The influence of pH, ionic strength and reactant concentrations on copper complexing by humified organic matter.

Summary The effects of varying the pH and ionic strength, and the concentrations of organic matter, copper, calcium and phosphate upon the complexing of copper by extracts of humified organic matter from laboratory preparations, soil and peat were measured. The extent of complexing increased as pH increased and ionic strength decreased, and with increasing organic matter: copper ratios in a way consistent with the complexant being heterogeneous. Calcium competed with copper for organic matter, but the effect of phosphate was negligible. The extent of complexing at pH 7 by equal weights of colloidal and dialysable material from the same extract were usually similar. Weight for weight of organic carbon, alkali-extracted humified organic matter complexed copper much more extensively than the corresponding water-soluble material.

[1]  J. Weber,et al.  Stability constants for the complexation of copper(II) ions with water and soil fulvic acids measured by an ion selective electrode , 1978 .

[2]  T. Takamatsu,et al.  DETERMINATION OF STABILITY CONSTANTS OF METAL‐HUMIC ACID COMPLEXES BY POTENTIOMETRIC TITRATION AND ION‐SELECTIVE ELECTRODES , 1978 .

[3]  J. R. Sanders,et al.  THE COMPLEXING OF COPPER BY HUMIFIED ORGANIC MATTER FROM LABORATORY PREPARATIONS, SOIL AND PEAT , 1977 .

[4]  J. Buffle,et al.  Measurement of complexation properties of humic and fulvic acids in natural waters with lead and copper ion-selective electrodes. , 1977, Analytical chemistry.

[5]  A. Mann,et al.  Solution geochemistry of copper in water containing carbonate, sulphate and chloride ions , 1977 .

[6]  F. J. Stevenson Stability constants of Cu/sup 2 +/, Pb/sup 2 +/, and Cd/sup 2 +/ complexes with humic acids , 1976 .

[7]  G. Pruden,et al.  A comparison of the compositions and properties of natural and laboratory-prepared humified organic matter , 1975 .

[8]  D. S. Gamble,et al.  METAL-FULVIC ACID CHELATION EQUILIBRIUM IN AQUEOUS NaNO3 SOLUTION. Hg(II), Cd(II), AND Cu(II) FULVATE COMPLEXES , 1974 .

[9]  V. Cheam CHELATION STUDY OF COPPER (II): FULVIC ACID SYSTEM , 1973 .

[10]  W. I. Kelso,et al.  THE MOBILIZATION AND FIXATION OF MOLYBDENUM, VANADIUM, AND URANIUM BY DECOMPOSING PLANT MATTER , 1973 .

[11]  G. Bradford,et al.  TRACE AND MAJOR ELEMENT CONTENTS OF SOIL SATURATION EXTRACTS , 1971 .

[12]  M. Stiff Copper/bicarbonate equilibria in solutions of bicarbonate ion at concentrations similar to those found in natural water , 1971 .

[13]  M. Lévesqué CHARACTERIZATION OF MODEL AND SOIL ORGANIC MATTER METAL-PHOSPHATE COMPLEXES , 1969 .

[14]  W. Lindsay,et al.  Micronutrient Cation Complexing in Soil Solution: II. Complexing of Zinc and Copper in Displaced Solution from Calcareous Soils , 1966 .

[15]  R. Soper,et al.  INTERACTION OF PHOSPHATES WITH FERRIC ORGANIC COMPLEXES , 1963 .