Anthropogenic chlorofluorocarbons in the Black Sea and the Sea of Marmara

Measurements of the distributions of two chlorofluorocarbons, CCl3F (CFC-11) and CCl2F2 (CFC-12), made during the June/July 1988 R. V. Knorr cruise in the Black Sea indicate that CFC-11 is non-conservative relative to CFC-12 in the strongly reducing anoxic waters. A multi-layer model combining horizontal/vertical renewal and vertical diffusion processes was tuned to the distributions of CFC-12 and salinity in suboxic and anoxic waters and used to estimate the residence times of subsurface waters and first-order in situ removal rate constants for CFC-11. The model-calculated residence times were B5 yr in the suboxic zone (80–120 m) and increased to B625 yr at 500 m. The first-order CFC-11 in situremoval coefficients were 0.52 70.19 yr � 1 for the depth range 160–480 m. Based on the observed CFC-12 concentrations, the residence time of cold intermediate layer water (B50–100 m) was estimated to be o5 yr. The residence time of the deep water (100–450 m) in the Sea of Marmara was estimated to be 12–19 yr using a box model tuned to CFC-12, implying an in situ oxygen utilization rate of 10–18mmol kg � 1 yr � 1 . r 2002 Elsevier Science Ltd. All

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