Ernest Rutherford, 1st Baron Rutherford of Nelson was a New Zealand chemist who has become known as the “father of nuclear physics.” In 1911, he was the first to discover that atoms have a small charged nucleus surrounded by largely empty space, and are circled by tiny electrons, which became known as the Rutherford model (or planetary model) of the atom. He is also credited with the discovery of the proton in 1919 and hypothesized the existence of the neutron. He was awarded the Nobel Prize in Chemistry in 1908 “for his investigations into the disintegration of the elements, and the chemistry of radioactive substances.”
Education and Influences
Ernest Rutherford was born on 30 August 1871 in Spring Grove (now called Brightwater) near Nelson, New Zealand, the fourth of twelve children of a Scottish farmer and an English schoolteacher. He was educated at Havelock School and then, at age 16, Nelson Collegiate School, before winning a scholarship to study at Canterbury College at the University of New Zealand in Wellington in 1889. He graduated with an MA in 1893, with a double first in Mathematics and Physical Science.
He continued with research work at Canterbury College for a short time, receiving a BSc degree in 1894, before traveling to England in 1895 for postgraduate study at the Cavendish Laboratory at the University of Cambridge, where he studied under J. J. Thompson (soon to become the discoverer of the electron). During Rutherford’s investigation of radioactivity at Cambridge, he invented an ingenious detector for electromagnetic waves and coined the terms “alpha” and “beta” to describe the two distinct types of radiation emitted by thorium and uranium. In 1897, he was awarded a BA Research Degree and the Coutts-Trotter Studentship of Trinity College, Cambridge.
Contributions and Impact
In 1898, Rutherford was appointed to the vacant chair of physics at McGill University in Montreal, Canada. In 1900, he married Mary Georgina Newton, and they had a daughter, Eileen Mary, the next year.
During his nine years in Montreal, Rutherford collaborated with the young Frederick Soddy (winner of the Nobel Prize in Chemistry in 1921) on ground-breaking research into the transmutation of elements. His “disintegration theory” of radioactivity identified radioactive phenomena as atomic, not molecular, processes, due to the spontaneous disintegration of atoms. He also noticed that a sample of radioactive material invariably took the same amount of time for half the sample to decay (known as its “half-life”) and suggested a practical application using this constant rate of radioactive 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). It was for this work that he was the Nobel Prize in Chemistry in 1908. Otto Hahn (who later discovered nuclear fission) worked under Rutherford at the Montreal Laboratory in 1905 – 1906.
In 1907, Rutherford was appointed a professor of physics at the University of Manchester, England. He directed Hans Geiger and Ernest Marsden in the famous Geiger-Marsden experiment (or “gold-foil experiment”) in 1909, which demonstrated the nuclear nature of atoms. It was his interpretation of these experiments in 1911 that led him to the Rutherford model of the atom, involving a tiny positively-charged nucleus orbited by even tinier negatively-charged electrons, a great advance on J. J. Thomson’s so-called “plum pudding” model.
In 1912, Niels Bohr joined him at Manchester, and Bohr adapted Rutherford’s nuclear structure to Max Planck’s quantum theory, and so obtained a theory of atomic structure which essentially remains valid to this day. In 1913, together with H. G. Moseley, Rutherford used cathode rays to bombard atoms of various elements and showed that the inner structures correspond with a group of lines which characterize the elements. Each element could then be assigned an atomic number which would define its specific properties.
In 1919, Rutherford returned to Cambridge when he was offered the Directorship of the Cavendish Laboratory in Cambridge, a position he retained for many years, effectively until the end of his life. He was considered an inspiring leader of the Cavendish Laboratory, and steered numerous future Nobel Prize winners towards their great achievements (including James Chadwick, Patrick Blackett, John Cockcroft and Ernest Walton) as well as working with many others for shorter or more extended periods (including George Thomson, Edward Appleton, Cecil Powell and Francis Aston).
In 1919, he became the first person to transmute one element into another when he converted nitrogen into oxygen through a nuclear reaction involving the shooting of alpha particles into nitrogen gas. He is also credited with the discovery of the proton when he noticed the signatures of hydrogen nuclei being emitted during this process. While working with Niels Bohr in 1921, he theorized about the existence of neutrons, which could somehow compensate for the repelling effect of the positive charge of protons by causing an attractive nuclear force and thus keeping the nuclei from breaking apart. Rutherford’s theory of neutrons was eventually proved in 1932 by his associate James Chadwick.
Rutherford had been knighted in 1914 and was subsequently awarded the Order of Merit in 1925. In 1931, he was created the 1st Baron Rutherford of Nelson and Cambridge. In addition to directing the Cavendish Laboratory, he also went on to take up several additional positions including Chairman of the Advisory Council of the Department of Scientific and Industrial Research, Professor of Natural Philosophy at the Royal Institution in London and Director of the Royal Society Mond Laboratory in Cambridge. He had been elected a Fellow of the Royal Society back in 1903, and he acted as its President from 1925 to 1930. He was awarded many prizes and honors, including the Rumford Medal, the Copley Medal, the Bressa Prize, the Albert Medal and the Faraday Medal, as well as countless honorary degrees and doctorates.
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