Redox zonation: Equilibrium constraints on the Fe(III)/SO4-reduction interface
- 1 September 1996
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 60 (17) , 3169-3175
- https://doi.org/10.1016/0016-7037(96)00156-1
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Deep subsurface microbial processesReviews of Geophysics, 1995
- Deducing the Distribution of Terminal Electron‐Accepting Processes in Hydrologically Diverse Groundwater SystemsWater Resources Research, 1995
- Field and laboratory studies of methane oxidation in an anoxic marine sediment: Evidence for a methanogen‐sulfate reducer consortiumGlobal Biogeochemical Cycles, 1994
- Reductive dissolution of iron(III) (hydr)oxides by hydrogen sulfideLangmuir, 1992
- Competitive Exclusion of Sulfate Reduction by Fe(lll)‐Reducing Bacteria: A Mechanism for Producing Discrete Zones of High‐Iron Ground WaterGroundwater, 1992
- Microbial production of organic acids in aquitard sediments and its role in aquifer geochemistryNature, 1991
- Sediment biogeochemistry of iron and sulfur in an acidic lakeGeochimica et Cosmochimica Acta, 1989
- Hydrogen concentrations as an indicator of the predominant terminal electron-accepting reactions in aquatic sedimentsGeochimica et Cosmochimica Acta, 1988
- Distributions of Ferrous Iron and Sulfide in an Anoxic HypolimnionCanadian Journal of Fisheries and Aquatic Sciences, 1984
- Oxidation–reduction sequences in ground water flow systemsCanadian Journal of Earth Sciences, 1979