1996
DOI: 10.1016/0169-7722(95)00081-x
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Diffusive transport through compacted Na- and Ca-bentonite

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Cited by 62 publications
(27 citation statements)
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“…This change in HTO diffusivity agrees with the experimental results described in a previous paper by Choi and Oscarson (1996), in which a higher apparent diffusivity of HTO in Ca-bentonite than in Na-bentonite was reported. They also reported that a greater proportion of large pores in Ca-bentonite than in Na-bentonite was determined by Hg intrusion porosimetry, and concluded that higher diffusivity of HTO in Ca-bentonite can be attributed to the different microstructure of the compared bentonite.…”
Section: Resultssupporting
confidence: 92%
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“…This change in HTO diffusivity agrees with the experimental results described in a previous paper by Choi and Oscarson (1996), in which a higher apparent diffusivity of HTO in Ca-bentonite than in Na-bentonite was reported. They also reported that a greater proportion of large pores in Ca-bentonite than in Na-bentonite was determined by Hg intrusion porosimetry, and concluded that higher diffusivity of HTO in Ca-bentonite can be attributed to the different microstructure of the compared bentonite.…”
Section: Resultssupporting
confidence: 92%
“…Thus, the smaller specific surface area measured by the BET method for Ca-montmorillonite suggests a larger aggregate size in the Ca-montmorillonite than in the Na-montmorillonite. Since there is no difference in the basal spacing between Na-and Ca-montmorillonite, the difference of the aggregate size can be attributed to the number of unit layers making up the montmorillonite aggregate, as pointed out by Choi and Oscarson (1996). That implies that the change in the apparent diffusion coefficient of HTO could be caused by the structural changes in the pore spaces rather than in the interlayer spaces where the basal spacing was found to remain constant.…”
Section: Resultsmentioning
confidence: 93%
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“…The unknown G // -value, considered to vary with 74 bentonite dry bulk density, is routinely estimated by fitting a diffusion model to experimental 75 data on the diffusion of water tracers in bentonite in the x // direction (5,14,(19)(20)(21)(22) …”
Section: Introductionmentioning
confidence: 99%
“…with regard to cationic, anionic and neutral species, in a given system). ) (Muurinen et al, 1986;Sato et al, 1992;Kozaki et al, 1996Kozaki et al, , 1998aChoi and Oscarson, 1996;Kozaki et al, 1999a;b, 2001, 2008Lee et al, 1996;Nakajima et al, 1997;Nakashima, 2000Nakashima, , 2002Nakashima, , 2003Nakashima, , 2006Molera, 2002;Molera and Eriksen, 2002;Molera et al, 2003;Sato and Suzuki, 2003;Van Loon et al, 2003a;b, 2004a;b, 2005a;b, 2007;Wang, 2003;Jansson and Eriksen, 2004;García-Gutiérrez et al, 2004;Sato and Miyamoto, 2004;Suzuki et al, 2004;García-Gutiérrez et al, 2009;Wang and Liu, 2004;Wang and Tao, 2004;Melkior et al, 2005Melkior et al, , 2007Melkior et al, , 2009Nakashima and Mitsumori, 2005;Wang et al, 2005;Appelo and Wersin, 2007;Glaus et al, 2011Glaus et al, , 2013Motellier et al, 2007;Glaus et al, 2007Glaus et al, , 2008Glaus et al, , 2010…”
Section: Introduction and Research Motivationmentioning
confidence: 99%