Abstract:This work aimed to employ differential scanning calorimetry to find the possible desidroxylation/amorphization temperatures of the main minerals composing a particular soil clay fraction, as well as characterize this fraction mineralogically through XRD at several temperatures. The clay fraction comes from the hardsetting horizon of a Yellow Latosol (Oxisol) formed from sandy and sandy-clayey non-consolidated sediments from the Barreiras formation (Pará State). Considering the soil solid phase, composed of org… Show more
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