Book contents
- Frontmatter
- Dedication
- Contents
- Preface
- Preface to Second Edition
- Preface to First Edition
- A Note About Software
- 1 Introduction
- 2 Modeling Overview
- PART I EQUILIBRIUM IN NATURAL WATERS
- PART II REACTION PROCESSES
- PART III APPLIED REACTION MODELING
- 26 Hydrothermal Fluids
- 27 Geothermometry
- 28 Evaporation
- 29 Sediment Diagenesis
- 30 Kinetics ofWater–Rock Interaction
- 31 Weathering
- 32 Oxidation and Reduction
- 33 Waste InjectionWells
- 34 Petroleum Reservoirs
- 35 Acid Drainage
- 36 Contamination and Remediation
- 37 Microbial Communities
- Appendix A Sources of Modeling Software
- Appendix B Evaluating the HMW Activity Model
- Appendix C Minerals in the LLNL Database
- Appendix D Nonlinear Rate Laws
- References
- Index
32 - Oxidation and Reduction
from PART III - APPLIED REACTION MODELING
Published online by Cambridge University Press: 09 December 2021
- Frontmatter
- Dedication
- Contents
- Preface
- Preface to Second Edition
- Preface to First Edition
- A Note About Software
- 1 Introduction
- 2 Modeling Overview
- PART I EQUILIBRIUM IN NATURAL WATERS
- PART II REACTION PROCESSES
- PART III APPLIED REACTION MODELING
- 26 Hydrothermal Fluids
- 27 Geothermometry
- 28 Evaporation
- 29 Sediment Diagenesis
- 30 Kinetics ofWater–Rock Interaction
- 31 Weathering
- 32 Oxidation and Reduction
- 33 Waste InjectionWells
- 34 Petroleum Reservoirs
- 35 Acid Drainage
- 36 Contamination and Remediation
- 37 Microbial Communities
- Appendix A Sources of Modeling Software
- Appendix B Evaluating the HMW Activity Model
- Appendix C Minerals in the LLNL Database
- Appendix D Nonlinear Rate Laws
- References
- Index
Summary
Many redox reactions in the natural environment proceed too slowly to approach their equilibrium state, absent the action of catalysts or enzymes. In this chapter, we consider how to trace multicomponent reaction paths in which the progress of redox reactions is described by kinetic rate laws. We frame our discussion in terms of three example calculations. In the first example, ferrous iron both catalyzes and provides reducing power to convert uranyl to insoluble uranium hydroxide. The autocatalysis of manganese, in which the reaction product operates as the catalyst that promotes the reaction, serves as the second example, and the microbial degradation of phenol makes up the final illustration of the method.
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- Geochemical and Biogeochemical Reaction Modeling , pp. 393 - 402Publisher: Cambridge University PressPrint publication year: 2022