“…However, a semi-quantitative approach based on the use of the natural abundance of the three Si isotopes leads to the conclusion that approximately 65% of the 14-Da peak in austenite can be attributed to N. In the rest of the paper, the contribution of the peaks at 14, 14.5, and 15 Da will be reported as 'Si + N'. For ferrite, because of the absence of N, this contribution is purely Si, whereas for austenite, knowing the natural abundance of 28 Si (92.22%), the respective contributions of Si and N are estimated to be approximately 40% and 60%, respectively. In aged martensite, Si and N were also shown to be present in the 14-Da peak in the same proportions as in austenite.…”