José D. Ayala
Universidade Federal de Minas Gerais
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Química Nova | 2009
Láuris Lucia da Silva; Claudio Luis Donnici; José D. Ayala; Cíntia Helena de Freitas; Rubens Martins Moreira; Amenônia Maria Ferreira Pinto
This paper presents a revision of the history, definitions, and classification of tracers (natural and artificial, internal and external). The fundamental ideas concerning tracers are described, followed by their application illustrated by typical examples. The advantages and disadvantages of five classes among the most frequently used external tracers (fluorescent, microbial, chemical, radioactive and activable isotopes) are also described in detail. This review also presents some interesting and modern applications of tracers in the areas of diagnostics in medical practice, environmental pollution, hydrology and petroleum chemistry.
Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy | 2014
Alex Borges; Jeferson G. Da Silva; José D. Ayala; José Diogo L. Dutra; Nivaldo L. Speziali; Hermi F. Brito; Maria Helena Araujo
New anionic complexes of lanthanide picrates containing 1-ethyl-3-methylimidazolium (EMIm) as countercation have been prepared. The Ln(III) complexes were characterized by complexometric titration, elemental analyses, infrared spectroscopy and molar conductivity. The molecular structures of the (EMIm)2[Ln(Pic)4(H2O)2]Pic complexes, Ln(III)=Sm, Eu, Gd and Tb, and Pic=picrate, were determined by X-ray crystallography. In these structures the picrate anion appears in three forms: as uncoordinated counteranion, as monodentated and bidentate ligand. The coordination polyhedron around the Ln(III) atom can be described as tricapped trigonal prismatic molecular geometry. The theoretical molecular structures of the complexes were also calculated using the Sparkle/PM3 model for Ln(III) complexes, allowing analysis of intramolecular energy transfer processes of the Eu(III) compound. The spectroscopic properties of the 4f(6) intraconfigurational transitions of the Eu(III) complex were then studied experimentally and theoretically. The low value of emission quantum efficiency of (5)D0 emitting level (η) of Eu(III) ion (ca. 10%) is due to the vibrational modes of the water molecule that act as luminescence quenching. In addition, the luminescence decay curves, the experimental intensity parameters (Ωλ), lifetimes (τ), radiative (Arad) and non-radiative (Anrad) decay rates, theoretical quantum yield (q) were also determined and discussed.
Acta Crystallographica Section E-structure Reports Online | 2008
Érica G. Gravina; José D. Ayala; Nelson G. Fernandes
A natural sample of perovskite (calcium caesium sodium iron titanium oxide) from the Tapira Alkaline Complex in southeastern Brazil was found by electron microprobe analysis to have the chemical formula (Ca2+ 0.95 (1)Ce3+ 0.011 (2)Na+ 0.010 (4))(Fe3+ 0.022 (2)Ti4+ 0.98 (1))O2− 3 and by IR spectroscopy to be an anhydrous mineral. Oxygen anions are arranged around Ti4+ in an almost perfect octahedron and around Ca2+ in a distorted 12-fold polyhedron.
Acta Crystallographica Section E-structure Reports Online | 2008
Érica G. Gravina; José D. Ayala; Nelson G. Fernandes
A natural sample of perovskite (calcium caesium sodium iron titanium oxide) from the Tapira Alkaline Complex in southeastern Brazil was found by electron microprobe analysis to have the chemical formula (Ca2+ 0.95 (1)Ce3+ 0.011 (2)Na+ 0.010 (4))(Fe3+ 0.022 (2)Ti4+ 0.98 (1))O2− 3 and by IR spectroscopy to be an anhydrous mineral. Oxygen anions are arranged around Ti4+ in an almost perfect octahedron and around Ca2+ in a distorted 12-fold polyhedron.
Acta Crystallographica Section E-structure Reports Online | 2008
Érica G. Gravina; José D. Ayala; Nelson G. Fernandes
A natural sample of perovskite (calcium caesium sodium iron titanium oxide) from the Tapira Alkaline Complex in southeastern Brazil was found by electron microprobe analysis to have the chemical formula (Ca2+ 0.95 (1)Ce3+ 0.011 (2)Na+ 0.010 (4))(Fe3+ 0.022 (2)Ti4+ 0.98 (1))O2− 3 and by IR spectroscopy to be an anhydrous mineral. Oxygen anions are arranged around Ti4+ in an almost perfect octahedron and around Ca2+ in a distorted 12-fold polyhedron.
Polyhedron | 2004
V.D. de Castro; Geraldo M. de Lima; A.O. Porto; Helmuth G. L. Siebald; José Dias de Souza Filho; José D. Ardisson; José D. Ayala; Gabriella Bombieri
ABSTRACTS OF PAPERS - AMERICAN CHEMICAL SOCIETY | 2005
Heloisa Beraldo; G.M. de Lima; Anayive Pérez-Rebolledo; Nicoletta Marchini; Gabriella Bombieri; Elaine Maria de Souza Fagundes; Carlos L. Zani; José D. Ayala
Archive | 2009
Láuris Lucia da Silva; Claudio Luis Donnici; José D. Ayala; Rubens Martins Moreira; Amenônia Maria Ferreira Pinto
Acta Crystallographica Section E-structure Reports Online | 2008
Érica G. Gravina; José D. Ayala; Nelson G. Fernandes
Journal of Chemical Crystallography | 1995
José D. Ayala; Gabriella Bombieri; Franco Benetollo