1. Nuclear Magnetic Resonance Study of Hydrated Bentonite.
- Author
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Donoso, J. P., Tambelli, C. E., Magon, C. J., Mattos, R. I., Silva, I. D. A., Souza, J. E. de, Moreno, M., Benavente, E., and Gonzalez, G.
- Subjects
NUCLEAR magnetic resonance ,BENTONITE ,SPECTRUM analysis ,PROPERTIES of matter ,PROTONS ,SEMICONDUCTOR doping ,ELECTROCHEMICAL analysis ,TEMPERATURE ,IMPEDANCE spectroscopy - Abstract
Impedance spectroscopy and nuclear magnetic resonance (NMR) were used to investigate the mobility of water molecules located in the interlayer space of H+ - exchanged bentonite clay. The conductivity obtained by ac measurements was 1.25 × 10-4 S/cm at 298 K. Proton (1H) lineshapes and spin-lattice relaxation times were measured as a function of temperature over the temperature range 130-320 K. The NMR experiments exhibit the qualitative features associated with the proton motion, namely the presence of a 1H NMR line narrowing and a well-defined spin-lattice relaxation rate maximum. The temperature dependence of the proton spin-lattice relaxation rates was analyzed with the spectral density function appropriate for proton dynamics in a two-dimensional system. The self-diffusion coefficient estimated from our NMR data, D ∼ 2 × 10-7 cm2/s at 300 K, is consistent with those reported for exchanged montmorillonite clay hydrates studied by NMR and quasi-elastic neutron scattering (QNS). [ABSTRACT FROM AUTHOR]
- Published
- 2010
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