1991
DOI: 10.1016/0008-8846(91)90097-2
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Mössbauer and X-ray diffraction studies of two dry and hydrated portland cements and their clinker

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(4 citation statements)
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“…[41][42][43][44][45] However, the higher CS values for the abiotic treated cement sample are consistent with the view that the average Fe 3+ coordination number is higher than in the other two samples and consequently there may be small differences in the partitioning of iron between the hydrated phases containing iron. [41][42][43][44][45] The overall absorption intensity for the abiotic HAp samples is similar to that of the untreated cement, indicating a higher iron content than the biogenic HAp sample. This suggests that the HAp layer covering the cement is thinner in the abiotic sample than in the biogenic sample as it is diluting the Fe signal less, which is confirmed by EPMA imaging (as described below, Fig.…”
Section: Impacts Of Treatment On the Composition Speciation And Distribution Of Mineral And Cement Phasessupporting
confidence: 83%
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“…[41][42][43][44][45] However, the higher CS values for the abiotic treated cement sample are consistent with the view that the average Fe 3+ coordination number is higher than in the other two samples and consequently there may be small differences in the partitioning of iron between the hydrated phases containing iron. [41][42][43][44][45] The overall absorption intensity for the abiotic HAp samples is similar to that of the untreated cement, indicating a higher iron content than the biogenic HAp sample. This suggests that the HAp layer covering the cement is thinner in the abiotic sample than in the biogenic sample as it is diluting the Fe signal less, which is confirmed by EPMA imaging (as described below, Fig.…”
Section: Impacts Of Treatment On the Composition Speciation And Distribution Of Mineral And Cement Phasessupporting
confidence: 83%
“…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).…”
Section: Impacts Of Treatment On the Composition Speciation And Distribution Of Mineral And Cement Phasesmentioning
confidence: 65%
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