Abstract

A detailed description of the structure of the amphibole-supergroup minerals is very challenging owing to their complex chemical composition that renders the process of cation partition extremely difficult, particularly because of the occurrence of multivalent elements. Since amphiboles naturally occur under a fibrous morphology and have largely been used to produce asbestos, there is a growing demand for detailed and accurate structural data in order to study the relationships between structure, composition and toxicity. The present study proposes a recommended refinement procedure for both X-ray single-crystal structure refinement (SREF) and Rietveld analysis for tremolite, selected as a test case. The corresponding structural results are compared to estimate the `degree of confidence' of the Rietveld refinement with regard to SREF. In particular, it is shown that the interpretation of the electron density of the tremolite structure by SREF is model dependent. By assuming that the site-scattering values from SREF should be as close as possible to those from electron microprobe analysis, as a crucial constraint for the correct description of the final crystal-chemical model, it is found that it is best satisfied by using partially ionized scattering curves (SCs) for O and Si, and neutral SCs (neutral oxygen curves or NOCs) for other atoms. This combination leads to the best fit to the diffraction data. Moreover, it is found that Rietveld refinement using NOCs produces the best structural results, in excellent agreement with SREF. It is worth noting that, due to the complexity of the diffraction pattern and the fairly large number of freely refinable parameters, refinements with different combinations of SCs produce results almost indistinguishable from a statistical point of view, albeit showing significant differences from a structural point of view.

Highlights

  • Amphiboles are among the most thoroughly investigated minerals from a structural and crystal-chemical viewpoint

  • We have shown that the interpretation of the electron density of the tremolite structure is modeldependent

  • As a valid constraint for the correct description of the model, we assumed that site scattering (SS) values from structure refinement (SREF) should be as close as possible to those from electron microprobe analysis (EMPA)

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Summary

Introduction

Amphiboles are among the most thoroughly investigated minerals from a structural and crystal-chemical viewpoint. This is due to the fact that their use implies a different number of electrons at = 0 affecting the correlation between displacement parameters and scale factor (Coppens, 1997). The use of different combinations of SCs has been commonly used to compensate empirically for perturbation of the electron density caused by interaction with other atoms in cases where more refined approaches are not applicable (Coppens, 1997) This is promoted by the fact that the scattering of the atomic valence electrons is concentrated in the low-order region of reciprocal space, i.e. in the diffraction zone sin / < 0.25 A À1, where neutral and ionized SCs differ more significantly

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