2016
DOI: 10.1007/s10973-016-5987-4
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Synthesis, Rietveld refinement and DSC analysis of Al-goethites to support mineralogical quantification of gibbsitic bauxites

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Cited by 9 publications
(2 citation statements)
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“…Quartz (d 101 = 3.34 Å) may be present in some samples, but in minor content. Hematite (d 104 = 2.69 Å) is observed as the main iron mineral, with intensity varying significantly among the lithologies, and Al-goethite (d 101 ranging from 4.18 Å to 4.14 Å) is also observed, usually as a broad peak due to variations in the isomorphic substitution of Al in the structure [12,34]. Anatese (d 101 = 3.52 Å) is also present in all samples.…”
Section: Xrd Datamentioning
confidence: 90%
“…Quartz (d 101 = 3.34 Å) may be present in some samples, but in minor content. Hematite (d 104 = 2.69 Å) is observed as the main iron mineral, with intensity varying significantly among the lithologies, and Al-goethite (d 101 ranging from 4.18 Å to 4.14 Å) is also observed, usually as a broad peak due to variations in the isomorphic substitution of Al in the structure [12,34]. Anatese (d 101 = 3.52 Å) is also present in all samples.…”
Section: Xrd Datamentioning
confidence: 90%
“…The applied methodology was based on the study developed by Paz et al (Paz et al, 2017). According to this methodology, the heat of the decarbonation reaction measured by DSC ∼750°C can be used for phase quantification because the ratio between the peak area and the enthalpy can be determined using a temperature-dependent calibration factor.…”
Section: Differential Scanning Calorimetry (Dsc) Combined With Xrd (Pmentioning
confidence: 99%