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DOI | 10.1126/science.abb8092 |
Deep abiotic weathering of pyrite | |
Gu X.; Heaney P.J.; Reis F.D.A.A.; Brantley S.L. | |
发表日期 | 2020 |
ISSN | 0036-8075 |
卷号 | 370期号:6515 |
英文摘要 | Pyrite is a ubiquitous iron sulfide mineral that is oxidized by trace oxygen. The mineral has been largely absent from global sediments since the rise in oxygen concentration in Earth's early atmosphere. We analyzed weathering in shale, the most common rock exposed at Earth's surface, with chemical and microscopic analysis. By looking across scales from 10-9 to 102 meters, we determined the factors that control pyrite oxidation. Under the atmosphere today, pyrite oxidation is rate-limited by diffusion of oxygen to the grain surface and regulated by large-scale erosion and clast-scale fracturing. We determined that neither iron- nor sulfur-oxidizing microorganisms control global pyrite weathering fluxes despite their ability to catalyze the reaction. This multiscale picture emphasizes that fracturing and erosion are as important as atmospheric oxygen in limiting pyrite reactivity over Earth's history. © 2020 American Association for the Advancement of Science. All rights reserved. |
英文关键词 | ferric hydroxide; iron oxide; oxygen; pyrite; abiotic factor; concentration (composition); diffusion; iron sulfide; microbial activity; microstructure; oxidation; pyrite; rock microstructure; sediment analysis; trace element; weathering rate; catalysis; catalyst; grain size; trace gas; weathering; abiotic stress; Article; catchment area (hydrology); chemical reaction kinetics; concentration (parameter); controlled study; density; electron diffraction; environmental erosion; environmental exposure; high resolution transmission electron microscopy; microbial activity; microorganism; nonhuman; oxidation; porosity; priority journal; scanning transmission electron microscopy; stoichiometry; weathering; acidification; catalysis; catchment area; diffusion; land use; scanning electron microscopy; surface property; transmission electron microscopy |
语种 | 英语 |
来源期刊 | Science
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/243889 |
作者单位 | Department of Geosciences, Pennsylvania State University, University Park, PA 16802, United States; Instituto de Física, Universidade Federal Fluminense, Avenida Litorânea s/n, Niterói, RJ, 24210-340, Brazil; Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA 16802, United States |
推荐引用方式 GB/T 7714 | Gu X.,Heaney P.J.,Reis F.D.A.A.,et al. Deep abiotic weathering of pyrite[J],2020,370(6515). |
APA | Gu X.,Heaney P.J.,Reis F.D.A.A.,&Brantley S.L..(2020).Deep abiotic weathering of pyrite.Science,370(6515). |
MLA | Gu X.,et al."Deep abiotic weathering of pyrite".Science 370.6515(2020). |
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