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Difference in Particle Transport Between Two Coastal Areas in the Baltic Sea Investigated with High-Resolution Trajectory Modeling

机译:高分辨率轨迹建模研究波罗的海两个沿海地区之间的颗粒输运差异

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摘要

A particle-tracking model based on high-resolution ocean flow data was used to investigate particle residence times and spatial distribution of settling sediment for two geo-morphologically different Swedish coastal areas. The study was a part of a safety assessment for the location of a future nuclear-waste repository, and information about the particle-transport patterns can contribute to predictions of the fate of a possible leakage. It is also, to our knowledge, the first time particle-transport differences between two coastal areas have been quantified in this manner. In Forsmark, a funnel-shaped bay shielded by a number of islands, the average residence time for clay particles was 5 times longer than in the modeled part of Simpevarp, which is open to the Baltic Sea. In Forsmark, <10 % of the released particles left the domain compared to 60–80 % in Simpevarp. These site-specific differences will increase over time with the differences in land uplift between the areas.
机译:基于高分辨率海洋流量数据的粒子追踪模型用于研究两个地貌形态不同的瑞典沿海地区的粒子停留时间和沉降沉积物的空间分布。这项研究是对未来核废料储存库位置进行安全评估的一部分,有关粒子传输方式的信息可有助于预测可能发生的泄漏。据我们所知,这是第一次对两个沿海地区之间的颗粒运输差异进行了量化。在福斯马克(Forsmark)中,漏斗状的海湾被许多岛屿所遮蔽,黏土颗粒的平均停留时间比向波罗的海开放的辛佩瓦尔普(Simpevarp)的模型部分长5倍。在Forsmark中,<10%的已释放粒子离开了域,而Simpevarp中则只有60–80%。这些特定地点的差异将随着时间的推移而增加,因为这些地区之间的土地隆起差异也不同。

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