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Ernest Rutherford
Ernest Rutherford, 1st Baron Rutherford of Nelson OM, FRS (30 August 1871 – 19 October 1937) was a New Zealand-born British chemist and physicist who became known as the father of nuclear physics.[1] In early work he discovered the concept of radioactive half-life, proved that radioactivity involved the transmutation of one chemical element to another, and also differentiated and named alpha and beta radiation. This work was done at McGill University in Canada. It is the basis for the Nobel Prize in Chemistry he was awarded in 1908 "for his investigations into the disintegration of the elements, and the chemistry of radioactive substances".[2]
Rutherford performed his most famous work after he had moved to the U.K. in 1907 and was already a Nobel laureate. In 1911, he postulated that atoms have their positive charge concentrated in a very small nucleus,[3] and thereby pioneered the Rutherford model of the atom, through his discovery and interpretation of Rutherford scattering in his gold foil experiment. He is widely credited with first "splitting the atom" in 1917 in a nuclear reaction between nitrogen and alpha particles, in which he also discovered (and named) the proton.[4] This led to the first experiment to split the nucleus in a fully controlled manner, performed by two students working under his direction, John Cockcroft and Ernest Walton, in 1932.
After his death in 1937, he was honoured by being interred with the greatest scientists of the United Kingdom, near Sir Isaac Newton's tomb in Westminster Abbey. The chemical element rutherfordium (element 104) was named for him in 1997.
Rutherford performed his most famous work after he had moved to the U.K. in 1907 and was already a Nobel laureate. In 1911, he postulated that atoms have their positive charge concentrated in a very small nucleus,[3] and thereby pioneered the Rutherford model of the atom, through his discovery and interpretation of Rutherford scattering in his gold foil experiment. He is widely credited with first "splitting the atom" in 1917 in a nuclear reaction between nitrogen and alpha particles, in which he also discovered (and named) the proton.[4] This led to the first experiment to split the nucleus in a fully controlled manner, performed by two students working under his direction, John Cockcroft and Ernest Walton, in 1932.
After his death in 1937, he was honoured by being interred with the greatest scientists of the United Kingdom, near Sir Isaac Newton's tomb in Westminster Abbey. The chemical element rutherfordium (element 104) was named for him in 1997.
Born 30 August 1871
Brightwater, New Zealand Died 19 October 1937 (aged 66)
Cambridge, England Residence New Zealand, UK, Canada Citizenship United Kingdom Nationality British-New Zealander Fields Physicist-Chemist Institutions McGill University
University of Manchester Alma mater University of Canterbury
University of Cambridge Academic advisors Alexander Bickerton
J. J. Thomson Doctoral students Edward Victor Appleton
Alexander MacAulay
Ernest Walton
Robert William Boyle
Cecil Powell
Nazir Ahmed
Rafi Muhammad Chaudhry
C. E. Wynn-Williams
Other notable students Mark Oliphant
Patrick Blackett
Hans Geiger
Niels Bohr
Otto Hahn
Teddy Bullard
Pyotr Kapitsa
John Cockcroft
Charles Drummond Ellis
James Chadwick
Ernest Marsden
Edward Andrade
Frederick Soddy
Edward Victor Appleton
Bertram Boltwood
Kazimierz Fajans
Charles Galton Darwin
A. J. B. Robertson
George Laurence
Henry DeWolf Smyth
Harriet Brooks
Douglas Hartree
Iven Mackay
Norman Alexander Known for Father of nuclear physics
Rutherford model
Rutherford scattering
Rutherford backscattering spectroscopy
Discovery of proton
Rutherford (unit)
Coining the term 'artificial disintegration' Influenced Henry Moseley
Hans Geiger
Albert Beaumont Wood Notable awards Rumford Medal (1905)
Nobel Prize in Chemistry (1908)
Elliott Cresson Medal (1910)
Matteucci Medal (1913)
Copley Medal (1922)
Franklin Medal (1924)
Brightwater, New Zealand Died 19 October 1937 (aged 66)
Cambridge, England Residence New Zealand, UK, Canada Citizenship United Kingdom Nationality British-New Zealander Fields Physicist-Chemist Institutions McGill University
University of Manchester Alma mater University of Canterbury
University of Cambridge Academic advisors Alexander Bickerton
J. J. Thomson Doctoral students Edward Victor Appleton
Alexander MacAulay
Ernest Walton
Robert William Boyle
Cecil Powell
Nazir Ahmed
Rafi Muhammad Chaudhry
C. E. Wynn-Williams
Other notable students Mark Oliphant
Patrick Blackett
Hans Geiger
Niels Bohr
Otto Hahn
Teddy Bullard
Pyotr Kapitsa
John Cockcroft
Charles Drummond Ellis
James Chadwick
Ernest Marsden
Edward Andrade
Frederick Soddy
Edward Victor Appleton
Bertram Boltwood
Kazimierz Fajans
Charles Galton Darwin
A. J. B. Robertson
George Laurence
Henry DeWolf Smyth
Harriet Brooks
Douglas Hartree
Iven Mackay
Norman Alexander Known for Father of nuclear physics
Rutherford model
Rutherford scattering
Rutherford backscattering spectroscopy
Discovery of proton
Rutherford (unit)
Coining the term 'artificial disintegration' Influenced Henry Moseley
Hans Geiger
Albert Beaumont Wood Notable awards Rumford Medal (1905)
Nobel Prize in Chemistry (1908)
Elliott Cresson Medal (1910)
Matteucci Medal (1913)
Copley Medal (1922)
Franklin Medal (1924)
Scientific research During the investigation of radioactivity he coined the terms alpha ray and beta ray in 1899 to describe the two distinct types of radiation emitted by thorium and uranium. These rays were differentiated on the basis of penetrating power. From 1900 to 1903 he was joined at McGill by the young Frederick Soddy (Nobel Prize in Chemistry, 1921) and they collaborated on research into the transmutation of elements. Rutherford had demonstrated that radioactivity was the spontaneous disintegration of atoms. He noticed that a sample of radioactive material invariably took the same amount of time for half the sample to decay—its "half-life"—and created a practical application using this constant rate of decay as a clock, which could then be used to help determine the age of the Earth, which turned out to be much older than most of the scientists at the time believed.
