Oxygen Fugacity Buffers and an Interactive Calculator

IF 3.3 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Michael Anenburg
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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.

Abstract Image

氧逸度缓冲器和交互式计算器
氧逸度缓冲液是限制氧化学势的平衡相组合。它们可能是共存的矿物质或液体,或者是它们的亚稳态外推。氧逸度值随压力和温度的变化而变化,因此原始数据通常没有什么解释价值。相反,氧逸度通常被报告为相对于氧逸度缓冲,提供方便和有形的参考曲线。这些曲线的精确计算通常是高度复杂的,涉及使用高级代数、微积分和数值方法求解热力学关系。因此,通常使用易于实现的简单参数化来计算缓冲区。这种氧逸度缓冲曲线的简化是以压力和温度空间的准确性和精度为代价的。有时,单个缓冲区存在多个参数化,从而导致公布的结果不一致。在这里,我们介绍一个使用R编程语言的闪亮包构建的在线计算器。该计算器解决了通常复杂的热力学问题,并为用户提供了一个简单的界面来操作输入参数。所有的计算都有充分的记录和证明。本文介绍了氧逸度缓冲液的一些常用计算方法,包括1 bar参数化、标准压力数据表的正确使用、高压状态和相变方程、低压和高压下的气体混合等。对当前文献中的许多挑战和问题进行了描述,并对未来的校准提出了建议。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
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.
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