Tj. Andersen et al., Deposition and mixing depths on some European intertidal mudflats based onPb-210 and Cs-137 activities, CONT SHELF, 20(12-13), 2000, pp. 1569-1591
Vertical profiles of Pb-210 and Cs-137 have been collected at micro-, meso-
and macrotidal mudflats in order to calculate present accumulation rates.
Sediment cores were taken at the mudflat at Kongsmark in the microtidal Lis
ter Dyb tidal area (Denmark), at the BOA bridge in the mesotidal Dollard es
tuary (Netherlands), and at the Skeffling mudflat in the macrotidal Humber
estuary (UK). Except for the Kongsmark site and site A in the Humber estuar
y, no accurate calculation of accumulation rates was possible for the inves
tigated sites. The accumulation rate obtained for the Kongsmark site is con
firmed by other independent data and shows that the accumulation is not sup
ply limited at this site at present. For site A in the Humber estuary a mod
ified CIC method was applied to the Pb-210-profile and the result agrees wi
th results from the nearby Welwick Marsh. The salt marsh at Skeffling is ad
vancing out onto the fringing mudflat with accumulation at the innermost pa
rt of the mudflat but with erosion taking place further offshore. The reaso
ns for the generally poor dating results seems to be either erosion (two Hu
mber sites) or postdepositional reworking of the deposited material (biotur
bation and continued resuspension) and the data set suggests that the mixin
g depth may increase with tidal range and thereby hydrodynamic forcing. (C)
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