2007
DOI: 10.1016/j.ijms.2006.07.026
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The isotope abundances and the atomic weight of cadmium by a metrological approach

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Cited by 42 publications
(56 citation statements)
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“…The Commission has changed the recommended value for the standard atomic weight of cadmium, A r (Cd), to 112.414(4) from 112.411(8) based on an evaluation published by Pritzkow et al [45]. While the majority of atomic-weight determinations of multi-isotopic elements employ a single gravimetrically prepared mixture of two near-pure isotopes, this work is a tour de force of seven near-pure isotopes of cadmium (cadmium has a total of eight stable isotopes).…”
Section: Cadmiummentioning
confidence: 99%
“…The Commission has changed the recommended value for the standard atomic weight of cadmium, A r (Cd), to 112.414(4) from 112.411(8) based on an evaluation published by Pritzkow et al [45]. While the majority of atomic-weight determinations of multi-isotopic elements employ a single gravimetrically prepared mixture of two near-pure isotopes, this work is a tour de force of seven near-pure isotopes of cadmium (cadmium has a total of eight stable isotopes).…”
Section: Cadmiummentioning
confidence: 99%
“…Further, stable isotopes of these elements may somehow fall into both groups: traditional as well as non-traditional stable isotopes, depending on the isotopes of interest and the ratios being calculated. The natural variation of the 87 Sr/ 86 Sr isotope ratio, as a result of the radioactive decay of 87 Rb, has been used for decades in geochronology and can -in good conscience -be considered as a traditional isotope ratio. In contrast to that the other three naturally occurring isotopes 84 Sr, 86 Sr and 88 Sr have been taken as invariant in nature until the early 2000s when first papers about an observed variation were published.…”
Section: What Is a Non-traditional Stable Isotope?mentioning
confidence: 99%
“…Industrial Cd emissions are prone to processes that involve evaporation and condensation, which induce significant fractionation effects (< 1 ‰ for 114 Cd/ 110 Cd), thus providing potential signatures to trace human sources of Cd in the environment [32]. The extent of isotopic fractionation of Cd is rather low compared to the traditional systems, not significantly exceeding the range from -3.6 ‰ to +3.4 ‰ in terrestrial materials [87]. So far, the largest Cd isotope fractionations were determined in oceanic environments (up to 4 ‰ for 114 Cd/ 110 Cd) and attributed to biological uptake and utilization of dissolved seawater Cd [88].…”
Section: Fig 4 Distribution Of Publications Between 2010 and 2015 Fomentioning
confidence: 99%
“…Most of these local laboratory materials are not available as a general resource internationally. Pritzkow et al [266] prepared and characterized a material named Cd-2211, which they suggested as the zero-delta material, but which is not yet commercially available. On this scale, the BAM-I012 material (named Cd-I012 herein) is listed with δ…”
Section: Cadmiummentioning
confidence: 99%