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Deposition of organic matter and particulate nitrogen and phosphorus at the North Sea-Baltic Sea transition - a GIS study

机译:北海-波罗的海过渡带的有机物沉积以及颗粒氮和磷沉积-GIS研究

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A GIS (Geographical Information System) based study on deposition in the North Sea-Baltic Sea transition area has been carried out. The study is based on (i) a digital bathymetry model, (ii) 93 available 210Pb / 137Cs sedimentation rate estimations, (iii) grain-size distributions, organic matter, C, N and P content of 64 top 1 cm sediment samples from the study area, and (iv) GIS-based modelling of resuspension potentials based on wind statistics. With the use of regression statistics on depth, resuspension potential and sediment characteristics, results are extrapolated area-wide from the 64 sampling positions. The area is divided into sediment types and classified as accumulation or erosion/transport bottoms. Model results show good agreement with existing maps of sediment distributions, indicating that the sediment distribution is governed to a large extent by wind-induced waves. Correlations of sediment types, their deposition rates and their N and P contents were used to estimate spatial deposition rates. In all, the yearly deposition in the study area amounts to 2.8 million tons of organic matter, 0.14 million tons of total nitrogen, and 0.035 million tons of total phosphorus. Correlations of sediment types and dry bulk densities were used to infer spatial inventories of organic matter and total nitrogen and phosphorus in the top 1 cm of the sediments. A total of 100 million tons of organic matter, 4 million tons of total nitrogen, and 0.019 million tons of total phosphorus are contained in the top 1 cm of the sediments in the study area. In general, the deep parts of the study area with low resuspension potentials act as sinks for the fine-grained sediments and their associated particulate nutrients.
机译:进行了基于GIS(地理信息系统)的北海-波罗的海过渡区沉积研究。该研究基于(i)数字测深模型,(ii)93种可用的210Pb / 137Cs沉降速率估算值,(iii)来自64个顶部1 cm沉积物样品的粒度分布,有机质,C,N和P含量研究领域;以及(iv)基于风力统计的基于GIS的重悬潜力建模。利用深度,重悬潜能和沉积物特征的回归统计数据,从64个采样位置向整个区域外推结果。该区域分为沉积物类型,分为堆积或侵蚀/运输底部。模型结果与已有的泥沙分布图显示出很好的一致性,表明泥沙分布在很大程度上受到风浪的影响。利用沉积物类型,沉积速率及其氮和磷含量的相关性来估算空间沉积速率。总的来说,研究区域的年沉积量为280万吨有机物,14万吨总氮和30.5万吨总磷。沉积物类型与干密度的相关性可用来推断沉积物顶部1 cm处的有机物以及总氮和磷的空间清单。在研究区域的前1 cm沉积物中总共含有1亿吨有机物,400万吨总氮和19.9万吨总磷。通常,研究区的深处具有低的重悬潜力,可作为细颗粒沉积物及其相关颗粒营养物的汇。

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