Orbital - Vol. 8 No. 6 - October - December 2016
FULL PAPERS

Determination of the Critical Micelle Concentration of Triton X-100 Using the Compound 3-(benzoxazol-2-yl)-7-(N,N-diethylamino)chromen-2-one as Fluorescent Probe

Antonio Eduardo da Hora Machado
Universidade Federal de Uberlândia
Hueder Paulo Moisés de Oliveira
Universidade Federal do ABC
Lidiaine Maria dos Santos
Universidade Federal de Uberlândia
Higor de Oliveira Alves
Universidade Federal de Uberlândia
Werick Alves Machado
Universidade Federal de Uberlândia
Bruno Pontes Caixeta
Universidade Federal de Uberlândia
Tatiana Aparecida da Silva
Universidade Federal de Uberlândia
Diesley Martins da Silva Araújo
Universidade Federal de Uberlândia
Published December 26, 2016
Keywords
  • critical micelle concentration,
  • Triton X-100,
  • extrinsic fluorescence,
  • 3-(benzoxazol-2-yl)-7-(N,N-diethylamino)chromen-2-one,
  • polarity,
  • viscosity
  • ...More
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How to Cite
(1)
Machado, A. E. da H.; de Oliveira, H. P. M.; dos Santos, L. M.; Alves, H. de O.; Machado, W. A.; Caixeta, B. P.; da Silva, T. A.; Araújo, D. M. da S. Determination of the Critical Micelle Concentration of Triton X-100 Using the Compound 3-(benzoxazol-2-Yl)-7-(N,N-diethylamino)chromen-2-One As Fluorescent Probe. Orbital: Electron. J. Chem. 2016, 8, 329-333.

Abstract

In the present study we estimated the Critical Micelle Concentration (CMC) of Triton X-100 in an aqueous buffered medium (PBS buffer, pH 7.4), using 3-(benzoxazol-2-yl)-7-(N,N-diethylamino)chromen-2-one (BDC), a push-pull compound, as extrinsic fluorescence probe. The CMC value found, 0.33 mmol L-1, shows good agreement with data from literature obtained using the fluorescence probe technique. Additionally, the polarity, in terms of the ET(30) scale, and the viscosity of the micelle microenvironment in which the probe is preferentially allocated, was estimated as being 46.9 kcal mol-1 and 70.3 cP, respectively, confirming that this microdomain is polar and highly viscous, with characteristics of polyethylene glycol groups consisting in the palisade layer at the micelle-water interface.

DOI: http://dx.doi.org/10.17807/orbital.v0i0.923