Проект Жданова Романа
Ernest Rutherford
Biography
Ernest Rutherford was born on August 30, 1871, in Nelson, New Zealand, the fourth child
and second son in a family of seven sons and five daughters. His father James
Rutherford, a Scottish wheelwright, emigrated to New Zealand with Ernest's
grandfather and the whole family in 1842. His mother, née Martha Thompson, was
an English schoolteacher, who, with her widowed mother, also went to live there
in 1855.
Ernest received his early education in Government schools and at the
age of 16 entered Nelson Collegiate School. In 1889 he was awarded a University
scholarship and he proceeded to the University of New Zealand, Wellington,
where he entered Canterbury College*. He graduated M.A. in 1893 with a double first in Mathematics and Physical
Science and he continued with research work at the College for a short time,
receiving the B.Sc. degree the following year.
That same year, 1894, he was
awarded an 1851 Exhibition Science Scholarship, enabling him to go to Trinity
College, Cambridge, as a research student at the Cavendish Laboratory
under J.J. Thomson. In 1897 he was awarded the B.A.
Research Degree and the Coutts-Trotter Studentship of Trinity College. An
opportunity came when the Macdonald Chair of Physics at McGill University,
Montreal, became vacant, and in 1898 he left for Canada to take up the post. Rutherford
returned to England in 1907 to become Langworthy Professor of Physics in the
University of Manchester, succeeding Sir Arthur Schuster, and in 1919 he
accepted an invitation to succeed Sir Joseph Thomson as Cavendish Professor of
Physics at Cambridge.
He also became Chairman of the Advisory Council, H.M. Government,
Department of Scientific and Industrial Research; Professor of Natural
Philosophy, Royal Institution, London; and Director of the Royal Society Mond
Laboratory, Cambridge. Rutherford's first researches, in New Zealand, were
concerned with the magnetic properties of iron exposed to high-frequency
oscillations, and his thesis was entitled Magnetization of Iron by
High-Frequency Discharges. He was one of the first to design highly
original experiments with high-frequency, alternating currents. His second
paper, Magnetic Viscosity, was published in the Transactions
of the New Zealand Institute (1896) and contains a description of a
time-apparatus capable of measuring time intervals of a hundred-thousandth of a
second. On his arrival at Cambridge his talents were quickly recognized by
Professor Thomson.
During his first spell at the Cavendish Laboratory, he
invented a detector for electromagnetic waves, an essential feature being an
ingenious magnetizing coil containing tiny bundles of magnetized iron wire. He
worked jointly with Thomson on the behaviour of the ions observed in gases
which had been treated with X-rays, and also, in 1897, on the mobility of ions
in relation to the strength of the electric field, and on related topics such
as the photoelectric effect.
In 1898 he reported the existence of alpha and
beta rays in uranium radiation and indicated some of their properties. In
Montreal, there were ample opportunities for research at McGill, and his work
on radioactive bodies, particularly on the emission of alpha rays, was
continued in the Macdonald Laboratory. With R.B. Owens he studied the
"emanation" of thorium and discovered a new noble gas, an isotope of
radon, which was later to be known as thoron.
Frederick
Soddy arrived at McGill in 1900 from Oxford, and he collaborated with
Rutherford in creating the "disintegration
theory" of radioactivity which regards radioactive phenomena as atomic -
not molecular - processes. The theory was supported by a large amount of
experimental evidence, a number of new radioactive substances were discovered
and their position in the series of transformations was fixed.
Otto Hahn, who later discovered atomic fission, worked under
Rutherford at the Montreal Laboratory in 1905-06. At Manchester, Rutherford
continued his research on the properties of the radium emanation and of the
alpha rays and, in conjunction with H. Geiger, a method of detecting a single
alpha particle and counting the number emitted from radium was devised. In
1910, his investigations into the scattering of alpha rays and the nature of
the inner structure of the atom which caused such scattering led to the
postulation of his concept of the "nucleus", his greatest
contribution to physics. According to him practically the whole mass of the
atom and at the same time all positive charge of the atom is concentrated in a
minute space at the centre.
