Kinetic inhibition of dolomite precipitation: Insights from Raman spectroscopy of Mg2+–SO42− ion pairing in MgSO4/MgCl2/NaCl solutions at temperatures of 25 to 200 °C
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Thermochemical sulfate reduction can remove sulfate to release Mg2+ and generate CO2 (CO3/HCO3), facilitating hydrothermal dolomite formation.
“Thermochemical sulfate reduction (TSR) can remove sulfate to release Mg 2+ and generate CO 2 (CO 2- 3 /HCO - 3 ), which facilitates the formation of hydrothermal dolomite”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [33]
Recent studies indicate that the inhibitory effect of sulfate is not strong at low temperatures.
“However, recent studies indicate that the inhibitory effect of sulfate is not strong at low temperatures [33].”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [33]
Dissolved sulfate inhibits dolomite formation at high temperatures due to strong ion pairing between Mg2+ and SO4, but its inhibitory effect is overestimated at low temperatures.
“they concluded that dissolved sulfate does inhibit the formation of dolomite at high temperatures due to the strong ion pairing between Mg 2+ and SO 2- 4 but is indeed overestimated at low temperatures.”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [33]
At high temperatures, SO4 combines with Mg2+ to form a tight contact ion pair (CIP).
“the experimental results of Wang et al. [33] demonstrate that at high temperatures, SO 2- 4 combines with Mg 2+ to form a tight contact ion pair (CIP).”
From Thermodynamic and Kinetic Studies of Dolomite Formation: A Review (2023) · cites this paper as [33]
Cites
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Concepts and models of dolomitization: a critical reappraisal
Machel, H. G. (2004) · Geological Society, London, Special Publications · doi:10.1144/gsl.sp.2004.235.01.02 · Cited by 787 · see citing works
Microbial mediation as a possible mechanism for natural dolomite formation at low temperatures
Vasconcelos, C., McKenzie, J. A., Bernasconi, S., Grujic, D., & Tiens, A. J. (1995) · Nature · doi:10.1038/377220a0 · Cited by 745 · see citing works
The Isotopic and Trace Element Geochemistry of Dolomite: The State of the Art
Land, L. S. (1980) · Concepts and Models of Dolomitization · doi:10.2110/pec.80.28.0087 · Cited by 664 · see citing works
Dolomitization; a critical view of some current views
Hardie, L. A. (1987) · Journal of Sedimentary Research · doi:10.1306/212f8ad5-2b24-11d7-8648000102c1865d · Cited by 603 · see citing works
Land, L. S. (1998) · Aquatic Geochemistry · doi:10.1023/a:1009688315854 · Cited by 396 · see citing works
Dolomite formation within microbial mats in the coastal sabkha of Abu Dhabi (United Arab Emirates)
BONTOGNALI, T. R. R., VASCONCELOS, C., WARTHMANN, R. J., BERNASCONI, S. M., DUPRAZ, C., STROHMENGER, C. J., & McKENZIE, J. A. (2010) · Sedimentology · doi:10.1111/j.1365-3091.2009.01121.x · Cited by 360 · see citing works
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Dolomite formation and biogeochemical cycles in the Phanerozoic
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MCKENZIE, J. A., & VASCONCELOS, C. (2009) · Sedimentology · doi:10.1111/j.1365-3091.2008.01027.x · Cited by 186 · see citing works
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Thermodynamic and Kinetic Studies of Dolomite Formation: A Review
Chen, C., Zhong, H., Wang, X., Ning, M., Wang, X., Ge, Y., Wang, H., Tang, R., & Hou, M. (2023) · Minerals · doi:10.3390/min13121479 · Cited by 43 · see citing works
Self-citationAn Early Holocene Primary Dolomite Layer of Abiotic Origin in Lake Sayram, Central Asia
Cheng, J., Meng, X., Zhang, E., Jiang, Q., Ni, Z., & Ji, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl096309 · Cited by 20 · see citing works
Systematic laboratory approach to produce Mg-rich carbonates at low-temperature
Al Disi, Z. A., Zouari, N., Attia, E., Al-Asali, M., Al Saad Al-Kuwari, H., Sadooni, F., Dittrich, M., & Bontognali, T. R. R. (2021) · RSC Advances · doi:10.1039/d1ra06206a · Cited by 15 · see citing works
- Authors
- Wang, X., Chou, I.-M., Hu, W., Yuan, S., Liu, H., Wan, Y., & Wang, X.
- Affiliations
- Nanjing University (CN)
- Chinese Academy of Sciences (CN)
- Chinese Academy of Geological Sciences (CN)
- Corresponding author
- Wang, Xiaolin
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2016-10
- Volume
- 435
- Pages
- 10-21
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2344193291
- Cited by
- 25
- References
- 11
- Citations by year
- 2026: 2 · 2025: 2 · 2024: 5 · 2023: 2 · 2022: 2 · 2021: 3 · 2020: 1 · 2019: 2 · 2018: 2 · 2017: 4
- FWCI
- 1.09
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Funders
- National Natural Science Foundation of China (41573054, 41203045, 41230312)
- National Science and Technology Major Project of China (2016ZX05002-006-005)
- Chinese Academy of Sciences (SIDSSE-201302, XDB06060100)
- Topics
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Materials Science › Materials Chemistry › Crystallization and Solubility Studies
- Keywords
- dolomite precipitation, kinetic inhibition, dissolved sulfate, contact ion pairs, hydrothermal dolomite, thermochemical sulfate reduction, bacterial sulfate reduction, sulfate removal, high-temperature aqueous solutions
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