“…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 .…”