intro goals challenges background methane fluxes the methane barrier AOM hydro-acoustics microbiology methods - Seismics - Coring Equipment - Sediment physics - Sediment chemistry - Process rates - Microbiology - Molecular biology - Water column modeling database work packages working areas publications |
Reactive iron
Reactive iron is an operationally defined quantity of solid phase iron oxides that are thought to be available for bacterial iron reduction and/or sulfide oxidation. Iron oxides range from amorphous iron oxides (e.g., ferrihydrite) to more crystalline iron oxides such as goethite, magnetite, and hematite. Furthermore, iron may exist in the solid phase in its reduced, ferrous form adsorbed to surfaces, as sulfides (e.g., FeS, Fe3S4, FeS2), mixed oxides (e.g., magnetite), and in clays (e.g., in chlorite). Over the past thirty years a number of chemical extractions have been designed to extract and speciate one or more of these phases. Here we describe a protocol, based on the work of Kostka and Luther (1994), that attempts to distinguish amorphous iron oxides, magnetite, total reducible oxide iron, and readily extractable iron bound in silicates.
In this reaction we distinguish between readily reducible, amorphous iron oxides and iron contained in magnetite. The ascorbate step extracts the amorphous iron oxides and the oxalate step will attack magnetite (with some contributions from silicate bound iron). Reagents:
Step 1: Ascorbate Extraction: Add 10 mL of Ascorbate solution to a 50 mL screw-top, plastic centrifuge tube. Weigh 0.1 to 0.3 g of fresh sediment and add to solution. Extract for 24 hours with gentle shaking. Centrifuge (4500 rpm for 5 minutes) and save supernatant for Fe analysis. Step 2. Anaerobic Oxalate Extraction: Wrap centrifuge vial with remaining sediment with aluminum foil. De-gas Oxalate solution. Add 10 mL of oxalate solution to Corning vial and de-gas vial. Re-suspend sample and shake for 24 hours. Centrifuge (4500 rpm for 5 minutes) and measure Fe(II) and total Fe immediately. back to start sediment chemistry |