Estimating benthic Fe and reactive solute fluxes
暂无分享,去创建一个
[1] W. Burnett,et al. A global assessment of the mixed layer in coastal sediments and implications for carbon storage , 2022, Nature Communications.
[2] D. König,et al. Iron colloids dominate sedimentary supply to the ocean interior , 2021, Proceedings of the National Academy of Sciences.
[3] C. Slomp,et al. Coastal hypoxia and eutrophication as key controls on benthic release and water column dynamics of iron and manganese , 2020, Limnology and Oceanography.
[4] D. Burdige,et al. Iron redox cycling, sediment resuspension and the role of sediments in low oxygen environments as sources of iron to the water column , 2020, Marine Chemistry.
[5] Lin Wei,et al. Large benthic fluxes of dissolved iron in China coastal seas revealed by 224Ra/228Th disequilibria , 2019, Geochimica et Cosmochimica Acta.
[6] J. Erez,et al. Comparing Rhizon samplers and centrifugation for pore‐water separation in studies of the marine carbonate system in sediments , 2018, Limnology and Oceanography: Methods.
[7] F. Meysman,et al. Two dimensional mapping of iron release in marine sediments at submillimetre scale , 2017 .
[8] G. Henderson,et al. Quantifying trace element and isotope fluxes at the ocean–sediment boundary: a review , 2016, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[9] A. Oschlies,et al. A revised global estimate of dissolved iron fluxes from marine sediments , 2015 .
[10] L. Nielsen,et al. Rethinking sediment biogeochemistry after the discovery of electric currents. , 2015, Annual review of marine science.
[11] L. Wehrmann,et al. Iron and manganese speciation and cycling in glacially influenced high-latitude fjord sediments (West Spitsbergen, Svalbard): Evidence for a benthic recycling-transport mechanism , 2014 .
[12] J. Moffett,et al. The flux of iron and iron isotopes from San Pedro Basin sediments , 2012 .
[13] R. Aller,et al. Two-dimensional dissolved ferrous iron distributions in marine sediments as revealed by a novel planar optical sensor , 2012 .
[14] P. Statham,et al. Dissolved oxygen and suspended particles regulate the benthic flux of iron from continental margins , 2012 .
[15] M. Taillefert,et al. The flux of soluble organic‐iron(III) complexes from sediments represents a source of stable iron(III) to estuarine waters and to the continental shelf , 2011 .
[16] D. Wethey,et al. Mechanical imitation of bidirectional bioadvection in aquatic sediments , 2011 .
[17] D. Hammond,et al. The continental shelf benthic iron flux and its isotope composition , 2010 .
[18] R. Glud. Oxygen dynamics of marine sediments , 2008 .
[19] K. Bruland,et al. Elevated Fe(II) and dissolved Fe in hypoxic shelf waters off Oregon and Washington: an enhanced source of iron to coastal upwelling regimes. , 2008, Environmental science & technology.
[20] P. Worsfold,et al. Distribution and redox speciation of dissolved iron on the European continental margin , 2007 .
[21] M. Taillefert,et al. The effect of tidal forcing on biogeochemical processes in intertidal salt marsh sediments , 2007, Geochemical transactions.
[22] R. Feely,et al. Relating estimates of CaCO3 production, export, and dissolution in the water column to measurements of CaCO3 rain into sediment traps and dissolution on the sea floor: A revised global carbonate budget , 2007 .
[23] T. Lyons,et al. A critical look at iron paleoredox proxies: New insights from modern euxinic marine basins , 2006 .
[24] J. Morse,et al. Dissolved Fe2+ and ∑H2S Behavior in Sediments Seasonally Overlain by Hypoxic-to-anoxic Waters as Determined by CSV Microelectrodes , 2006 .
[25] J. R. Nelson,et al. Organic matter remineralization and porewater exchange rates in permeable South Atlantic Bight continental shelf sediments , 2005 .
[26] Michael Schlüter,et al. Rhizon sampling of porewaters near the sediment‐water interface of aquatic systems , 2005 .
[27] R. Aller. Conceptual models of early diagenetic processes: The muddy seafloor as an unsteady, batch reactor , 2004 .
[28] K. Coale,et al. The flux of iron from continental shelf sediments: A missing source for global budgets , 2004 .
[29] A. Roychoudhury,et al. The ferrozine method revisited: Fe(II)/Fe(III) determination in natural waters , 2000 .
[30] G. Luther,et al. Reactivity of Freshly Formed Fe(III) in Synthetic Solutions and (Pore)Waters: Voltammetric Evidence of an Aging Process , 2000 .
[31] B. Jørgensen,et al. Manganese, iron and sulfur cycling in a coastal marine sediment, Aarhus bay, Denmark , 1994 .
[32] F. Millero,et al. The oxidation kinetics of Fe(II) in seawater , 1987 .
[33] Per O.J. Hall,et al. The effect of oxygen on release and uptake of cobalt, manganese, iron and phosphate at the sediment-water interface , 1986 .
[34] B. Boudreau,et al. A model for the diffusion-controlled growth of deep-sea manganese nodules , 1978 .
[35] L. Stookey. Ferrozine---a new spectrophotometric reagent for iron , 1970 .
[36] G. Lee,et al. Oxygenation of Ferrous Iron , 1961 .
[37] D. Canfield,et al. The Iron Biogeochemical Cycle Past and Present , 2012 .
[38] T. Anderson,et al. Reactive iron enrichment in sediments deposited beneath euxinic bottom waters: constraints on supply by shelf recycling , 2005, Geological Society, London, Special Publications.
[39] B. Thamdrup. Bacterial Manganese and Iron Reduction in Aquatic Sediments , 2000 .
[40] Ronnie N. Glud,et al. Benthic chamber and profiling landers in oceanography-A review of design, technical solutions and functioning. , 1995 .
[41] R. Aller,et al. Diagenesis of Fe and S in Amazon inner shelf muds: apparent dominance of Fe reduction and implications for the genesis of ironstones , 1986 .
[42] G. Gill,et al. The geochemistry of iron in puget sound , 1978 .
[43] Konrad B. Krauskopf,et al. Separation of manganese from iron in sedimentary processes , 1957 .