The coprecipitation of manganese(II) with calcite: an experimental study
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Although the ionic radius of Ca2+ is approximately 20% larger than that of Mn2+, Mn can substitute Ca in the calcite lattice.
“Although the ionic radius of Ca2+ is approximately 20% larger than that of Mn2+, Mn can substitute Ca in the calcite lattice [9].”
From Dissolution and solubility of calcite-rhodochrosite solid solutions [(Ca1-xMnx)CO3] at 25 °C (2021) · cites this paper as [9]
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Dissolution and solubility of calcite-rhodochrosite solid solutions [(Ca1-xMnx)CO3] at 25 °C
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Kinetic control of Mn incorporation during CaCO3 precipitation in Ca–carbonate systems
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- Authors
- Pingitore, N. E., Eastman, M. P., Sandidge, M., Oden, K., & Freiha, B.
- Affiliations
- The University of Texas at El Paso (US)
- Venue
- Marine Chemistry
- Publisher
- Elsevier BV
- Published
- 1988-10
- Volume
- 25
- Issue
- 2
- Pages
- 107-120
- ISSN
- 0304-4203 (ISSN-L)
- OpenAlex
- W2141655611
- Cited by
- 129
- References
- 30
- Citations by year
- 2026: 6 · 2025: 2 · 2024: 5 · 2023: 1 · 2022: 6 · 2021: 5 · 2020: 6 · 2019: 5 · 2018: 4 · 2017: 1 · 2016: 2 · 2015: 1 · 2014: 5 · 2013: 1 · 2012: 4
- FWCI
- 6.70
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Marine Chemistry (publishedVersion)
- Funders
- Welch Foundation
- 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 › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- calcite, precipitation rate, electron spin resonance, trace element incorporation
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