Alpha particle: Difference between revisions
imported>Ro Thorpe m (→History) |
imported>Mark Widmer m (→History) |
||
| Line 5: | Line 5: | ||
==History== | ==History== | ||
In 1899<ref>E. Rutherford, ''Uranium Radiation and the Electrical conduction Produced by it'', Phil. Mag., vol. '''47''', p. 109 (1899)</ref> Rutherford determined several properties of the "uranium rays" (thus named because the most common [[uranium]] isotope, <sup>238</sup>U, is an α emitter and uranium salts were used as source of α-radiation), but at that time the cause and origin of the radiation emitted by uranium was an enigma. He discovered that there were two kinds of radiation involved, which he called α and β [[radiation]]. In retrospect, the nuclear reactions in the uranium salt likely to have been involved were: | In 1899<ref>E. Rutherford, ''Uranium Radiation and the Electrical conduction Produced by it'', Phil. Mag., vol. '''47''', p. 109 (1899)</ref> Rutherford determined several properties of the "uranium rays" (thus named because the most common [[uranium]] isotope, <sup>238</sup>U, is an α emitter and uranium salts were used as a source of α-radiation), but at that time the cause and origin of the radiation emitted by uranium was an enigma. He discovered that there were two kinds of radiation involved, which he called α and β [[radiation]]. In retrospect, the nuclear reactions in the uranium salt likely to have been involved were: | ||
:<math> | :<math> | ||
{}^{238}_{\,\;92}\mathrm{U} \rightarrow {}^{234}_{\,\;90}\mathrm{Th} + {}^{4}_{2}\mathrm{He} + \gamma | {}^{238}_{\,\;92}\mathrm{U} \rightarrow {}^{234}_{\,\;90}\mathrm{Th} + {}^{4}_{2}\mathrm{He} + \gamma | ||
Revision as of 19:02, 20 September 2021
An alpha particle (α-particle) is a positively charged particle with absolute value of charge 2e, where e is the elementary charge. An α-particle is in fact the nucleus of the helium-4 isotope, consisting of two protons and two neutrons, thus having a mass close to 4 u (u stands for unified atomic mass unit). More precisely: mα = 4.001 506 179 127 u.[1]
Discovered and named in 1899 by Ernest Rutherford, alpha radiation (α-radiation) was used by him and co-workers in experiments that probed the structure of atoms in thin metallic foils, work that resulted in the first conception of the atom as a heavy nucleus with light electrons orbiting the nucleus (1909–1911). Later Rutherford and collaborators bombarded nitrogen with α-particles, changing it to oxygen, producing in 1919 the first artificial nuclear transmutation.
History
In 1899[2] Rutherford determined several properties of the "uranium rays" (thus named because the most common uranium isotope, 238U, is an α emitter and uranium salts were used as a source of α-radiation), but at that time the cause and origin of the radiation emitted by uranium was an enigma. He discovered that there were two kinds of radiation involved, which he called α and β radiation. In retrospect, the nuclear reactions in the uranium salt likely to have been involved were:
Beta-radiation arises from the "daughter" element thorium (Th) that becomes protactinium (Pa) upon emission of a negative elementary charge,
Ten years later Rutherford knew the nature of the α-particle: Hans Geiger and he wrote a paper on its nature and charge,[3] in which it was explained that α-particles are helium atoms that have lost their negative charge. In 1908 it was not yet known that an atom consists of a nucleus plus orbiting electrons, though the existence of atoms had already been firmly established by then.
Reference
- ↑ NIST CODATA Retrieved 12 June 2009
- ↑ E. Rutherford, Uranium Radiation and the Electrical conduction Produced by it, Phil. Mag., vol. 47, p. 109 (1899)
- ↑ E. Rutherford and H. Geiger, The Charge and Nature of the α-particle, Proc. Royal Soc. vol. A 81, p. 162–174 (1908). doi Subscription required
External link
Copy of Rutherford's 1899 paper Retrieved June 12, 2009.