Abstract
This study examines the systematics and rate of alkali transport in haplogranite diffusion couples in which a chemical potential gradient in Al is established between near water-saturated metaluminous and peraluminous liquids that differ only in their initial content of normative corundum. At 800°C, measurable chemical diffusion of alkalis occurs throughout the entire length (∼1 cm) of the diffusion couples in 2–6 h, indicating long range diffusive communication through melt. Alkali transport results in homogenization of initially different Na/Al and ASI [=mol. Al2O3/(CaO + Na2O + K2O)] throughout the couples within ∼24 h, whereas initially homogenous K* evolves to become uniformly different between metaluminous and peraluminous ends. Calculated effective binary diffusion coefficients for alkalis in experiments that do not significantly violate the requirement of a semi-infinite chemical reservoir (0- to 2-h duration at 800°C) are similar to those observed in previous studies: in the range of (1–8) × 10−12 m2/s. Such a magnitude of diffusivity, however, is inadequate to account for the observed changes of alkali concentrations and molecular ratios throughout the couples in 2- to 6-h experiments. The latter changes are consistent with diffusivities estimated via the x 2 = Dt approximation, which yields effective values around 10−9 m2/s. These observations suggest that Fick’s law alone does not adequately describe the diffusive transport of alkalis in granitic liquids. In addition to simple ionic diffusion associated with local gradients in concentration or chemical potential of the diffusing component described by Fick’s second law (local diffusion), alkali transport through melt involves system-wide diffusion (field diffusion) driven by chemical potential gradients that also include components with which the alkalis couple or complex (e.g., Al). Field diffusion involves the coordinated migration of essentially all alkali cations, resembling a positive ionic current that drives the system to a metastable state having a minimum energy configuration with respect to alkali distribution. The net result is effective transport rates perhaps three orders of magnitude faster than simple local alkali diffusion, and at least seven to eight orders of magnitude faster than the diffusive equilibration of Al and Si.
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Acosta-Vigil A, London D, Dewers TA, Morgan GB VI (2002) Dissolution of corundum and andalusite in H2O-saturated haplogranitic melts at 800°C and 200 MPa: constraints on diffusivities and the generation of peraluminous melts. J Petrol 43:1885–1908
Acosta-Vigil A, London D, Morgan GB VI, Dewers TA (2003) Solubility of excess alumina in hydrous granitic melts in equilibrium with peraluminous minerals at 700–800°C and 200 MPa, and applications of the aluminum saturation index. Contrib Mineral Petrol 146:100–119
Acosta-Vigil A, London D, Morgan GB VI (2005) Contrasting interactions of sodium and potassium with H2O in haplogranitic liquids and glasses at 200 MPa from hydration-diffusion experiments. Contrib Mineral Petrol 149:276–287
Acosta-Vigil A, London D, Dewers TA, Morgan GB VI (2006a) Dissolution quartz, albite, and orthoclase in H2O-saturated haplogranitic melt at 800°C and 200 MPa: diffusive transport properties of granitic melts at crustal anatectic conditions. J Petrol 47:231–254
Acosta-Vigil A, London D, Morgan GB VI (2006b) Experiments on the kinetics of partial meeting of a leucogranite at 200 MPa and 690–800°C: compositional variability of melts during the onset of H2O-saturated crustal anatexis. Contrib Mineral Petrol 151:539–557
Anovitz LM, Blencoe W (1997) Experimental determination of the composition of aqueous fluids coexisting with silicate melts. Geol Soc Am Abstr Prog 29:A-394
Baker DR (1990) Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambers. Contrib Mineral Petrol 104:407–423
Baker DR (1991) Interdiffusion of hydrous dacitic and rhyolitic melts and the efficacy of rhyolite contamination of dacitic enclaves. Contrib Mineral Petrol 106:462–473
Baker DR (1992) Estimation of diffusion coefficients during interdiffusion of geologic melts: application of transition state theory. Chem Geol 98:11–21
Cerny P (1982) The Tanco pegmatite at Bernic Lake, Manitoba, vol 8. Mineralogical Association of Canada Short Course Handbook, pp 527–543
Chakraborty S (1995) Diffusion in silicate melts. In: Stebbins JF, McMillan PF, Dingwell DB (eds) Structure, dynamics, and properties of silicate melts. Reviews in mineralogy, vol 32. Mineralogical Society of America, Washington, pp 409–503
Cooper AR Jr (1968) The use and limitations of the concept of an effective binary diffusion coefficient for multi-component diffusion. In: Wachtman JB Jr, Franklin AD (eds) Mass Transport in Oxides, vol 196. Nat Bur Stand Spee Pub, pp 79–84
Crank J (1964) The mathematics of diffusion. Oxford University Press, Oxford, p 347
Dingwell DB (1990) Effects of structural relaxation on cationic tracer diffusion in silicate melts. Chem Geol 82:209–216
