Fluxes of Cd, Co, Cu, Fe, Mn, Ni, Pb, and Zn through the strait of dover into the southern north-sea

Type Article
Date 1993
Language English
Author(s) Statham Pj, Auger Y, Burton Jd, Choisy P, Fischer Jc, James Rh, Morley Nh, Ouddane B, Puskaric E, Wartel M
Affiliation(s) UNIV SCI & TECH LILLE FLANDRES ARTOIS,CHIM ANALYT & MARINE LAB,F-59655 VILLENEUVE DASCQ,FRANCE
Meeting Channel Symposium on Fluxes and Processes within a Macrotidal Sea, BREST, FRANCE, SEP 02-04, 1992
Source Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 5-6 , P. 541-552
WOS© Times Cited 31
Keyword(s) DISSOLVED TRACE METALS, PARTICULATE TRACE METALS, SEAWATER, FLUXES, STRAIT OF DOVER
Abstract Measurements of dissolved and particulate Cd, Co, Cu, Fe, Mn, Ni, Pb and Zn have been made on a regular basis over a fifteen month period at stations across the Strait of Dover, as a part of the Fluxmanche programme. These measurements have been integrated with data on fluxes of water and suspended particulate matter also obtained within the Fluxmanche programme to provide estimates of fluxes of these elements into the southern North Sea. For Fe, Mn, and Pb, particulate fluxes are greater than dissolved fluxes, whilst the reverse is true for Cd, Cu and Ni. Significant daily changes in magnitude of the modelled fluxes of water through the Strait when combined with averaged metal concentrations over longer timescales, result in large changes of fluxes of metals on a day to day basis. However, relatively small changes are evident for integrated autumn fluxes of metals for consecutive years using the available database. The annual fluxes of dissolved plus-leachable particulate metals through the Strait of Dover relative to the most recent estimates of riverine and atmospheric inputs to the North Sea were in the order Cu (44%) > Cd (39%) > Zn (16%) > Pb (11%).
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Statham Pj, Auger Y, Burton Jd, Choisy P, Fischer Jc, James Rh, Morley Nh, Ouddane B, Puskaric E, Wartel M (1993). Fluxes of Cd, Co, Cu, Fe, Mn, Ni, Pb, and Zn through the strait of dover into the southern north-sea. Oceanologica Acta, 16(5-6), 541-552. Open Access version : https://archimer.ifremer.fr/doc/00100/21076/