Thermodynamic model for diffusion controlled reaction rim growth in a binary system: Application to the forsterite-enstatite-quartz system

Clicks: 4
ID: 298797
2009
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal
Emerging

Ranked #192 of 8,486 articles by views in american journal of science

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 8,486 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Abstract
We present a thermodynamic model for diffusion controlled growth of a reaction rim of phase γ between the phases α and β in a two component system. We investigate the case, where the reactant phase α has planar, cylindrical and spherical geometry and is embedded in a matrix of phase β. We find that for non planar geometry and for the general case, where the molar volumes of the reactant phases are different, the rim growth rate depends on the matrix-inclusion arrangement. The model is applied to growth of enstatite reaction rims that form at quartz-forsterite interfaces. Two different geometrical setups are considered, namely a spherical grain of forsterite in a quartz matrix and a spherical quartz grain in a forsterite matrix. The enstatite rims are polycrystalline and transfer of the MgO and SiO2 components across the growing rim occurs by a combination of volume− and grain boundary diffusion. For enstatite rims that were grown at experimental conditions of 1000°C and 1 GPa (Milke and others, 2008) bulk mass transfer may be described by effective diffusion coefficients in the range of 1.8 · 10−17m2s−1DSiO2 ≤ 1.1 · 10−16m2s−1 and 2.7 · 10−17m2s−1DMgO ≤ 1.6 · 10−16m2s−1.
Reference Key
openalex_W1979326917 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Rainer Abart, Elena Petrishcheva, F.D. Fischer, Jiřı́ Svoboda
Journal american journal of science
Year 2009
DOI
10.2475/02.2009.02
URL
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.