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In Situ Observation of Domain Structure in Monolayers of Arachidic Acid/Fe2O3 Nanoparticle Complexes at the Air/Water Interface

Year: 2002

Journal: J. Phys. Chem. B 2002, 106, 9341-9346, 20111221

Authors: Young Soo Kang, Don Keun Lee, Choong Sub Lee and Pieter Stroeve

Organizations: a Department of Chemistry, Pukyong National University, Pusan 608-737, Korea b Department of Chemical Engineering and Materials Science, University of California, Davis, California 95616

γThe Langmuir layer behavior of arachidic acid/γ-Fe2O3 nanoparticle complexes was studied at the air/water interface. The subphase was an aqueous colloidal solution (hydrosol) of γ-Fe2O3 nanoparticles with an average diameter of 8.3 nm and with a standard deviation of (1.4 nm. Formation of the complex between arachidic acid and γ-Fe2O3 nanoparticles was studied with surface pressure-area isotherms, surface potential-area isotherms and Brewster angle microscopy. Increasing surface pressure resulted in a transition from wellseparated domains of the complex to well-compressed, nanoparticulate layers and, ultimately, to multiparticulate layers. The magnetic nanoparticles and layers of nanoparticles on solid substrates were studied with FTIR, Mössbauer spectroscopy and vibrating sample magnetometry (VSM). The γ-Fe2O3 nanoparticles and Langmuir-Blodgett films with the nanoparticles showed superparamagnetic properties. The stability of the γ-Fe2O3 nanoparticle hydrosol solution was studied by ζ potential measurements. Positively charged γ-Fe2O3 nanoparticles in aqueous hydrosol solution at pH 3.5-5 showed excellent long-term colloidal stability.