Calcium carbonate formation and dissolution.

By J. Morse, R. Arvidson, A. Lüttge. Chemical Reviews, 2007

1,156 citations recorded by the source corpus.

Subfields: Biomaterials, Environmental Chemistry, Paleontology

View Paper: https://www.semanticscholar.org/paper/b70b31b2957ae4c7f39e06ba9e00b816d0d6a114

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In Biomaterials

1. J. Provis
2. S. A. Bernal
3. C. Langdon
4. R. Myers

In Environmental Chemistry

1. R. Myers
2. S. A. Bernal
3. J. Provis

Citations in the corpus

• Bioerosion: the other ocean acidification problem: Towards a Broader Perspective on Ocean Acidification Research Part 2 A special issue of the ICES Journal of Marine Science (2017, background): “Abiogenic chemical erosion is the thermodynamically driven, passive dissolution of carbonates through acidity or undersaturation (X< 1; e.g. Pytkowics, 1969; Trudgill, 1976a; Morse et al., 2007; Andersson and Gledhill, 2013; see also Table 1, Supplementary data S1).”
• Phase diagrams for alkali-activated slag binders (2017, background): “polymorphs may also form in NC-activated slag binders, which is experimentally observed [16,17,52]: the thermodynamic stabilities of these phases are similar ([11]), and their precipitation tends to be controlled by kinetics and by the nature of minor dissolved species [53].”
• Calcite growth kinetics: Modeling the effect of solution stoichiometry (2012, background): “The effects of physico-chemical parameters, including temperature, pressure, pH, ionic strength, degree of supersaturation and the presence of inhibitors, on the precipitation of calcite have been studied extensively (see for example the review by Morse et al., 2007).”
• A developmental and energetic basis linking larval oyster shell formation to acidification sensitivity (2013, background): “It is important to note that in this formulation, precipitation rates would be better described as per surface area (rather than mass) [Morse et al., 2007], however, surface area estimates of calcification surfaces are lacking.”
• Oyster Shell Dissolution Rates in Estuarine Waters: Effects of pH and Shell Legacy (2011, background): “In addition, the pitting associated with fouling organisms changes the surface topography of shell material at small spatial scales (millimeters to centimeters), creating additional surface area where thermodynamic dissolution is thereby accelerated (Morse et al. 2007).”