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European Journal of Mineralogy; May/June 2007; v. 19; no. 3; p. 333-338; DOI: 10.1127/0935-1221/2007/0019-1738
© 2007 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Mineral Surface Reativity

Shape of growth hillocks produced by impurity uptake

Marco Rubbo

Università di Torino, Dipartimento di Scienze Mineralogiche e Petrologiche, via Valperga Caluso 35, 10125 Torino, Italy e-mail: marco.rubbo{at}unito.it

Developing classical works, we propose a model to describe the evolution with time, of the profile of a growing hillock whose initial shape is known. The profile is the envelope of the steps originated at a dislocation line, so its evolution is related to the movement of the steps as determined by the surface diffusion followed by the integration of the growth units in the kinks. When impurities poison the kinks the profile is determined also by the kinetics of impurities adsorption. In the model the kinetic processes are described in terms of several parameters. An example of a calculated profile is presented and discussed. It is suggested that simulations performed varying the values of the parameters can help to understand hillocks morphology and to asses the growth mechanism.

Key-words: surface processes limited growth, impurity uptake and surface patterns of minerals.







JOURNAL HOME HELP FEEDBACK/COMMNET SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers