Thermodynamic and Kinetic Studies of Dolomite Formation: A Review
The “dolomite problem”, which has confused scientists for nearly two centuries, is an important fundamental geological problem. The mineralogical characteristics of carbonate minerals show that the dolomite structure consists of an ordered arrangement of alternating layers of Ca<sup>2+</sup...
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MDPI AG
2023-11-01
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| Series: | Minerals |
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| Online Access: | https://www.mdpi.com/2075-163X/13/12/1479 |
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| author | Chao Chen Hanting Zhong Xinyu Wang Meng Ning Xia Wang Yuzhu Ge Han Wang Ruifeng Tang Mingcai Hou |
| author_facet | Chao Chen Hanting Zhong Xinyu Wang Meng Ning Xia Wang Yuzhu Ge Han Wang Ruifeng Tang Mingcai Hou |
| author_sort | Chao Chen |
| collection | DOAJ |
| description | The “dolomite problem”, which has confused scientists for nearly two centuries, is an important fundamental geological problem. The mineralogical characteristics of carbonate minerals show that the dolomite structure consists of an ordered arrangement of alternating layers of Ca<sup>2+</sup> and Mg<sup>2+</sup> cations interspersed with <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msubsup><mrow><mi mathvariant="normal">C</mi><mi mathvariant="normal">O</mi></mrow><mrow><mn>3</mn></mrow><mrow><mn>2</mn><mo>−</mo></mrow></msubsup></mrow></semantics></math></inline-formula> anion layers normal to the c-axis. The dolomite structure violates the c glide plane in the calcite structure, which means that dolomite has R<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mover accent="true"><mrow><mn>3</mn></mrow><mo>¯</mo></mover></mrow></semantics></math></inline-formula> space group symmetry. The ordered dolomite has superlattice XRD reflections [e.g., (101), (015) and (021)], which distinguish it from calcite and high-Mg calcite. The calculation of thermodynamic parameters shows that modern seawater has a thermodynamic tendency of dolomite precipitation and the dolomitization reaction can be carried out in standard state. However, the latest thermodynamic study shows that modern seawater is not conducive to dolomitization, and that seawater is favorable for dolomitization in only a few regions, such as Abu Dhabi, the Mediterranean and the hypersaline lagoons in Brazil. The kinetic factors of dolomite formation mainly consist of the hydration of Mg<sup>2+</sup>, the presence of sulfate and the activity of carbonate. Current studies have shown that the presence of microorganisms, exopolymeric substances (EPS), organic molecules, carboxyl and hydroxyl functional groups associated with microorganisms and organic molecules, clay minerals with negative charges and dissolved silica facilitate magnesium ions to overcome hydration and thus promote Mg<sup>2+</sup> incorporation into growing Ca-Mg carbonates. Similarly, the metabolic activity of microorganisms is conducive to the increase in alkalinity. However, the inhibitory effect of sulfate on dolomite formation seems to be overestimated, and sulfate may even be a catalyst for dolomite formation. Combining the carbonate crystallization mechanism with thermodynamic and kinetic factors suggests that the early stage of dolomite precipitation or the dolomitization reaction may be controlled by kinetics and dominated by unstable intermediate phases, while metastable intermediate phases later transform to ordered dolomite via an Ostwald’s step rule. |
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| publishDate | 2023-11-01 |
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| spelling | doaj.art-6e75eef91f2a4a28bd8786ce822c48d32023-12-22T14:26:29ZengMDPI AGMinerals2075-163X2023-11-011312147910.3390/min13121479Thermodynamic and Kinetic Studies of Dolomite Formation: A ReviewChao Chen0Hanting Zhong1Xinyu Wang2Meng Ning3Xia Wang4Yuzhu Ge5Han Wang6Ruifeng Tang7Mingcai Hou8State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaInstitute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, ChinaState Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, ChinaThe “dolomite problem”, which has confused scientists for nearly two centuries, is an important fundamental geological problem. The mineralogical characteristics of carbonate minerals show that the dolomite structure consists of an ordered arrangement of alternating layers of Ca<sup>2+</sup> and Mg<sup>2+</sup> cations interspersed with <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><msubsup><mrow><mi mathvariant="normal">C</mi><mi mathvariant="normal">O</mi></mrow><mrow><mn>3</mn></mrow><mrow><mn>2</mn><mo>−</mo></mrow></msubsup></mrow></semantics></math></inline-formula> anion layers normal to the c-axis. The dolomite structure violates the c glide plane in the calcite structure, which means that dolomite has R<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mover accent="true"><mrow><mn>3</mn></mrow><mo>¯</mo></mover></mrow></semantics></math></inline-formula> space group symmetry. The ordered dolomite has superlattice XRD reflections [e.g., (101), (015) and (021)], which distinguish it from calcite and high-Mg calcite. The calculation of thermodynamic parameters shows that modern seawater has a thermodynamic tendency of dolomite precipitation and the dolomitization reaction can be carried out in standard state. However, the latest thermodynamic study shows that modern seawater is not conducive to dolomitization, and that seawater is favorable for dolomitization in only a few regions, such as Abu Dhabi, the Mediterranean and the hypersaline lagoons in Brazil. The kinetic factors of dolomite formation mainly consist of the hydration of Mg<sup>2+</sup>, the presence of sulfate and the activity of carbonate. Current studies have shown that the presence of microorganisms, exopolymeric substances (EPS), organic molecules, carboxyl and hydroxyl functional groups associated with microorganisms and organic molecules, clay minerals with negative charges and dissolved silica facilitate magnesium ions to overcome hydration and thus promote Mg<sup>2+</sup> incorporation into growing Ca-Mg carbonates. Similarly, the metabolic activity of microorganisms is conducive to the increase in alkalinity. However, the inhibitory effect of sulfate on dolomite formation seems to be overestimated, and sulfate may even be a catalyst for dolomite formation. Combining the carbonate crystallization mechanism with thermodynamic and kinetic factors suggests that the early stage of dolomite precipitation or the dolomitization reaction may be controlled by kinetics and dominated by unstable intermediate phases, while metastable intermediate phases later transform to ordered dolomite via an Ostwald’s step rule.https://www.mdpi.com/2075-163X/13/12/1479dolomite problemdolomite mineralogythermodynamicskinetics |
| spellingShingle | Chao Chen Hanting Zhong Xinyu Wang Meng Ning Xia Wang Yuzhu Ge Han Wang Ruifeng Tang Mingcai Hou Thermodynamic and Kinetic Studies of Dolomite Formation: A Review Minerals dolomite problem dolomite mineralogy thermodynamics kinetics |
| title | Thermodynamic and Kinetic Studies of Dolomite Formation: A Review |
| title_full | Thermodynamic and Kinetic Studies of Dolomite Formation: A Review |
| title_fullStr | Thermodynamic and Kinetic Studies of Dolomite Formation: A Review |
| title_full_unstemmed | Thermodynamic and Kinetic Studies of Dolomite Formation: A Review |
| title_short | Thermodynamic and Kinetic Studies of Dolomite Formation: A Review |
| title_sort | thermodynamic and kinetic studies of dolomite formation a review |
| topic | dolomite problem dolomite mineralogy thermodynamics kinetics |
| url | https://www.mdpi.com/2075-163X/13/12/1479 |
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