| 2004 Denver Annual Meeting (November 7–10, 2004) | |
| Paper No. 141-9 | |
| Presentation Time: 10:25 AM-10:40 AM | ||
STEP VELOCITIES AND RATES OF DISSOLUTION AT DIFFERENT SATURATION INDICES AND VARYING IONIC RATIOS STUDIED DURING DISSOLUTION OF CELESTITE (SRSO4) | ||
|
BOSE, Sweta1, HU, X.2, and HIGGINS, S.R2, (1) Department of Chemistry (Environmental Sciences PhD Program), Wright State Univ, 3640 Colonel Glenn Hwy, Dayton, OH 45435, bose.2@wright.edu, (2) Department of Chemistry, Wright State Univ, 3640 Colonel Glenn Hwy, Dayton, OH 45435 Dissolution kinetics of Celestite was studied using AFM (atomic force microscopy). Experiments were carried out on freshly cleaved 001 surfaces of the SrSO4 crystal at room temperature and at a pH of 5.0. In-situ AFM experiments were designed in a fluid cell system, which aided the understanding of the dissolution behavior under flow through conditions. On the basis of movement of microscopic surface structures (e.g. steps), step velocities and rates of dissolution were calculated as functions of different saturation indices of the solution flowing into the system. Similarly, rates were also calculated under conditions of varying ionic ratios (of the participating Sr2+ and SO42- ions) at a fixed saturation index. Step velocities and dissolution rates follow the trend of increasing order of magnitude with decreasing saturation indices. On the other hand, varying ionic ratios revealed an interesting effect on the anisotropic step kinetics suggesting varying roles of the two ions on varying step structures. Experiments also show etch pit morphologies and step distribution at different conditions.
| ||
|
2004 Denver Annual Meeting (November 7–10, 2004)
General Information for this Meeting | ||
| Session No. 141 Looking Forward to the Past: A Session in Honor of Paul Ribbe and the Reviews in Mineralogy and Geochemistry II Colorado Convention Center: 708/710/712 8:00 AM-12:00 PM, Tuesday, November 9, 2004 Geological Society of America Abstracts with Programs, Vol. 36, No. 5, p. 338 | ||
© Copyright 2004 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions. | ||