Alpha particle: Difference between revisions
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Discovered and named (1899) by [[Ernest Rutherford]], α-radiation was used by him and coworkers in experiments that probed the structure of [[atom]]s 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]] by α-particles, changing it to [[oxygen]], producing in 1919 the first artificially nuclear transmutation. | Discovered and named (1899) by [[Ernest Rutherford]], α-radiation was used by him and coworkers in experiments that probed the structure of [[atom]]s 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]] by α-particles, changing it to [[oxygen]], producing in 1919 the first artificially nuclear transmutation. | ||
In 1899<ref>E. Rutherford, Phil. Mag., vol. '''47''', p. 109 (1899)</ref> Rutherford determined some properties of the "Uranic 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 nature of the radiation was an enigma. Ten years later Rutherford knew | In 1899<ref>E. Rutherford, Phil. Mag., vol. '''47''', p. 109 (1899)</ref> Rutherford determined some properties of the "Uranic 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 nature of the radiation was an enigma. The nuclear reactions in the uranium salt likely to have been involved were: | ||
:<sup>238</sup>U<sub>92</sub> → <sup>234</sup>Th<sub>90</sub> + <sup>4</sup>He<sub>2</sub> + γ | |||
[[Beta-radiation]] arises from the "daughter" element [[thorium]] (Th) that becomes [[protactinium]] (Pa) upon emission of a negative elementary charge, | |||
:<sup>234</sup>Th<sub>90</sub> → <sup>234</sup>Pa<sub>91</sub> + β<sup>−</sup> | |||
Ten years later Rutherford knew its nature: he and [[Hans Geiger]] wrote a paper, ''On the Nature of the α-particle'',<ref>E. Rutherford and H. Geiger, Proc. Royal Soc. vol. '''A 81''', p. 162 (1908)</ref> in which it was explained that α-particles are helium atoms that have lost their negative charge. Note that it was not known yet in 1908 that an atom consists of a nucleus plus orbiting electrons, but the existence of atoms had been firmly established at that time. | |||
==Reference== | ==Reference== | ||
<references /> | <references /> |
Revision as of 06:01, 12 June 2009
An alpha particle is a positively charged particle with of 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 (1899) by Ernest Rutherford, α-radiation was used by him and coworkers 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 by α-particles, changing it to oxygen, producing in 1919 the first artificially nuclear transmutation.
In 1899[2] Rutherford determined some properties of the "Uranic rays" (thus named because the most common uranium isotope, 238U, is an α emitter and uranium salts were used as source of α-radiation), but at that time the nature of the radiation was an enigma. The nuclear reactions in the uranium salt likely to have been involved were:
- 238U92 → 234Th90 + 4He2 + γ
Beta-radiation arises from the "daughter" element thorium (Th) that becomes protactinium (Pa) upon emission of a negative elementary charge,
- 234Th90 → 234Pa91 + β−
Ten years later Rutherford knew its nature: he and Hans Geiger wrote a paper, On the Nature of the α-particle,[3] in which it was explained that α-particles are helium atoms that have lost their negative charge. Note that it was not known yet in 1908 that an atom consists of a nucleus plus orbiting electrons, but the existence of atoms had been firmly established at that time.
Reference
- ↑ NIST CODATA Retrieved 12 June 2009
- ↑ E. Rutherford, Phil. Mag., vol. 47, p. 109 (1899)
- ↑ E. Rutherford and H. Geiger, Proc. Royal Soc. vol. A 81, p. 162 (1908)