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Sediment dynamics and resuspension processes in a shallow-water Posidonia oceanica meadow

机译:浅水中的沉积物动力学和重悬浮过程 posidonia大洋洲草地

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In the study, we describe the sedimentary dynamics in a shallow-water seagrass meadow. We examined the dynamics of vertical sedimentation flux over aPosidonia oceanicameadow during the course of a one-year investigation. Total sedimentary flux was monitored off the northern Latium coast (Italy) in the central Tyrrhenian Sea using sediment traps from October 2015 to December 2016 at three stations established on bare sand, in theP. oceanicameadow, and on a sand patch within the meadow. The traps were deployed during 11 surveys planned on the basis of the weather conditions and seagrass growth phase. The trap content was analysed for the amount of mass trapped and particle grain size, useful for describing sedimentary processes during storms. The meteorological data,P. oceanicaleaf biometry, and sand patch evolution during the year were analysed to determine their relation to the vertical sedimentation flux. The resuspension process dominated the shallow-water dynamics, butP. oceanicabuffers the resuspension, especially during calm sea conditions. The sedimentological tracers showed that when high energy-flow regimes were present, the vegetation near the bottom enhanced the deposition of particles transported from adjacent unvegetated areas. During late summer, leaf litter deposited on the unvegetated seafloor buffered the seabed sediment particles, preventing resuspension. We also detected the active transport of material from the sand patch to the meadow that was dependent on the energy flow regime, showing that the vegetation plays two roles: preventing resuspension and promoting deposition.
机译:在研究中,我们描述了浅水海草草甸中的沉积动态。在一年的调查过程中,我们检查了垂直沉积助焊剂的动态。从2015年10月到2016年10月到2016年12月在2016年12月,在2016年12月,在2016年12月,在2016年12月,在2016年12月,在2016年12月在裸露的沙滩上,在裸露的沙滩上。 Oceanicameadow,以及在草地上的沙子贴片。在11个调查期间部署了陷阱,该计划根据天气条件和海草生长阶段进行计划。分析捕集物含量的捕获量和颗粒粒度,可用于描述风暴期间的沉积过程。气象数据,p。在年内OceaniceAdeaFomometry和沙贴进化分析,以确定其与垂直沉降通量的关系。重悬浮过程主导了浅水动力学,Butp。 Oceoicabuffers重新悬浮,特别是在平静的海洋状况期间。沉积物示踪剂表明,当存在高能量流动制度时,底部附近的植被增强了从相邻的未凝固区域输送的颗粒的沉积。在夏末期间,叶子凋落物沉积在未在线的海底缓冲海底沉积物粒子,防止重悬浮。我们还检测到从沙贴片到依赖于能量流动制度的草地的材料的主动运输,表明植被起作用两个角色:防止重悬浮和促进沉积。

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