Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria

A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic stre...

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Veröffentlicht in:Geochim. Cosmochim. Acta; (United States) 1988, Vol.52 (1), p.185-193
Hauptverfasser: Cabaniss, S.E., Shuman, M.S.
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description A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic strength 0.005–0.1. Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca ++ or Mg ++ from 0 to 10 mM slightly increases Cu ++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu ++ activity. An empirical N- site model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs.
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Suwannee River fulvic acid equilibria</title><title>Geochim. Cosmochim. Acta; (United States)</title><description>A cupric ion-selective electrode measured free Cu in solutions of Suwannee River fulvic acid (FA) in a series of 30 titrations carried out both at variable and at constant (5.14, 7.00, 8.44) pH. Total Cu varied 0.1–100 μM, dissolved organic carbon (DOC) 1–10 mg C/l, Ca and Mg 0–10 mM, and ionic strength 0.005–0.1. Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca ++ or Mg ++ from 0 to 10 mM slightly increases Cu ++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu ++ activity. An empirical N- site model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. 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Copper complexation by FA is first order in DOC for 1–10 mg C/liter, and variable-order in pH. Increasing Ca ++ or Mg ++ from 0 to 10 mM slightly increases Cu ++ activity, while increasing ionic strength from 0.005 to 0.1 significantly increases Cu ++ activity. An empirical N- site model was calibrated using a pooled set of six titrations with varying pH and DOC. Five binding components of varying proton dependence predict Cu binding by FA over a range of pH, DOC and total Cu in two verification tests of the model parameters. Parameters in this and other models tested are only empirical constructs.</abstract><cop>United States</cop><pub>Elsevier Ltd</pub><doi>10.1016/0016-7037(88)90066-X</doi><tpages>9</tpages></addata></record>
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subjects 580400 - Geochemistry- (-1989)
CALCIUM IONS
CARBON IONS
CHARGED PARTICLES
CHEMICAL ANALYSIS
CHEMICAL COMPOSITION
CHEMICAL REACTIONS
CHEMISTRY
COPPER IONS
EQUILIBRIUM
FULVIC ACIDS
GEOCHEMISTRY
GEOSCIENCES
IONS
MAGNESIUM IONS
MATHEMATICAL MODELS
MOLECULAR MODELS
ORGANIC ACIDS
ORGANIC COMPOUNDS
PH VALUE
RIVERS
STOICHIOMETRY
STREAMS
SURFACE WATERS
WATER CHEMISTRY
title Copper binding by dissolved organic matter: I. Suwannee River fulvic acid equilibria
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