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My Goldschmidt

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All abstracts by William B. Homoky in conference series: Goldschmidt

(2023) Production of Geopolymerised Organic Carbon in Association with Iron at Hydrothermal Vents
Moore OW, Lough AJM, Woulds C, Homoky WB, Curti L & Peacock CL

(2023) Ligand-Induced Isotopically Heavy Zn Release during Marine Birnessite Transformation to Todorokite
Wang Z, Li W, Homoky WB, Little SH & Peacock CL

(2022) Iron & Manganese Catalysis of Reactive Organic Carbon Molecules into Stable Forms within Marine Sediments
Moore OW, Curti L, Woulds C, Bradley JA, Mills BJW, Homoky WB, Xiao K-Q, Babakhani P, Fisher BJ & Peacock CL

(2022) The Unreconciled Significance of Terrigenous Iron Supply for the Ocean Carbon Cycle
Homoky WB

(2018) Barium Isotopes in South Atlantic Sediment Pore Waters
Hsieh Y-T, Bridgestock L, Homoky WB & Henderson GM

(2018) Investigating the Isotopic Signature and Release of Iron Sourced from Sediments to the UK South Atlantic GEOTRACES GA10 Section
Summers B, Homoky W, Mills R, John S & Conway T

(2013) Fluid Flow and Redox Metal Cycling in Cayman Trough Hydrothermal Sediments
Mills RA & Homoky WB

(2013) Trace Metal Inputs from River-Fed and River-Starved Margin Sediments of the South Atlantic Ocean
Homoky WB, Mills RA, Hsieh Y-T, Hembury DJ, Woodward EMS & Henderson GM

(2013) Diagenetic Mobilisation of Fe and Mn in Hydrothermal Sediments
Aquilina A, Homoky WB, Hepburn LE, John SG, Conway TM, Lyons T & Mills RA

(2013) Suboxic Sediments as an Oceanic Sink of Isotopically-Light Cadmium
Horner TJ, Homoky WB, Georgiev SV, Stein HJ, Hannah JL, Mills RA, Rehkämper M & Henderson GM

(2013) Assessing the Dissolution of Marine Sediment with 230Th, and the Impact of Dissolution on Sedimentary 231Pa/230Th
Deng F, Henderson G, Thomas A, Homoky W & Mills R

(2011) Quantifying Fluxes of Metals to Surface Waters of the South-East Atlantic
Henderson GM, Achterberg E, Baker A, Chance R, Geibert W, Homoky W, Hwieh Y-T, Klunder M, Lohan M, Martin P, Mills R, Milne A, Palmer M, Sanders R, Thomas A, Wake B & Woodward M

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