In situ observation of domain structure in monolayers of arachidic acid/γ-Fe2O3 nanoparticle complexes at the air/water interface

被引:52
作者
Kang, YS [1 ]
Lee, DK
Lee, CS
Stroeve, P
机构
[1] Pukyong Natl Univ, Dept Chem, Pusan 608737, South Korea
[2] Univ Calif Davis, Dept Chem Engn & Mat Sci, Davis, CA 95616 USA
关键词
D O I
10.1021/jp014484c
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 [物理化学]; 081704 [应用化学];
摘要
The Langmuir layer behavior of arachidic acid/gamma-Fe2O3 nanoparticle complexes was studied at the air/water interface. The subphase was an aqueous colloidal solution (hydrosol) of gamma-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 gamma-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 well-separated 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, Mossbauer spectroscopy and vibrating sample magnetometry (VSM). The gamma-Fe2O3 nanoparticles and Langmuir-Blodgett films with the nanoparticles showed superparamagnetic properties. The stability of the gamma-Fe2O3 nanoparticle hydrosol solution was studied by zeta potential measurements. Positively charged gamma-Fe2O3 nanoparticles in aqueous hydrosol solution at pH 3.5-5 showed excellent long-term colloidal stability.
引用
收藏
页码:9341 / 9346
页数:6
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