{"title":"Oxygen Fugacity Buffers and an Interactive Calculator","authors":"Michael Anenburg","doi":"10.1029/2026GC013032","DOIUrl":null,"url":null,"abstract":"<p>Oxygen fugacity buffers are equilibrium phase assemblages that constrain the chemical potential of oxygen. They may be coexisting minerals or fluids, or their metastable extrapolations. Oxygen fugacity values vary as a function of pressure and temperature, such that raw numbers often have little interpretive value. Instead, oxygen fugacity is generally reported relative to oxygen fugacity buffers that provide convenient and tangible reference curves. The exact calculation of these curves is typically highly complex, involving the solution of thermodynamic relationships using advanced algebra, calculus, and numerical methods. As a result, buffers are often calculated using simple parameterizations which are easily implemented. This simplification of oxygen fugacity buffer curves comes at the cost of accuracy and precision in pressure and temperature space. Occasionally, several parameterizations for a single buffer exist, causing discrepancies in published results. Here, we introduce an online calculator built using the shiny package for the R programming language. The calculator solves the often complex thermodynamics and provides a simple interface for users to manipulate input parameters. All calculations are fully documented and justified. This paper describes some of the common calculation methods for oxygen fugacity buffers, including 1 bar parameterizations, correct usage of tabulated standard pressure data, high-pressure equations of state and phase transitions, gas mixing at low and high pressures, and more. A description of the many challenges and problems in the current literature is provided, and recommendations for future calibrations are suggested.</p>","PeriodicalId":50422,"journal":{"name":"Geochemistry Geophysics Geosystems","volume":"27 8","pages":""},"PeriodicalIF":3.3000,"publicationDate":"2026-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2026GC013032","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochemistry Geophysics Geosystems","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2026GC013032","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Oxygen fugacity buffers are equilibrium phase assemblages that constrain the chemical potential of oxygen. They may be coexisting minerals or fluids, or their metastable extrapolations. Oxygen fugacity values vary as a function of pressure and temperature, such that raw numbers often have little interpretive value. Instead, oxygen fugacity is generally reported relative to oxygen fugacity buffers that provide convenient and tangible reference curves. The exact calculation of these curves is typically highly complex, involving the solution of thermodynamic relationships using advanced algebra, calculus, and numerical methods. As a result, buffers are often calculated using simple parameterizations which are easily implemented. This simplification of oxygen fugacity buffer curves comes at the cost of accuracy and precision in pressure and temperature space. Occasionally, several parameterizations for a single buffer exist, causing discrepancies in published results. Here, we introduce an online calculator built using the shiny package for the R programming language. The calculator solves the often complex thermodynamics and provides a simple interface for users to manipulate input parameters. All calculations are fully documented and justified. This paper describes some of the common calculation methods for oxygen fugacity buffers, including 1 bar parameterizations, correct usage of tabulated standard pressure data, high-pressure equations of state and phase transitions, gas mixing at low and high pressures, and more. A description of the many challenges and problems in the current literature is provided, and recommendations for future calibrations are suggested.
期刊介绍:
Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged.
Areas of interest for this peer-reviewed journal include, but are not limited to:
The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution
Principles and applications of geochemical proxies to studies of Earth history
The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them
The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales
Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets
The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets
Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.