Abstract:The use of the Rietveld Method (RM) with X-ray diffraction data (XRD) in soils becomes difficult in relation to the best adjustment and higher reliability of the mineralogical quantification. One of these difficulties is related to the mineral phase starting crystalline structures, once they derive from natural samples. Therefore, it is necessary to seek starting structures of the mineral present in the soil closer to that found in Brazilian soils. This study analyzed samples coming from the hardsetting of a Y… Show more
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