Issue 2, 1986

Water spin relaxation in colloidal systems. Part 1.—17O and 2H relaxation in dispersions of colloidal silica

Abstract

Extensive water 17O and 2H spin-relaxation data from alkali-stabilized aqueous dispersions of spherical colloidal silica particles are presented. Longitudinal (R1) and transverse (R2) relaxation rates of both nuclei have been measured in samples of varying particle diameter (ca. 10–80 nm) as functions of resonance frequency, temperature, alkali content and particle concentration. Qualitative and quantitative differences in the results from the two nuclei demonstrate that surface silanol groups, exchanging deuterons very rapidly with bulk water, contribute to R1(2H) and dominate R2(2H). At the highest measured resonance frequencies, the enhancement of R1 relative to bulk water is entirely due to rapid, local dynamics of water molecules (and, for 2H, silanol groups), whereas R2 contains additional contributions from slow diffusive processes. The fast and slow dynamics are independent of particle concentration. The R1 relaxation enhancement depends only on the ratio of silica surface area to water volume, independent of particle size, indicating that the structure of the particle surface is size invariant. In contrast, the slow dynamics contributing to R2 has a systematic dependence on particle size.

Article information

Article type
Paper

J. Chem. Soc., Faraday Trans. 1, 1986,82, 387-399

Water spin relaxation in colloidal systems. Part 1.—17O and 2H relaxation in dispersions of colloidal silica

L. Piculell, J. Chem. Soc., Faraday Trans. 1, 1986, 82, 387 DOI: 10.1039/F19868200387

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