In 1912 Niels Bohr joined him at Manchester and he adapted Rutherford's nuclear
structure to Max Planck's quantum theory and so obtained a theory of atomic structure
which, with later improvements, mainly as a result of Heisenberg's concepts,
remains valid to this day.
In 1913, together with H. G. Moseley, he 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 and, more important, the
properties of each element could be defined by this number.
In 1919, during his
last year at Manchester, he discovered that the nuclei of certain light
elements, such as nitrogen, could be "disintegrated" by the impact of
energetic alpha particles coming from some radioactive source, and that during
this process fast protons were emitted. Blackett later proved, with the cloud chamber, that the nitrogen in this
process was actually transformed into an oxygen isotope, so that Rutherford was
the first to deliberately transmute one element into another. G. de Hevesy was
also one of Rutherford's collaborators at Manchester.
An
inspiring leader of the Cavendish Laboratory, he steered numerous future Nobel
Prize winners towards their great achievements: Chadwick, Blackett, Cockcroft and Walton; while
other laureates worked with him at the Cavendish for shorter or longer
periods: G.P. Thomson,Appleton, Powell,
and Aston. C.D. Ellis, his co-author in 1919 and 1930, pointed out
"that the majority of the experiments at the Cavendish were really started
by Rutherford's direct or indirect suggestion". He remained active and
working to the very end of his life. Rutherford married Mary Newton, only
daughter of Arthur and Mary de Renzy Newton, in 1900.
Their only child, Eileen,
married the physicist R.H. Fowler. Rutherford's chief recreations were golf and
motoring. He died in Cambridge on October 19, 1937. His ashes were buried in
the nave of Westminster Abbey, just west of Sir Isaac Newton's tomb and by that
of Lord Kelvin.
Словарь:
wheelwright- колесник
widowed -вдова
awarded - награжденный
proceeded -продолжаемый
graduated -окончил
following-после
enabling-позволяющей
opportunity -возможность
accepted –принимать
invitation -приглашение
chairman -председатель
Advisory Council- консультативный совет
concerned -заинтересованными
magnetic properties of iron exposed - магнитный свойства железа подвергаются
high-frequency oscillations - высокочастотные колебания
entitled-право
Magnetization of Iron by High-Frequency Discharges-намагничиваемость железа высокочастотными разрядами
alternating currents – переменный ток
Magnetic Viscosity – магнитная вязкость
contains – сожержит
description – описание
a time-apparatus capable of measuring time intervals время-аппарата, способного измерить интервалы времени
arrival – прибытие
recognized – признать
waves-волны
essential-существенный
ingenious-гениальное
coil – катушка
tiny- крошечные
bundles – связки
wire – провода
jointly - совместно
behaviour - поведение
observed – соблюдается
treated- обработаны
relation – связи
strength – прочность
field – поле
related – связанных
topics – темы
reported – сообщили
existence – существование
indicated – указано
properties – свойства
ample – широкие
particularly – в частности
emanation – излучение
thorium – торий
noble – благородный
collaborated – сотрудничал
creating – создание
disintegration – распад
regards – касается
as atomic - not molecular – processes - как атомно - не молекулярно – процессов
supported – поддерживаемые
amount – объем
evidence – доказательства
transformations – преобразований
fission – деления
conjunction – связи
detecting – обнаружения
particle – частиц
counting – подсчет
emitted – излучаемые
devised – разработан
investigations – исследования
scattering – рассеяние
inner – внутренний
caused – причиной
led – привело
nucleus – ядро
contribution – вклад
according – в соответствие
positive – положительные
charge – заряд
joined – присоединился к
adapted – адаптировался
obtained – получены
remains - остается
valid – действительной
assigned – назначен
certain – некоторые
disintegrated – распадается
impact – влияние
defined – определены
nitrogen – азот
source –источник
emitted – излучаемая
proved – доказал
cloud chamber – камера Вильсона
actually – на самом деле
deliberately transmute – намерено
трансмутировать
collaborators – сотрудники
аn inspiring – вдохновляющим
steered – управляемые
pointed out – указал
majority – большинство
direct – прямой
suggestion – предложение
chief – главный
recreations – развлечения
motoring – автоспорт
ashes – пепел
buried – похоронен
tomb - гробница
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