Geochemical production of reactive oxygen species from biogeochemically reduced Fe

Environmental Science and Technology

Volumn 48, Issue 7, 2014, Pages 3815-3821

  Murphy, Sarah A ^a   Solomon, Benson M ^a   Meng, Shengnan ^a   Copeland, Justin M ^a   Shaw, Timothy J ^a   Ferry, John L ^a  

^a UNIVERSITY OF SOUTH CAROLINA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CHEMICAL PLANTS; GEOCHEMISTRY; GROUNDWATER; HYDROGEN PEROXIDE; OXYGEN; SEDIMENTS; SULFUR COMPOUNDS;

ACID VOLATILE SULFIDES; HYDROGEN PEROXIDE PRODUCTION; MAXIMUM CONCENTRATIONS; ORGANIC CARBON CONTENTS; PHOTOCHEMICAL REDUCTION; PREDICTIVE MODELING; PRODUCTION OF HYDROGEN; REACTIVE OXYGEN SPECIES;

PEROXIDES;

DISSOLVED OXYGEN; HYDROGEN PEROXIDE; HYDROGEN SULFIDE; IRON; ORGANIC CARBON; REACTIVE OXYGEN METABOLITE; SULFIDE;

ANOXIC CONDITIONS; BIOGEOCHEMISTRY; EPISODIC EVENT; HYDROGEN PEROXIDE; IRON; OXYGEN; PHOTOCHEMISTRY; SEDIMENT CHEMISTRY; TIDAL CYCLE;

AIR; ARTICLE; BIOGEOCHEMICAL CYCLING; CATALYSIS; EBB TIDE; ESTUARY; GEOCHEMISTRY; LIMIT OF DETECTION; OXIDATION; OXYGEN CONCENTRATION; SEDIMENT; UNITED STATES;

MURRELLS INLET; SOUTH CAROLINA; UNITED STATES;

GEOLOGIC SEDIMENTS; HYDROGEN PEROXIDE; HYDROGEN SULFIDE; IRON; MODELS, THEORETICAL; OXIDATION-REDUCTION; REACTIVE OXYGEN SPECIES; SOUTH CAROLINA; TIME FACTORS;

EID: 84897480117     PISSN: 0013936X     EISSN: 15205851     Source Type: Journal    
DOI: 10.1021/es4051764     Document Type: Article

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