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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Deposition and mixing depths on some European intertidal mudflats based on Pb-210 and Cs-137 activities
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Deposition and mixing depths on some European intertidal mudflats based on Pb-210 and Cs-137 activities

机译:基于Pb-210和Cs-137活性的一些欧洲潮间带滩涂的沉积和混合深度

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摘要

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 Lister Dyb tidal area (Denmark), at the BOA bridge in the mesotidal Dollard estuary (Netherlands), and at the Skeffling mudflat in the macrotidal Humber estuary (UK). Except for the Kongsmark site and site A in the Humber estuary, no accurate calculation of accumulation rates was possible for the investigated sites. The accumulation rate obtained for the Kongsmark site is confirmed by other independent data and shows that the accumulation is not supply limited at this site at present. For site A in the Humber estuary a modified CIC method was applied to the Pb-210-profile and the result agrees with results from the nearby Welwick Marsh. The salt marsh at Skeffling is advancing out onto the fringing mudflat with accumulation at the innermost part of the mudflat but with erosion taking place further offshore. The reasons for the generally poor dating results seems to be either erosion (two Humber sites) or postdepositional reworking of the deposited material (bioturbation and continued resuspension) and the data set suggests that the mixing depth may increase with tidal range and thereby hydrodynamic forcing. (C) 2000 Elsevier Science Ltd. All rights reserved. [References: 38]
机译:Pb-210和Cs-137的垂直剖面已在微潮,中潮和大潮滩上收集,以计算当前的堆积率。沉积物岩心取自微潮李斯特河Dyb潮汐区(丹麦)的Kongsmark泥滩,中生的美元级河口(荷兰)的BOA桥以及大潮汐Humber河口(英国)的Skeffling泥滩。除了亨伯河口的Kongsmark站点和A站点外,无法对被调查站点进行准确的堆积率计算。其他独立数据也证实了Kongsmark站点的累积率,表明该站点目前的存储量不受限制。对于亨伯河口的站点A,对Pb-210剖面应用了一种改进的CIC方法,其结果与附近的韦尔威克沼泽(Welwick Marsh)的结果一致。 Skeffling的盐沼正在向边缘的泥滩前进,堆积在泥滩的最内部,但侵蚀发生在更远的海上。测年结果普遍较差的原因似乎是由于侵蚀(两个亨伯位点)或沉积材料的沉积后再加工(生物扰动和持续的重悬浮),数据集表明,混合深度可能随着潮汐范围的增加而增加,从而引起水动力强迫。 (C)2000 Elsevier ScienceLtd。保留所有权利。 [参考:38]

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