Abstract
Dissolution of the BaSO4(001) surface was studied for the first time by hydrothermal atomic force microscopy. Step velocities and pit nucleation rates as a function of temperature along with observations of surface morphology led to the conclusion that the dissolution process is most accurately described by a two-dimensional birth-and-spread model.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 550 Earth sciences and geology |
Language: | English |
Item ID: | 18673 |
Date Deposited: | 10. Mar 2014, 14:12 |
Last Modified: | 29. Apr 2016, 09:15 |