首页> 外文期刊>Science of the total environment >Historical Storage Budgets Of Organic Carbon, Nutrient And Contaminant Elements In Saltmarsh Sediments: Biogeochemical Context For Managed Realignment, Humber Estuary, Uk
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Historical Storage Budgets Of Organic Carbon, Nutrient And Contaminant Elements In Saltmarsh Sediments: Biogeochemical Context For Managed Realignment, Humber Estuary, Uk

机译:盐沼沉积物中有机碳,营养素和污染物元素的历史存储预算:受控重组的生物地球化学背景,亨伯河口,英国

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Biogeochemical data from Welwick marsh (Humber Estuary, UK), an actively accreting saltmarsh, provides a decadal-centennial-scale natural analogue for likely future biogeochemical storage effects of managed realignment sites accreting either intertidal muds or saltmarsh. Marsh topographic profiles and progradation history from aerial photographs were combined with ~(137)Cs and niobium contamination history to establish and verify chronology and sediment mass accumulation. These data, combined with down-core measurements of particulate organic carbon (C_(org)), organic nitrogen (N_(org)), particle reactive phosphorus and selected contaminant metal (Zn, Pb, Cu, As and Nb) contents were then used to calculate sediment and chemical storage terms and to quantify changes in these over time. These data are used to help predict likely future biogeochemical storage changes at managed realignment sites in the estuary. The net effect of returning some 26 km~2 of reclaimed land to intertidal environments now (about 25% of the maximum possible realignment storage identified for the estuary) could result in the storage of some 40,000 tonnes a~(-1) of sediment which would also bury about 800 tonnes a~(-1) of C_(org) and 40 tonnes a~(-1) of N_(org). Particulate contaminant P burial would be around 25 tonnes a~(-1) along with ~6 tonnes a~(-1) contaminant Zn, 3 tonnes a~(-1) contaminant Pb, and -1 tonnes a~(-1) contaminant As and Cu. The study also shows that reclamation activities in the outer estuary since the mid-1700s has prevented, in total, the deposition of about 10 million tonnes of sediment, along with 320,000 tonnes of C_(org) and 16,000 tonnes of N_(org). The study provides a mid-1990s baseline against which future measurements at the site can determine changes in burial fluxes and improvement or deterioration in contaminant metal contents of the sediments. The data are directly relevant for local managed realignment sites but also broadly indicative for sites generally on the European North Sea Coast.
机译:来自威尔克沼泽(英国汉伯河口)的生物地球化学数据,是一个活跃的盐沼,能够为十年来百年规模的天然类似物提供可能的生物地球化学存储效应,这些结果可能是潮间带泥或盐沼被管理的重排位点。将航拍的沼泽地貌轮廓和发展历史与〜(137)Cs和铌污染历史相结合,以建立和验证年代学和沉积物质量积累。然后,将这些数据与颗粒有机碳(C_(org)),有机氮(N_(org)),颗粒活性磷和选定的污染物金属(Zn,Pb,Cu,As和Nb)含量的下限测量值相结合。用于计算沉积物和化学存储项,并量化随时间的变化。这些数据用于帮助预测未来在河口管理的重新定位点可能发生的生物地球化学存储变化。现在将大约26 km〜2的填海造地恢复到潮间带环境的净效应(约为为河口确定的最大可能的整齐存储量的25%)可能导致大约40,000吨a〜(-1)沉积物的存储也将埋没约800吨a〜(-1)的C_(org)和40吨a〜(-1)的N_(org)。颗粒污染物P的埋葬量约为25吨a〜(-1)以及〜6吨a〜(-1)污染物Zn,3吨a〜(-1)污染物Pb和-1吨a〜(-1)污染物砷和铜。研究还显示,自1700年代中期以来,在外河口进行的填海活动总共阻止了大约1000万吨沉积物,32万吨C_(org)和16,000吨N_(org)的沉积。这项研究提供了1990年代中期的基线,根据该基线将来的测量可以确定埋藏通量的变化以及沉积物中污染物金属含量的改善或恶化。数据与本地管理的重组站点直接相关,但也广泛地指示了通常位于欧洲北海海岸的站点。

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