Uranium Redox and Deposition Transitions Embedded in Deep‐Time Geochemical Models and Mineral Chemistry Networks

Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox proc...

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Published inGeochemistry, geophysics, geosystems : G3 Vol. 25; no. 2
Main Authors Moore, E. K., Li, J., Zhang, A., Hao, J., Morrison, S. M., Hummer, D. R., Yee, N.
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 01.02.2024
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Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Plain Language Summary Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO2) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings. Key Points Model calculations indicate Earth surface oxidation limited U4+ uraninite formation, in agreement with increased observed U6+ minerals U oxidation increases the diversity of mineral chemical element associations and distribution in the environment The later formation of U6+ minerals compared to S6+ minerals represents differential Earth surface oxidation
AbstractList Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Plain Language Summary Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO2) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings. Key Points Model calculations indicate Earth surface oxidation limited U4+ uraninite formation, in agreement with increased observed U6+ minerals U oxidation increases the diversity of mineral chemical element associations and distribution in the environment The later formation of U6+ minerals compared to S6+ minerals represents differential Earth surface oxidation
Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period.
Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period.
Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U 6+ mineral localities surpasses the number of U 4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U 6+ mineral localities increases earlier in the Phanerozoic than the number of U 4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U 6+ –U 4+ . Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U 4+ uraninite (UO 2 ) formation from weathered granite and basalt. Louvain network community detection shows that U 6+ forms minerals with many more shared elements and redox states than U 4+ . The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEE CV ) values of U 6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEE CV values of U 4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U 6+ minerals compared to S 6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Plain Language Summary Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO 2 ) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings. Key Points Model calculations indicate Earth surface oxidation limited U 4+ uraninite formation, in agreement with increased observed U 6+ minerals U oxidation increases the diversity of mineral chemical element associations and distribution in the environment The later formation of U 6+ minerals compared to S 6+ minerals represents differential Earth surface oxidation
Author Hummer, D. R.
Zhang, A.
Moore, E. K.
Li, J.
Hao, J.
Yee, N.
Morrison, S. M.
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SSID ssj0014558
Score 2.4594584
Snippet Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling....
Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical...
Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical...
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SubjectTerms Anoxia
Anoxic conditions
Anoxic sediments
Basalt
Chemical elements
Chemistry
Coefficient of variation
deep‐time
Distribution
Earth
Earth history
Energy resources
Energy sources
Environmental changes
Environmental conditions
Fossil fuels
geochemical model
Geochemistry
Greenhouse gases
Groundwater
History
mineral
Minerals
Modelling
network
Nuclear energy
Nuclear power plants
Organic matter
Oxic conditions
Oxidation
Oxidoreductions
Oxygenation
Phanerozoic
Power plants
redox
Relative abundance
Trace elements
Uranium
Weathering
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Title Uranium Redox and Deposition Transitions Embedded in Deep‐Time Geochemical Models and Mineral Chemistry Networks
URI https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2023GC011267
https://www.proquest.com/docview/2931618343
https://doaj.org/article/ab07c1357d0c4da586fca7eaf533f152
Volume 25
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