Pj. Statham et al., 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), 1993, pp. 541-552
Measurements of dissolved and particulate Cd, Co, Cu, Fe, Mn, Ni, Pb a
nd 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 prog
ramme. These measurements have been integrated with data on fluxes of
water and suspended particulate matter also obtained within the Fluxma
nche programme to provide estimates of fluxes of these elements into t
he southern North Sea. For Fe, Mn, and Pb, particulate fluxes are grea
ter than dissolved fluxes, whilst the reverse is true for Cd, Cu and N
i. Significant daily changes in magnitude of the modelled fluxes of wa
ter through the Strait when combined with averaged metal concentration
s over longer timescales, result in large changes of fluxes of metals
on a day to day basis. However, relatively small changes are evident f
or integrated autumn fluxes of metals for consecutive years using the
available database. The annual fluxes of dissolved plus-leachable part
iculate 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%).