Isotopically exchangeable concentrations of elements having multiple oxidation states: The case of Fe(II)/Fe(III) isotope self-exchange in coastal lowland acid sulfate soils

Environmental Science and Technology

Volumn 43, Issue 14, 2009, Pages 5365-5370

  Collins, Richard N ^a   David Waite, T ^a  

^a UNIVERSITY OF NEW SOUTH WALES   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

ACID SULFATE SOILS; AQUATIC SYSTEM; COASTAL LOWLAND; DISTRIBUTION COEFFICIENT; DYNAMIC EQUILIBRIA; FE REDUCTIONS; GROUND WATER TABLE; HYDRAULIC PROPERTIES; ISOTOPE EXCHANGE TECHNIQUE; MULTIPLE OXIDATION; OXIDATION STATE; RELATIVE IMPORTANCE; SELF-EXCHANGE; SOIL HORIZON; SOIL SAMPLE; SOIL SOLIDS; SOLID-PHASE;

ACIDS; CONCENTRATION (PROCESS); GROUNDWATER; HYDROGEOLOGY; IRON COMPOUNDS; ISOTOPES; OXIDATION;

SOILS;

ACID; FERRIC ION; GROUND WATER; ISOTOPE; SULFATE;

ACID SULFATE SOIL; AGRICULTURAL RUNOFF; HYDRAULIC PROPERTY; IRON; LOWLAND ENVIRONMENT; OXIDATION; REDUCTION; SOIL HORIZON; SOIL MICROORGANISM;

ANALYTIC METHOD; AQUATIC ENVIRONMENT; AQUEOUS SOLUTION; ARTICLE; CHEMICAL REACTION KINETICS; CONCENTRATION (PARAMETERS); OXIDATION KINETICS; SAMPLING; SEASHORE; SOIL ANALYSIS; SOIL POLLUTION; SOLID STATE;

ACIDS; IRON; IRON ISOTOPES; OXIDATION-REDUCTION; SOIL; SULFATES;

EID: 67650462687     PISSN: 0013936X     EISSN: 15205851     Source Type: Journal    
DOI: 10.1021/es900190p     Document Type: Article

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