Dingwell DB (2006) Transport properties of magmas: diffusion and rheology. Elements 2:281–286
Freda C, Baker DR (1998) Na–K interdiffusion in alkali feldspar melts. Geochim Cosmochim Acta 62:2997–3007
Harrison TM, Watson EB (1983) Kinetics of zircon dissolution and zirconium diffusion in granitic melts of variable water content. Contrib Mineral Petrol 84:66–72
Henderson P, Nolan J, Cunningham GC, Lowry RK (1985) Structural controls of diffusion in natural silicate melts. Contrib Mineral Petrol 89:263–272
Hutchinson RW (1959) Geology of the Montgary pegmatite. Econ Geol 54:1525–1542
Jahns RH, Tuttle FO (1963) Layered pegmatite-aplite intrusives. Mineral Soc Am Spec Pap 1:78–92
Jambon A (1982) Tracer diffusion in granitic melts: experimental results for Na, K, Rb, Cs, Ca, Sr, Ba, Ce, Eu to 1300°C and a model of calculation. J Geophys Res 87:10797–10810
Jambon A, Carron J-P (1976) Diffusion of Na, K, Rb, and Cs in glasses of albite and orthoclase composition. Geochim Cosmochim Acta 40:897–903
Lagache M, Weisbrod A (1977) The system: two feldspars-KCl-NaCl-H2O at moderate to high temperature and low pressures. Contrib Mineral Petrol 62:77–101
London D (1992) The application of experimental petrology to the genesis and crystallization of granitic pegmatites. Can Mineral 30:499–540
London D (1996) Granitic pegmatites. Trans R Soc Edinb Earth Sci 87:305–319
London D (2005) Geochemistry of alkalis and alkaline earths in ore-forming granites, pegmatites, and rhyolites. In: Linnen R, Sampson I (eds) Rare-element geochemistry of ore deposits, vol 17. Geological Association of Canada Short Course Handbook, pp 17–43
London D, Morgan GB VI, Acosta-Vigil A (2004) Alkali fractionation and feldspar zonation in granitic pegmatites. Geol Soc Am Abstr Prog 36:46
Lowry RK, Henderson P, Nolan J (1982) Tracer diffusion of some alkali, alkaline earth, and transition element ions in a basaltic and an andesitic melt, and the implications concerning melt structure. Contrib Mineral Petrol 809:254–261
Magaritz M, Hofmann AW (1978) Diffusion of Sr, Ba, and Na in obsidian. Geochim Cosmochim Acta 42:595–605
Morgan GB VI, London D (1996) Optimizing the electron microprobe analysis of hydrous alkali aluminosilicate glasses. Am Mineral 81:1176–1185
Morgan GB VI, London D (1999) Crystallization of the Little Three layered pegmatite-aplite dike, Ramona District, California. Contrib Mineral Petrol 136:310–330
Morgan GB VI, London D (2005a) The effect of current density on the electron microprobe analysis of alkali aluminosilicate glasses. Am Mineral 90:1131–1138
Morgan GB VI, London D (2005b) Phosphorus distribution between potassic alkali feldspar and metaluminous haplogranite liquid at 200 MPa (H2O): the effect of undercooling on crystal-liquid systematics. Contrib Mineral Petrol 150:456–471
Mungall JE, Romano C, Dingwell DB (1998) Multicomponent diffusion in the molten system K2O-Na2O-Al2O3-SiO2-H2O. Am Mineral 83:685–699
Pouchon JL, Pichoir F (1985) PAP ϕ (ρz) correction procedure for improved quantitative analysis. In: Armstrong (ed) Microbeam Analysis. San Francisco, pp 104–106
Sippel RF (1963) Sodium self diffusion in natural minerals. Geochim Cosmochim Acta 27:107–120
Smith HD (1974) An experimental study of the diffusion of Na, K, and Rb in magmatic silicate liquids. Ph.D. dissertation, University of Oregon
Tuttle OF, Bowen NL (1958) Origin of granite in light of experimental studies in the system NaAlSi3O8-KAlSi3O8-SiO2-H2O. Geol Soc Am Mem 74:153
van der Laan S, Wyllie PJ (1993) Experimental interaction of granitic and basaltic magmas and implications for mafic enclaves. J Petrol 34:491–517
Watson EB (1981) Diffusion in magmas at depth in the earth: the effects of pressure and dissolved H2O. Earth Planet Sci Lett 52:291–301
Watson EB (1982) Basalt contamination by continental crust: some experiments and models. Contrib Mineral Petrol 80:73–87
Watson EB, Jurewicz SR (1984) Behavior of alkalies during diffusive interaction of granitic xenoliths with basaltic magma. J Geol 92:121–131
Acknowledgments
We wish to thank Don Baker and Bruce Watson, whose reviews of the first draft of this manuscript were tremendously helpful for re-evaluating the diffusion modeling. We note that it was this re-evaluation that eventually led us to propose the mechanism of field diffusion of alkalis (which the reveiwers did not see). Support for this research was provided by National Science Foundation grants EAR-9603199, EAR-9618867, EAR-9625517, and EAR-9404658, and to A.A.-V. by a Ramón y Cajal research contract and project CTM2005-08071-C03-01 from the Ministerio de Educación y Ciencia, Spain.
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Communicated by T.L. Grove.
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Morgan, G.B., Acosta-Vigil, A. & London, D. Diffusive equilibration between hydrous metaluminous-peraluminous haplogranite liquid couples at 200 MPa (H2O) and alkali transport in granitic liquids. Contrib Mineral Petrol 155, 257–269 (2008). https://doi.org/10.1007/s00410-007-0242-4
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DOI: https://doi.org/10.1007/s00410-007-0242-4