Calcium Isotope Materials
Terrestrial isotopic-abundance variations for calcium are largest for biological systems, whereas inorganic materials exhibit only small calcium isotopic fractionations. Calcium-40 may be a poor choice for the denominator in the isotope ratio measurements because 40Ca is a product of 40K radioactive decay.
Name | Material | δSRM915a(44/42Ca) |
---|---|---|
NIST SRM 915a | CaCO3 | 0 ‰* |
NIST SRM 915 | CaCO3 | +0.085 ‰ ** |
IAPSO | seawater | +0.88(11) ‰ |
USGS EN-1 | shell from marine organism | +0.35(9) ‰ |
Name | Material | δSRM915a(44/42Ca) |
* Exact value defining the δ(44/42Ca) SRM915a scale.
** See the Assessment of international reference materials for isotope-ratio analysis for more details.
Values in parenthesis are expanded (k = 2) uncertainties applicable to the last digits. The values listed in this table are compilation and are not necessarily CIAAW recommendations.
Citation
W.A. Brand et al
Assessment of international reference materials for isotope-ratio analysis
Pure and Applied Chemistry 86, 425-467 (2014)