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首页> 外文期刊>Geoscientific Model Development Discussions >Ecological ReGional Ocean Model with vertically resolved sediments (ERGOM?SED?1.0): coupling benthic and pelagic biogeochemistry of the south-western Baltic Sea
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Ecological ReGional Ocean Model with vertically resolved sediments (ERGOM?SED?1.0): coupling benthic and pelagic biogeochemistry of the south-western Baltic Sea

机译:具有垂直解决沉积物的生态区域海洋模型(ERGOM?SED?1.0):耦合弯曲和骨质生物地球化学的西南波罗的海

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Sediments play an important role in organic matter mineralisation and nutrient recycling, especially in shallow marine systems. Marine ecosystem models, however, often only include a coarse representation of processes beneath the sea floor. While these parameterisations may give a reasonable description of the present ecosystem state, they lack predictive capacity for possible future changes, which can only be obtained from mechanistic modelling. This paper describes an integrated benthic–pelagic ecosystem model developed for the German Exclusive Economic Zone (EEZ) in the western Baltic Sea. The model is a hybrid of two existing models: the pelagic part of the marine ecosystem model ERGOM and an early diagenetic model by Reed et al.?(2011). The latter one was extended to include the carbon cycle, a determination of precipitation and dissolution reactions which accounts for salinity differences, an explicit description of the adsorption of clay minerals, and an alternative pyrite formation pathway. We present a one-dimensional application of the model to seven sites with different sediment types. The model was calibrated with observed pore water profiles and validated with results of sediment composition, bioturbation rates and bentho-pelagic fluxes gathered by in situ incubations of sediments (benthic chambers). The model results generally give a reasonable fit to the observations, even if some deviations are observed, e.g. an overestimation of sulfide concentrations in the sandy sediments. We therefore consider it a good first step towards a three-dimensional representation of sedimentary processes in coupled pelagic–benthic ecosystem models of the Baltic Sea.
机译:沉积物在有机物质矿化和营养回收中发挥着重要作用,特别是在浅海洋系统中。然而,海洋生态系统模型通常仅包括海底下面的过程的粗略表示。虽然这些参数化可以给出对当前生态系统状态的合理描述,但它们缺乏可能的未来变化的预测能力,这只能从机械模型获得。本文介绍了为德国独家经济区(EEZ)开发的综合底栖 - 古典生态系统模型。该模型是两种现有模型的混合动态:海洋生态系统模型ERGOM的骨质部分和REED等人的早期成岩模型。(2011)。后者延伸到包括碳循环,测定沉淀和溶解反应的沉淀反应,其占盐度差异,是粘土矿物吸附的明确描述,以及替代的黄铁矿形成途径。我们将模型的一维应用到具有不同沉积物类型的七个站点。该模型用观察到的孔隙水谱校准并验证了沉积物组成的结果,生物干扰速率和通过原位孵育沉积物(底腔室)而收集的Bentho-pelagic助液。即使观察到某些偏差,模型结果通常给出合理的拟合,例如观察。含沙沉积物中硫化物浓度的高估。因此,我们认为它是朝向波罗的海耦合的骨质底栖生态系统模型的沉积过程的三维表示的良好第一步。

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