A predictive thermodynamic model for element partitioning between plagioclase and melt as a function of pressure, temperature and composition

Ralf Dohmen*, Jon Blundy

*Corresponding author for this work

Research output: Contribution to journalArticle (Academic Journal)peer-review

42 Citations (Scopus)

Abstract

One-atmosphere experiments in the system diopside-albite-anorthite (Di-Ab-An) have been used to explore the controls on plagioclase-melt partitioning of trace elements (Li, K, Rb, Cs, Mg, Zn, Sr, Ba, La, Sm, Y). By performing experiments along isotherms it was possible to isolate compositional controls from those of temperature. The lattice strain model accounts for variations in partition coefficients (Kp(i)) for isovalent series of cations (in+) and the experimental data are used to optimize the lattice strain parameters so that partition coefficients for n = 1 to 3 can be derived from Kp(Na), Kp(Ca), and Kp(La), respectively, at the conditions of interest. The optimized lattice strain parameters have magnitudes and compositional and thermal dependences that are consistent with elastic data for plagioclases. Kp(La) is parameterized via an exchange reaction involving CaAl2Si2O8 and the La-feldspar component. La0.5Na0.5Al2Si2O8. The free energy change of this reaction is small, but well constrained by the data, such that for a given P-T-X Kp(La) can be derived from a combination of Kp(Na) and Kp(Ca). In the case where Kp(Na) and Kp(Ca) are independently constrained, the models reproduce the experimental values of 749 Kps for Li, Mg, K, Rb, Sr, Y, Cs, Ba, and REE (obtained from 91 individual experiments varying over five orders of magnitude) within a factor of 1.5 for 53 percent of the data and a factor of 2 for 74 percent of the data. The isothermal experimental data reveal that additional compositional effects, arising from non-ideal mixing in plagioclase and in melt, also influence Kp(i). A thermodynamic model based on the free energy of fusion of albite (NaAlSi3O8) and anorthite (CaAl2Si2O8), and taking into account plagioclase and melt non-ideality in Di-Ab-An, is developed to express Kp(Na), Kp(Ca) as functions of pressure (P), temperature (T) and composition (X). The thermodynamic models are extended to a wider compositional range by means of an empirical parameterization of 919 Kp(Na) and 920 Kp(Ca) from a database of 991 published experiments. These models are able to reproduce 919 measured partitioning values for Li, Na, Mg, Ca, K, Rb, Sr, Y, Cs, Ba, and REE (from 91 experiments) with 47 percent of the model values within a factor of 1.5 of the measured values and 69 percent within a factor of 2 for any P-T-X condition. The models can also be used to constrain the dependence of the chemical potential of trace cations in plagioclase solid solutions (μi pl) for use in diffusion chronometry where the fully equilibrated trace element concentration profile must be known in order to calculate timescales. It is shown that μi pl is not adequately described by existing empirical models used to predict Kp as a function of anorthite because of the conflating effects of T and X in the polythermal experimental datasets from which those models were derived.

Original languageEnglish
Pages (from-to)1319-1372
Number of pages54
JournalAmerican Journal of Science
Volume314
Issue number9
DOIs
Publication statusPublished - 1 Jan 2014

Keywords

  • Diffusion
  • Experimental petrology
  • Mineral-melt partitioning
  • Plagioclase
  • Thermodynamic modeling

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