DISSOLUTION KINETICS OF MAGNESITE IN ACIDIC AQUEOUS SOLUTION, A HYDROTHERMAL ATOMIC FORCE MICROSCOPY (HAFM) STUDY: STEP ORIENTATION AND KINK DYNAMICS

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dc.contributor.author Jordan G.
dc.contributor.author Higgins S.R.
dc.contributor.author Eggleston C.M.
dc.contributor.author Knauss K.G.
dc.contributor.author Schmahl W.W.
dc.date.accessioned 2021-03-17T00:04:41Z
dc.date.available 2021-03-17T00:04:41Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=830684
dc.identifier.citation Geochimica et Cosmochimica Acta, 2001, 65, 23, 4257-4266
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/26789
dc.description.abstract The dissolution kinetics of features on the magnesite (104) surface were studied in aqueous solutions from pH 4.2 to 2 and at temperatures between 60 and 90°C by hydrothermal atomic force microscopy (HAFM). At pH = 4.2, HAFM images showed magnesite step orientations that are comparable to the step orientations on calcite. Similar to calcite (104), there is anisotropy in the step velocity, but the magnitude of the anisotropy is much greater for magnesite. Furthermore, below pH = 4.2, changes in the dominant step orientation were observed. These results are discussed in terms of a nearest neighbor kink dynamic model, and the associated kink dynamics were tested with kinetic Monte Carlo (KMC) simulations. The KMC results suggest that the kink dynamic model does not account for the experimental observations and that further details such as second-nearest neighbor interactions or surface/edge diffusion cannot be excluded from the model. The dominant step orientations at low pH also point toward mechanisms stabilizing steps along periodic bond chain directions.
dc.title DISSOLUTION KINETICS OF MAGNESITE IN ACIDIC AQUEOUS SOLUTION, A HYDROTHERMAL ATOMIC FORCE MICROSCOPY (HAFM) STUDY: STEP ORIENTATION AND KINK DYNAMICS
dc.type Статья


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