“…All 57 Fe Mössbauer spectra could be fitted with two doublets (D1: centre shift: 0.26-0.42 mm s -1 , quadrupole splitting: 0.41-0.49 mm s -1 , and D2: centre shift: 0.23-0.45 mm s -1 , quadrupole splitting: 1.21-1.61 mm s -1 , Table 2). These doublets (within experimental uncertainties and taking into account the low signal-to-noise ratio) indicate the existence of at least two different paramagnetic Fe 3+ sites and that all of the observed iron is present as ferric iron in all three of the cement samples [41][42][43][44][45] . The hyperfine parameters from fitting the Mössbauer spectra associated with the cement samples are all fully consistent with values for cement from Harchand et al (D1: centre shift: 0.278 mm s -1 , quadrupole splitting: 0.428 mm s -1 , and D2: centre shift: 0.285 mm s -1 , quadrupole splitting: 1.667 mm s -1 , Table 2).…”