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Gypsum Overgrowths Passivate Calcite to Acid Attack

Abstract:
The dissolution of calcite (CaCO3) in aqueous solution at pH below ca. 5-6 is known to proceed via the direct reaction of protons at the solid surface. However, exposure of the mineral to sulfuric acid is shown to lead to the rapid formation of an overlayer of calcium sulfate (gypsum) which completely passivates the surface against further reaction and dissolution. The overlayer is nucleated instantaneously on CaCO3 surfaces. Scanning electron and atomic force microscopy show that strongly adherent overgrowths are encouraged by a lattice matching between the cleavage (211) plane of calcite and the (010) plane of CaSO4andmiddot;2H2O.
Publication status:
Published

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Publisher copy:
10.1006/jcis.1997.4978

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Chemistry
Sub department:
Physical & Theoretical Chem
Role:
Author


Journal:
Journal of colloid and interface science More from this journal
Volume:
192
Issue:
1
Pages:
207-214
Publication date:
1997-08-01
DOI:
EISSN:
1095-7103
ISSN:
0021-9797


Language:
English
Keywords:
UUID:
uuid:331c418e-e930-48d1-9c87-32eac1006538
Local pid:
pubs:36082
Source identifiers:
36082
Deposit date:
2012-12-19

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