Insights of the formation mechanism of nanostructured titanium oxide polymorphs from different macromolecular metal-complex precursors
Patricio Allende,
Alodia Orera,
Miguel Á. Laguna-Bercero,
María Luisa Valenzuela,
Carlos Díaz,
Lorena Barrientos
Affiliations
Patricio Allende
Departamento de Química, Universidad Católica del Norte, Avda Angamos, 0610, Antofagasta, Chile
Alodia Orera
Instituto de Nanociencia y Materiales de Aragón (INMA), CSIC-Universidad de Zaragoza, 50009, Zaragoza, Spain
Miguel Á. Laguna-Bercero
Instituto de Nanociencia y Materiales de Aragón (INMA), CSIC-Universidad de Zaragoza, 50009, Zaragoza, Spain; Corresponding author.
María Luisa Valenzuela
Universidad Autónoma de Chile, Institute of Applied Chemical Sciences, Inorganic Chemistry and Molecular Materials Group, Facultad de Ingeneria, Porvenir 580, Edificio L, Primer Piso, Temuco, Chile
Carlos Díaz
Departamento de Química, Facultad de Química, Universidad de Chile, La Palmeras 3425, Nuñoa, Casilla, 653, Santiago de Chile, Chile
Lorena Barrientos
Facultad de Química y de Farmacia, Centro de Investigación en Nanotecnología y Materiales Avanzados CIEN-UC, Pontificia Universidad Católica de Chile, Vicuña Mackenna, 4860, Macul, Santiago de Chile, Chile; Millennium Nuclei on Catalytic Processes Towards Sustainable Chemistry (CSC), Chile
The insight into the mechanism of the unprecedented formation of pure anatase TiO2 from the macromolecular (Chitosan)•(TiOSO4)n precursor has been investigated using micro Raman spectroscopy, Scanning Electron Microscopy (SEM) and thermogravimetric/differential thermal analysis (TGA/DTA). The formation of a graphitic film was observed upon annealing of the macromolecular precursor, reaching a maximum at about 500 °C due to decomposition of the polymeric chain of the Chitosan and (PS-co-4-PVP) polymers. The proposed mechanism is the nucleation and growth of TiO2 nanoparticles over this graphitic substrate. SEM and Raman measurements confirm the formation of TiO2 anatase around 400 °C. The observation of an exothermic peak around 260 °C in the TGA/DTA measurements confirms the decomposition of carbon chains to form graphite. Another exothermic peak around 560 °C corresponds to the loss of additional carbonaceous residues.