Abstract
The method of Koiwa and Ishioka (Philos Mag A 47:927–938, 1983) is used, with slight modification, to evaluate the correlation factor for vacancy-mediated diffusion of impurity atoms on the sublattice of dodecahedral sites in garnet, as a function of the relevant vacancy-jump frequencies. The required values of the lattice Green’s function were obtained from multiple Monte Carlo simulations in lattices of progressively larger size, extrapolated to an infinite lattice using a model that linearizes the dependence of the functional value on lattice size. As Online Resources, codes are provided that permit evaluation of the correlation factor for any chosen set of vacancy-jump frequencies, for implementation in either Mathematica ® or Matlab ®.
Similar content being viewed by others
Notes
Lattice sites are identified by vector components in the x, y, and z directions; unit vectors in those directions are oriented parallel to crystallographic axes a 1, a 2, and a 3 in garnet, with magnitudes equal to 1/8 of the garnet unit-cell dimension.
In the course of our study, we replicated the calculations of K&I83 that produced their g matrices for the bcc, fcc, and dmd lattices. Doing so revealed four typographical errors, as follows. (1) In their Table 1, for element g 33, "(200)" should instead read "(220)". (2) In their Table 3, for element g 44, “(442)” should instead read "(422)". (3) In their Table 4, for element g 31, "g 13" should instead read “2g 13”. (4) In their Table 4, for element g 14, "(200)" should instead read "(220)". We verified that all further calculations used the correct lattice Green's function, so these errors are purely typographical and did not propagate into their final expressions for the correlation factors.
References
Allnatt AR, Lidiard AB (1993) Atomic transport in solids. Cambridge University Press, Cambridge
Bloch E, Ganguly J, Hervig R, Cheng W (2015) 176Lu–176Hf geochronology of garnet I: experimental determination of the diffusion kinetics of Lu3+ and Hf4+ in garnet, closure temperatures and geochronological implications. Contrib Mineral Petr 169:12
Cahalan RC, Kelly ED, Carlson WD (2014) Rates of Li diffusion in garnet: coupled transport of Li and Y+REEs. Am Mineral 99:1676–1682
Carlson WD (2006) Rates of Fe, Mg, Mn and Ca diffusion in garnet. Am Mineral 91:1–11
Carlson WD (2012) Rates and mechanism of Y, REE, and Cr diffusion in garnet. Am Mineral 97:1598–1618
Chu X, Ague JJ (2015) Analysis of experimental data on divalent cation diffusion kinetics in aluminosilicate garnets with application to timescales of peak Barrovian metamorphism, Scotland. Contrib Mineral Petr 170:25
Crispin KL, Saha S, Morgan D, Van Orman JA (2012) Diffusion of transition metals in periclase by experiment and first-principles, with implications for core-mantle equilibration during metal percolation. Earth Planet Sci Lett 357–358:42–53
Ganguly J (2010) Cation diffusion kinetics in aluminosilicate garnets and geological applications. Rev Mineral Geochem 72:559–601
Hughes BD (1995) Random walks and random environments, volume 1: random walks. Clarendon Press, Oxford
Koiwa M, Ishioka S (1983) Integral methods in the calculation of correlation factors for impurity diffusion. Philos Mag A 47:927–938
Lidiard AB (1955) Impurity diffusion in crystals (mainly ionic crystals with the sodium chloride structure). Philos Mag 46:1218–1237
Manning JE (1964) Correlation factors for impurity diffusion. bcc, diamond, and fcc structures. Phys Rev A 136:1758–1766
Mehrer H (2007) Diffusion in solids: fundamentals, methods, materials, diffusion-controlled processes. Springer, Berlin
Tirone M, Ganguly J, Dohmen R, Langenhorst F, Hervig R, Becker H-W (2005) Rare earth diffusion kinetics in garnet: experimental studies and applications. Geochim Cosmochim Acta 69:2385–2398
Van Orman JA, Krawczynski MJ (2015) Theoretical constraints on the isotope effect for diffusion in minerals. Geochim Cosmochim Acta 164:365–381
Zhang Y, Cherniak DJ (2010) Diffusion in minerals and melts. Reviews in mineralogy and geochemistry, vol 72. Mineralogical Society of America, Geochemical Society, Chantilly
Acknowledgments
The support of the Geology Foundation of the University of Texas at Austin is gratefully acknowledged.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary materials
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Carlson, W.D., Wilson, C.R. Correlation factors for impurity diffusion on the sublattice of dodecahedral sites in garnet. Phys Chem Minerals 43, 363–369 (2016). https://doi.org/10.1007/s00269-016-0800-2
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00269-016-0800-2