The distribution of Cd and Ni in the sediments of Foundry Cove, a shallow embayment of the Hudson River, is determined as a function of distance from an industrial pointsource of Cd-Ni release. Concentrations of Cd and Ni decrease smoothly by 4 and 3 orders of magnitude, respectively, to the cove margin. High values in surface sediments decrease to preindustrial background levels of 2 ppm Cd and 30 ppm Ni at sediment depths of -20 cm. Budget calculations indicate that 20-50 tons of Cd and 10-30 tons of Ni are now present in the sediments of the cove. Cd is less mobile than Ni in the immediate vicinity of the industrial outfall due to the formation of a solid, mixed, calcium-cadmium carbonate phase from the alkaline waste discharge. Cesium-137 activity is useful in defining areas of sediment scour or recent dredging activities. Concentrations of Zn, Cu, and Pb are related to diffuse metal sources common to all recent Hudson sediments, and not to the local source of Cd and Ni. Preindustrial values of Pb, Cu, and Zn are found at approximately twice the depth for which background values of Cd and Ni are found.
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