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Effect of sample history on dissolution rates of gypsum {010} surfaces

Lennaerts, Dennis Stefan Renier
http://rave.ohiolink.edu/etdc/view?acc_num=wright1366826120

Abstract Details

2013, Master of Science (MS), Wright State University, Chemistry.
Mineral dissolution plays a significant role in geochemical processes such as carbon sequestration and isotope geochemistry. While factors such as temperature, pressure, and solution chemistry have been widely studied, the effects of sample history and surface morphology on dissolution rates have been studied to a lesser extent. This research focuses on the dissolution of cleaved, polished, and reacted samples of the atomically flat natural {010} cleavage plane of gypsum (CaSO4·2H2O) to further investigate upon the effect of sample history. Gypsum was chosen as the mineral of interest because of its planar crystal surface and relatively fast dissolution rate. Chemical dissolution rates as well as changes in surface morphologies were determined for cleaved, polished, and reacted crystals exposed to undersaturated solutions in continuously stirred, free–drift, batch reactors. Results from chemical rate determination showed a history effect as dissolution rate decreased in consecutive dissolution runs for polished samples. For cleaved samples, relatively slow initial dissolution rates were observed. Surface morphology development showed that cleaved samples initially dissolved through etch pit nucleation and growth, while polished samples initially dissolved through step retreat. After dissolution, both cleaved and polished surfaces only showed step bunches along the [001] direction suggesting that both cleaved and polished crystals will eventually have similar surface morphologies and dissolution rates. In conclusion, surface morphology and thus sample preparation affect the initial dissolution rates on the (010) surface of gypsum. Therefore, sample preparation is a variable that should be accounted for in laboratory experiments.
Steven R. Higgins, Ph.D (Advisor)
David A. Grossie, Ph.D (Committee Chair)
Andrew G. Stack, Ph.D (Committee Member)
David A. Dolson, Ph.D (Committee Member)
Ioana E.P. Sizemore, Ph.D (Committee Member)
68 p.
Chemistry; Geochemistry; Geology; Mineralogy
gypsum; mineral dissolution; surface morphology; sample history; atomic force microscopy;

Recommended Citations

Citations

  • Lennaerts, D. S. R. (2013). Effect of sample history on dissolution rates of gypsum {010} surfaces [Master's thesis, Wright State University]. OhioLINK Electronic Theses and Dissertations Center. http://rave.ohiolink.edu/etdc/view?acc_num=wright1366826120

    APA Style (7th edition)

  • Lennaerts, Dennis. Effect of sample history on dissolution rates of gypsum {010} surfaces. 2013. Wright State University, Master's thesis. OhioLINK Electronic Theses and Dissertations Center, http://rave.ohiolink.edu/etdc/view?acc_num=wright1366826120.

    MLA Style (8th edition)

  • Lennaerts, Dennis. "Effect of sample history on dissolution rates of gypsum {010} surfaces." Master's thesis, Wright State University, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=wright1366826120

    Chicago Manual of Style (17th edition)

wright1366826120
502
© 2013, all rights reserved.
This open access ETD is published by Wright State University and OhioLINK.