skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Measuring the multicomponent diffusion matrix: Experimental design and data analysis for silicate melts

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
;  [1]
  1. Univ. of California, Santa Barbara, CA (United States)

The extended form of Fick's Law, which allows the diffusive flux of a chemical species to be a function of all the concentration gradients, provides an accurate and useful description of chemical diffusion in isothermal, multicomponent systems. For an (N + 1)-component system, N[sup 2] diffusion coefficients are required, however. Although recent attempts to measure the multicomponent diffusion matrix for natural silicate compositions and simpler analogs have been unsuccessful, this does not mean that the extended Fick's Law is inapplicable. The authors show that the diffusion matrix cannot be measured unless the experiment is carefully designed. The optimal experiment is a set of 2N isothermal interdiffusion runs using at least N distinct diffusion couples. The concept of orthogonal couples, i.e., mutually perpendicular composition directions, provides a practical guide for choosing distinct couples. The number of couples required depends on the size of the errors in the concentration measurements. Chi-square fitting is an appropriate technique for analyzing diffusion data, because it allows one to directly apply thermodynamic constraints on the eigenvalues of the diffusion matrix. They discuss the details of implementing chi-square fitting for isothermal interdiffusion experiments, including Jacobian and Hessian matrices for both the finite and infinite diffusion couple models. They also apply this method to data from the literature, extracting the diffusion matrix for a Na[sub 2]O-CaO-SiO[sub 2] composition and making preliminary observations about some dacite-rhyolite and CaMgSi[sub 2]O[sub 6]-CaAl[sub 2]Si[sub 2]O[sub 8] experiments.

DOE Contract Number:
FG03-91ER14211
OSTI ID:
6766542
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Vol. 58:18; ISSN 0016-7037
Country of Publication:
United States
Language:
English

Similar Records

Tracer diffusion of network formers and multicomponent diffusion in dacitic and rhyolitic melts
Journal Article · Sat Feb 01 00:00:00 EST 1992 · Geochimica et Cosmochimica Acta; (United States) · OSTI ID:6766542

Theoretical investigation of multicomponent volatile organic vapor diffusion: Steady-state fluxes
Journal Article · Fri Oct 01 00:00:00 EDT 1993 · Journal of Environmental Quality · OSTI ID:6766542

Influence of liquid structure on diffusive isotope separation in molten silicates and aqueous solutions
Journal Article · Tue Mar 01 00:00:00 EST 2011 · Geochimica et Cosmochimica Acta · OSTI ID:6766542