{"title":"The passage of gamma-rays through water","authors":"V.I. Kukhtevich, Yu.A. Kazanskii, Sh.S. Nikolaishvili, S.G. Tsypin","doi":"10.1016/0891-3919(59)90149-7","DOIUrl":null,"url":null,"abstract":"<div><p>The dosage attenuation in water of γ-rays from <sup>198</sup>Au, <sup>60</sup>Co and <sup>24</sup>Na has been measured as a function of the source-detector distance over a range from some 3–4 to about 8–12 scattering mean free paths. The primary radiation was collimated in such a direction that none fell on the detector, down to an angle which was varied between 30° and 80°. Theoretical intensities have been calculated by an approximate procedure that replaces the direct solution of the kinetic equation by the reduction of a triple integral and are in satisfactory agreement with observation.</p></div>","PeriodicalId":100812,"journal":{"name":"Journal of Nuclear Energy (1954)","volume":"9 1","pages":"Pages 128-134"},"PeriodicalIF":0.0000,"publicationDate":"1959-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0891-3919(59)90149-7","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Nuclear Energy (1954)","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0891391959901497","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The dosage attenuation in water of γ-rays from 198Au, 60Co and 24Na has been measured as a function of the source-detector distance over a range from some 3–4 to about 8–12 scattering mean free paths. The primary radiation was collimated in such a direction that none fell on the detector, down to an angle which was varied between 30° and 80°. Theoretical intensities have been calculated by an approximate procedure that replaces the direct solution of the kinetic equation by the reduction of a triple integral and are in satisfactory agreement with observation.