Sponsor:
This present research was funded by the Community of Madrid
under the GEOMATERIALES 2 project (S2013/MIT-2914), by the
Complutense University of Madrid’s Research Group: “The Alteration
and Conservation of Stone Heritage” (921349), the Autonomous
Region Program of Madrid, MULTIMAT-CHALLENGE (ref.
S2013/MIT‐2862), the Innovation and Education Ministry ref.
(MAT2013-47460-C5-5-P) and the Mat201019837/C06-05 projects.
Project:
Comunidad de Madrid. GEOMATERIALES 2 (S2013/MIT-2914) Comunidad de Madrid. S2013/MIT-2862 MULTIMAT-CHALLENGE Gobierno de España. MAT2013-47460-C5-5-P Gobierno de España. MAT2010-19837/C06-05
Rights:
Published by Elsevier Ltd and Techna Group S.r.l. Atribución-NoComercial-SinDerivadas 3.0 España
Abstract:
The dehydration process from Mg0.97Ca0.03 (OH)(2) nanoparticles (brucite type hexagonal structure) to Mg0.97Ca0.03 (periclase type cubic structure) was studied by Transmission Electron Microscopy (TEM-HRTEM), Electron Diffraction (SAED), Electron Energy Loss SThe dehydration process from Mg0.97Ca0.03 (OH)(2) nanoparticles (brucite type hexagonal structure) to Mg0.97Ca0.03 (periclase type cubic structure) was studied by Transmission Electron Microscopy (TEM-HRTEM), Electron Diffraction (SAED), Electron Energy Loss Spectroscopy (EELS) and image analysis. The transformation process was monitored in function of the reaction time applying 200 and 300 KV. Changes in porosity were possible to observe only during the irradiation with 200 KV. Depending on the irradiation time, the changes were gradual, producing an increase from the particle's edge towards the inner region. Different stages were observed, corresponding to the amount of water extracted from the particle, until finally a decrease in porosity and particle shrinkage occurs, coinciding with the formation of the Mg-Ca oxide.[+][-]