4.7 Article

J-aggregation of a sulfonated amphiphilic porphyrin at the air-water interface as a function of pH

Journal

JOURNAL OF COLLOID AND INTERFACE SCIENCE
Volume 356, Issue 2, Pages 775-782

Publisher

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jcis.2011.01.066

Keywords

J-aggregation; Soret band splitting; Porphyrinoids; Air-water interface; pH; Thin films

Funding

  1. Spanish CICYT [CTQ2007-64474/BQU, CTQ2010-17481/BQU]
  2. Junta de Andalucia (Consejeria de Innovacion, Ciencia y Empresa) [P08-FQM-4011]
  3. MEXT (Japan) [19350068]
  4. JSPS
  5. Grants-in-Aid for Scientific Research [19350068] Funding Source: KAKEN

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pi-A isotherms, ellipsometric measurements, Brewster angle microscopy (BAM) and reflection spectroscopy have been utilized to characterize the films of an amphiphilic porphyrin ((OD)(3)TPPS3) at the air-water interface as a function of pH. This porphyrin forms stable mono-molecular layers at such interfaces, and exhibits different J-aggregation as a function of pH. The J-aggregation of (OD)(3)TPPS3 on neutral pH subphases is notable considering that the nitrogen atoms at the central macrocycle have a pK(a) approximate to 4.9. The type of aggregates at neutral pH is like those detected at pH <4, because the central porphyrin ring is already protonated. However at basic pH the aggregation happens without protonation of the central ring but can be instead controlled by application of the surface pressure. At the air-water interface, (OD)(3)TPPS3 shows two bands, a red component and a blue component, which have characteristics of non-degenerate linear oscillators being perpendicularly polarized between each other. The spectral behavior observed on subphases at different pHs is qualitatively interpreted by means of exciton coupling theory, assuming that the degenerate transitions attributed to the Soret band are split. Additionally, highly oriented molecular films of these J-aggregates were deposited onto transparent quartz slides. (C) 2011 Elsevier Inc. All rights reserved.

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