1993
DOI: 10.1351/pac199365112361
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Depth of origin of sputtered atoms (Technical Report)

Abstract: Names of countries given after Members' names are in accordance with the ZUPAC Handbook 1991-93; changes will be effected in the 1993-95 edition.Republication of this report is permitted without the need for formal IUPAC permission on condition that an acknowledgement, with full reference together with IUPAC copyright symbol (0 I993 IUPAC), is printed.Publication of a translation into another language is subject to the additional condition of prior approval from the relevant IUPAC National Adhering Organizatio… Show more

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Cited by 8 publications
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“…The first factor, the composition of the sputtered flux, is dominantly affected by the oxidation state of the sample surface. The depth of origin of sputtered species is only 1–2 monolayers, and it is well-known that U sputters overwhelmingly as uranium oxides when oxygen is present on the surface. Measurements on cuprosklodowskite, a uranium-bearing silicate mineral, showed a RIMS useful yield of 5 × 10 –5 , which was attributed to the dominance of oxides in the sputtered flux .…”
Section: Resultsmentioning
confidence: 99%
“…The first factor, the composition of the sputtered flux, is dominantly affected by the oxidation state of the sample surface. The depth of origin of sputtered species is only 1–2 monolayers, and it is well-known that U sputters overwhelmingly as uranium oxides when oxygen is present on the surface. Measurements on cuprosklodowskite, a uranium-bearing silicate mineral, showed a RIMS useful yield of 5 × 10 –5 , which was attributed to the dominance of oxides in the sputtered flux .…”
Section: Resultsmentioning
confidence: 99%