In 1903, Rutherford realised that a type of radiation from radium discovered (but not named) by French chemist Paul Villard in 1900, must represent something different from alpha rays and beta rays, due to its very much greater penetrating power. Rutherford gave this third type of radiation its name also: the gamma ray.
In Manchester he continued to work with alpha radiation. In conjunction with Hans Geiger he developed zinc sulfide scintillation screens and ionisation chambers to count alphas. By dividing the total charge they produced by the number counted, Rutherford decided that the charge on the alpha was two. In late 1907 Ernest Rutherford and Thomas Royds allowed alphas to penetrate a very thin window into an evacuated tube. As they sparked the tube into discharge, the spectrum obtained from it changed, as the alphas accumulated in the tube. Eventually, the clear spectrum of helium gas appeared, proving that alphas were at least ionised helium atoms, and probably helium nuclei.
Rutherford remains the only science Nobel Prize winner to have performed his most famous work after receiving the prize. Along with Hans Geiger and Ernest Marsden in 1909 he carried out the Geiger–Marsden experiment, which demonstrated the nuclear nature of atoms. Rutherford was inspired to ask Geiger and Marsden in this experiment to look for alpha particles with very high deflection angles, of a type not expected from any theory of matter at that time. Such deflections, through rare, were found, and proved to be a smooth but high-order function of the deflection angle. It was Rutherford's interpretation of this data that led him to formulate the Rutherford model of the atom in 1911 — that a very small positively charged nucleus was orbited by electrons.
Before leaving Manchester in 1919 to take over the Cavendish laboratory in Cambridge, Rutherford became in 1917 the first person to deliberately transmute one element into another, when he converted nitrogen into oxygen through the nuclear reaction 14N + α → 17O + proton. In the products of this reaction he recognized the particle radiation from earlier experiments in which he had bombarded hydrogen gas with alpha particles, and thus as hydrogen nuclei. This result showed that hydrogen nuclei were a part of nitrogen nuclei (and by inference, probably other nuclei as well). Such a construction had been suspected for many years on the basis of atomic weights which were whole numbers of that of hydrogen; see Prout's hypothesis. Now Rutherford decided that a hydrogen nucleus was a fundamental building block and a particle, which he named the proton.
In 1921, while working with Niels Bohr (who postulated that electrons moved in specific orbits), Rutherford theorised about the existence of neutrons, which could somehow compensate for the repelling effect of the positive charges of protons by causing an attractive nuclear force and thus keeping the nuclei from breaking apart. Rutherford's theory of neutrons was proved in 1932 by his associate James Chadwick, who in 1935 was awarded the Nobel Prize in Physics for this discovery.
In 1903, Rutherford realised that a type of radiation from radium discovered (but not named) by French chemist Paul Villard in 1900, must represent something different from alpha rays and beta rays, due to its very much greater penetrating power. Rutherford gave this third type of radiation its name also: the gamma ray.
In Manchester he continued to work with alpha radiation. In conjunction with Hans Geiger he developed zinc sulfide scintillation screens and ionisation chambers to count alphas. By dividing the total charge they produced by the number counted, Rutherford decided that the charge on the alpha was two. In late 1907 Ernest Rutherford and Thomas Royds allowed alphas to penetrate a very thin window into an evacuated tube. As they sparked the tube into discharge, the spectrum obtained from it changed, as the alphas accumulated in the tube. Eventually, the clear spectrum of helium gas appeared, proving that alphas were at least ionised helium atoms, and probably helium nuclei.
Rutherford remains the only science Nobel Prize winner to have performed his most famous work after receiving the prize. Along with Hans Geiger and Ernest Marsden in 1909 he carried out the Geiger–Marsden experiment, which demonstrated the nuclear nature of atoms. Rutherford was inspired to ask Geiger and Marsden in this experiment to look for alpha particles with very high deflection angles, of a type not expected from any theory of matter at that time. Such deflections, through rare, were found, and proved to be a smooth but high-order function of the deflection angle. It was Rutherford's interpretation of this data that led him to formulate the Rutherford model of the atom in 1911 — that a very small positively charged nucleus was orbited by electrons.
Before leaving Manchester in 1919 to take over the Cavendish laboratory in Cambridge, Rutherford became in 1917 the first person to deliberately transmute one element into another, when he converted nitrogen into oxygen through the nuclear reaction 14N + α → 17O + proton. In the products of this reaction he recognized the particle radiation from earlier experiments in which he had bombarded hydrogen gas with alpha particles, and thus as hydrogen nuclei. This result showed that hydrogen nuclei were a part of nitrogen nuclei (and by inference, probably other nuclei as well). Such a construction had been suspected for many years on the basis of atomic weights which were whole numbers of that of hydrogen; see Prout's hypothesis. Now Rutherford decided that a hydrogen nucleus was a fundamental building block and a particle, which he named the proton.
In 1921, while working with Niels Bohr (who postulated that electrons moved in specific orbits), Rutherford theorised about the existence of neutrons, which could somehow compensate for the repelling effect of the positive charges of protons by causing an attractive nuclear force and thus keeping the nuclei from breaking apart. Rutherford's theory of neutrons was proved in 1932 by his associate James Chadwick, who in 1935 was awarded the Nobel Prize in Physics for this discovery.