Marine Chemistry, 14 (1984) 201--212
Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands
201
ORGANIC AND INORGANIC SPECIATION OF COPPER IN THE IRISH
SEA
CONSTANT M.G. VAN DEN BERG
Department of Oceanography, University of Liverpool, Liverpool L69 3BX (Gt. Britain)
(Received January 17, 1983 ; revision accepted August 22, 1983)
ABSTRACT
Van den Berg, C.M.G., 1984. Organic and inorganic speciation of copper in the Irish Sea.
Mar. Chem., 14: 201--212.
The metal complexing ability of surface water of the Irish Sea has been measured by
the MnO2 adsorption method. In all samples strong copper-chelating compounds are
present at concentrations of 60--150 nM, with conditional stability constants (log values)
of 10.0--10.4. The concentrations of Cu, Pb and Cd in the samples are 16--39 nM,
1--7nM and 0.1--2nM, respectively; much less than the ligand concentrations. The
organic compounds form complexes with 94--98% of dissolved copper, and therefore
constitute the major form of copper in surface water of the Irish Sea. Recalculation of
speciation of the inorganic fraction of copper in seawater reveals that the major complex
ion is that of CuCO ° (60%), followed by CuOH + (16%) and Cu(OH) ° (16%). Complexes
with borate ions form a small and rather insignificant fraction of 1%.
INTRODUCTION
The concentrations of trace metals in oceanic seawater are normally
extremely low and can be determined directly only by electrochemical
techniques unless some form of preconcentration is used. It is important,
nevertheless, to investigate their speciation, as several trace metals are known
to form complexes with inorganic and organic components of seawater. It is
likely that complexation affects strongly the bioavailability of metal ions
(Jackson and Morgan, 1978; van den Berg et al., 1979) as well as the removal
of trace metals from the seawater column by adsorption on settling particles.
Adsorption processes may be expected to suffer from competition from
dissolved complexing agents, although in some cases surface adsorption may
be enhanced by the presence of complexing material (Davis and Leckie,
1978).
Seawater is a medium of very complex composition, but the concentration
ratios of the major ions are constant. The concentrations of organic
complexing ligands are very low, but their complexing ability should never-
theless be investigated in this medium, without any alteration to the
concentrations of either complexing ligands or competing ions as this may
affect the distribution of metal ions over the various competing ligands in
soriition.
The separation of copper into organic and inorganic fractions has been
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