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The r-unit at 320 and 160 Mev

Autore: Edwin M McMillan; Wade Blocker; Robert W Kenney; U.S. Atomic Energy Commission.; Lawrence Radiation Laboratory.
Editore: Oak Ridge, Tenn. : U.S. Atomic Energy Commission, Technical Information Service, 1950.
Serie: UCRL (Series), 1004.
Edizione/Formato:   Libro : National government publication : EnglishVedi tutte le edizioni e i formati
Banca dati:WorldCat
Sommario:
The r-unit is used today in at least two different ways: as a measure of radiation dosage, and as a measure of x-ray intensity. The meaning of the former is fairly well defined in terms of energy absorbed per gram of tissue, and the standard thimble chambers are calibrated to read in these terms. The meaning of the latter is much less clear. As originally defined, the r-unit referred to the ionization in air due to  Per saperne di più…
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Informazioni aggiuntive sul formato: Online version:
McMillan, Edwin M. (Edwin Mattison), 1907-
R-unit at 320 and 160 Mev.
Oak Ridge, Tenn. : U.S. Atomic Energy Commission, Technical Information Service, 1950
(OCoLC)852767089
Tipo materiale: Government publication, National government publication
Tipo documento: Book
Tutti gli autori / Collaboratori: Edwin M McMillan; Wade Blocker; Robert W Kenney; U.S. Atomic Energy Commission.; Lawrence Radiation Laboratory.
Numero OCLC: 796815662
Note: "November 10, 1950."
Work performed at the Radiation Laboratory, University of California.
Descrizione: 5 p. ; 28 cm.
Titolo della serie: UCRL (Series), 1004.
Altri titoli: Technical Report Archive & Image Library (TRAIL)
Responsabilità: By Edwin M. McMillan, Wade Blocker [and] Robert W. Kenney/

Abstract:

The r-unit is used today in at least two different ways: as a measure of radiation dosage, and as a measure of x-ray intensity. The meaning of the former is fairly well defined in terms of energy absorbed per gram of tissue, and the standard thimble chambers are calibrated to read in these terms. The meaning of the latter is much less clear. As originally defined, the r-unit referred to the ionization in air due to secondary electrons in equilibrium with the primary beam of x-rays. With low-energy x-rays equilibrium is easily attained since the range of the secondaries is small compared with the absorption distance of the primaries in air, but with high-energy-x-rays this is no longer true. Since a clearly defined equilibrium no longer exists, the old definition must be abandoned and the question remains: what should the r-unit mean in connection with the intensity of a beam of high-energy x-rays?

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