TY - JOUR
T1 - Calorimetric study of maghemite nanoparticles synthesized by laser-induced pyrolysis
AU - Bomatí-Miguel, Oscar
AU - Mazeina, Lena
AU - Navrotsky, Alexandra
AU - Veintemillas-Verdaguer, Sabino
N1 - Copyright:
Copyright 2011 Elsevier B.V., All rights reserved.
PY - 2008/1/22
Y1 - 2008/1/22
N2 - The thermodynamic properties of maghemite (γ-Fe2O 3) nanoparticles with size smaller than 10 nm had not been studied previously because of particle size limitations for samples synthesized by wet chemical methods. Laser-induced pyrolysis is a well-established method of producing maghemite with particle sizes smaller than 10 nm. Maghemite nanoparticles, obtained by this method and having a size range of 2-40 nm, were fully characterized and studied by solution calorimetry. The enthalpy of water adsorption was also measured. The surface enthalpy obtained from calorimetric data for the hydrated maghemite surface is 0.57 ± 0.10 J/m2 and is in good agreement with previously reported values. The surface enthalpy for the dry, water-free surface is 0.71 ± 0.13 J/m2 and is reported for the first time. The difference in the surface enthalpy for the dry surface between α- and γ-polymorphs of Fe2O3 is similar to that between α-and γ-Al2O3. This large difference in surface enthalpy (∼1.2 J/m2) creates an energy crossover so that fine-grained hematite is metastable relative to fine-grained maghemite at particle size <15 nm.
AB - The thermodynamic properties of maghemite (γ-Fe2O 3) nanoparticles with size smaller than 10 nm had not been studied previously because of particle size limitations for samples synthesized by wet chemical methods. Laser-induced pyrolysis is a well-established method of producing maghemite with particle sizes smaller than 10 nm. Maghemite nanoparticles, obtained by this method and having a size range of 2-40 nm, were fully characterized and studied by solution calorimetry. The enthalpy of water adsorption was also measured. The surface enthalpy obtained from calorimetric data for the hydrated maghemite surface is 0.57 ± 0.10 J/m2 and is in good agreement with previously reported values. The surface enthalpy for the dry, water-free surface is 0.71 ± 0.13 J/m2 and is reported for the first time. The difference in the surface enthalpy for the dry surface between α- and γ-polymorphs of Fe2O3 is similar to that between α-and γ-Al2O3. This large difference in surface enthalpy (∼1.2 J/m2) creates an energy crossover so that fine-grained hematite is metastable relative to fine-grained maghemite at particle size <15 nm.
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U2 - 10.1021/cm071178o
DO - 10.1021/cm071178o
M3 - Article
AN - SCOPUS:38949099030
SN - 0897-4756
VL - 20
SP - 591
EP - 598
JO - Chemistry of Materials
JF - Chemistry of Materials
IS - 2
ER -