The transformation of aragonite to Mn Ca(1 − )CO3 solid-solutions at 20 °C: An experimental study
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a0 = −1 ± 3 at 20 °C is derived from the experimental stoichiometric solubilities of synthetic Mn-calcite [Ca0.75Mn0.25CO3].
“and a0 = − 1 ± 3 (20 °C) is derived from the experimental stoichiometric solubilities of synthetic Mn-calcite [Ca0.75Mn0.25CO3] [17].”
From Dissolution and solubility of calcite-rhodochrosite solid solutions [(Ca1-xMnx)CO3] at 25 °C (2021) · cites this paper as [17]
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- Authors
- Böttcher, M. E.
- Affiliations
- Carl von Ossietzky Universität Oldenburg (DE)
- Corresponding author
- Böttcher, Michael E.
- ORCID
- Böttcher, Michael E.
- Venue
- Marine Chemistry
- Publisher
- Elsevier BV
- Published
- 1997-05
- Volume
- 57
- Issue
- 1-2
- Pages
- 97-106
- ISSN
- 0304-4203 (ISSN-L)
- OpenAlex
- W2040531695
- Cited by
- 28
- References
- 47
- Citations by year
- 2025: 1 · 2022: 1 · 2021: 2 · 2019: 1 · 2018: 1 · 2015: 1 · 2013: 1 · 2012: 1
- FWCI
- 2.70
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Marine Chemistry (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Keywords
- dissolution-precipitation, manganese enrichment, kutnahorite, reaction kinetics, marine mud
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