1982
DOI: 10.1063/1.555665
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Molten Salts Data: Diffusion Coefficients in Single and Multi-Component Salt Systems

Abstract: The property of diffusion is one of the basic properties of fluid systems. In molten salts, more than 700 studies have been reported to August, 1980, with more than 15 diffusion measurement techniques. A critical examination of these studies with a review of the techniques is presented. The results for more than 140 salt systems are reported in this communication as a series of data tables, with numerical values, value judgements, and literature citations. Silicates, slags, and oxide melts are excluded.

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Cited by 122 publications
(91 citation statements)
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“…Janz also worked in cumulative results for the salts properties between 1972 and 1983 (the Molten Salts Standards Program) [50][51][52][53][54][55][56]. This general database, subsequently reprinted and summarized in 1988 [57], is widely used today for any purpose due to its updated recommendations and reexamined best values for making density and viscosity predictions [58].…”
Section: Introductionmentioning
confidence: 99%
“…Janz also worked in cumulative results for the salts properties between 1972 and 1983 (the Molten Salts Standards Program) [50][51][52][53][54][55][56]. This general database, subsequently reprinted and summarized in 1988 [57], is widely used today for any purpose due to its updated recommendations and reexamined best values for making density and viscosity predictions [58].…”
Section: Introductionmentioning
confidence: 99%
“…The dynamics for molten Flibe salt is complicated; self-diffusion coefficient data from different references are inconsistent with each other [14][15][16][17][18][19]. In general, those data have the same trend: lithium has the strongest diffusivity and beryllium is the hardest to migrate; each of them has positive correlation with temperature.…”
Section: Dynamics Of Liquid Flibementioning
confidence: 85%
“…These observations are consistent with the fact that sodium, nitrate, and chlorine were detected frequently in the deepest ice by Raman (Figure ) and SEM/EDS (Figure ) measurements. This ion‐reduction timing as a function of ion species cannot be explained by differences in ion diffusivity in liquid water (self‐diffusion coefficient, D ), namely in possible liquid veins: D Cl > D Na > D NO3 > D SO4 > D Ca ≈ D Mg [ Janz and Bansal , ; Mills and Lobo , ]. We infer that differences in the location and chemical form are more important: possibly, SO 4 , MSA, and Mg were located preferentially at ice grain boundaries rather than at hydrate surfaces as compared with other chemical components, resulting in the observed antecedent ion depression.…”
Section: Discussionmentioning
confidence: 99%