“…The regression model, which also uses a primary isotope reference material of a different element but is not derived from either the exponential or the Russell law, is one of the most state-of-the-art methods for instrumental fractionation correction. , Initially proposed by Marechal et al, this model was modified and applied for the determination of absolute isotopic composition and atomic weight of Ge and In. , Further development of the modified regression model led to the reduction of measurement time from 6–15 h to less than 30 min per session. ,, By means of this optimized regression model (ORM), the absolute isotopic composition was re-established for such elements as Ir, Mo, Pb, Os, Lu, and Hf, ,− and most of the results obtained were adopted by IUPAC as best atomic weight values (Ir, Hf, Ge, In). Moreover, after the primary validation of ORM, it was additionally cross-validated with the expensive full gravimetric isotope mixture model, which on the contrary requires matrix matching .…”