  • Sir Edward Victor Appleton (http://www.nobel-winners.com/Physics/edward_appleton.html)
  • Sir Edward Appleton (http://www.radio-electronics.com/info/radio_history/gtnames/appleton.php) A summary of the life and work of Sir Edward Appleton and his contribution to radio science.

  Results from FactBites:
 
Stritmatter Appleton Review (2282 words)
Appleton identifies as the 17th Earl of Oxford -- who seized the gauntlet thrown down by the elusive Puritan satirist, "Martin Marprelate," against the episcopacy of the Anglican reformed church in 1589, and answered Martin on behalf of the orthodox church.
Appleton's new book, an expansion of her 1985 monograph, is the most comprehensive study of the attribution of the Pasquill pamphlets ever done.
Appleton's inference that de Vere was the mind and pen behind "Pasquill" (a name which, incidentally, although of course Italian in origin, makes a stunning Anglo-French pun on the loss of public identity invoked in the adoption of the pseudonym: "ne pas quill").
Appleton, Edward V. (1892-1965) -- from Eric Weisstein's World of Scientific Biography (100 words)
Appleton, Edward V. English physicist who studied the fading of radio signals.
In 1924, Appleton found the Kennelly-Heaviside layer was about 60 miles high, and that it indeed broke up at night.
By 1926, Appleton determined the higher permanent layer to be at a height of about 150 miles.
  More results at FactBites »


 
 

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