Abstract

Complexing capacities and complexation constants of copper by water samples taken from two sites of the Eassin d'Arcachon have been studied by DPASV. The variations are linked with those of water salinity and nature of sediment, 50% of the complexing capacity is due to <0,025 μm species. The fate of inorganic copper spikes has been studied in laboratory simulations of the water‐sediment system and the influence of suspended matter demonstrated.

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