Effects of clay fraction and temperature on the H2O self-diffusivity in hectorite gel: A pulsed-field-gradient spinecho nuclear magnetic resonance study

Clays and Clay Minerals

Volumn 48, Issue 6, 2000, Pages 603-609

  Nakashima, Yoshito ^a  

^a GEOLOGICAL SURVEY OF JAPAN   (Japan)

Author keywords

Complexity of Pore Structure; H2O; Hectorite; NMR; Self Diffusion

Indexed keywords

ACTIVATION ENERGY; DIFFUSION; MOLECULAR STRUCTURE; NUCLEAR MAGNETIC RESONANCE SPECTROSCOPY; POROSITY; THERMAL EFFECTS; WATER;

COMPLEXITY OF PORE STRUCTURE; HECTORITE GEL; SELF DIFFUSION;

CLAY MINERALS;

CLAY MINERAL; CONTAINMENT BARRIER; DIFFUSIVITY; HECTORITE; NUCLEAR MAGNETIC RESONANCE; RADIOACTIVE WASTE; WASTE DISPOSAL; WATER;

EID: 0034352258     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2000.0480602     Document Type: Article

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