Rubidium Isotope Materials
In both terrestrial materials and chondrites, δ(87Rb) values usually do not vary by more than 1–2 ‰, indicating a very homogeneous mixture of rubidium isotopes throughout the solar system. Owing to this isotopic invariability, changes in the rubidium isotope ratio have only rarely been studied.
Name | Material | δSRM984(87Rb) |
---|---|---|
NIST SRM 984 | RbCl | 0 ‰* |
IRMM-619 | RbNO3 solution | 0(1) ‰ |
Name | Material | δSRM984(87Rb) |
* Exact value defining the δ(87Rb) SRM984 scale.
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)