Jago Colin, Robins Peter, Howlett Eleanor, Hassard Francis, Rajko-Nenow Paulina, Jackson Suzanna, Chien Nguyen, Malham Shelagh
School of Ocean Sciences, Bangor University, Marine Centre Wales, Menai Bridge LL59 5AB, UK.
School of Ocean Sciences, Bangor University, Marine Centre Wales, Menai Bridge LL59 5AB, UK.
Sci Total Environ. 2024 Mar 20;917:170343. doi: 10.1016/j.scitotenv.2024.170343. Epub 2024 Jan 26.
Hydrodynamic controls of the transport of suspended particulate matter (SPM), particulate nutrients and faecal indicator organisms (FIOs) in the river-estuary transition zone (RETZ) of a shallow macrotidal estuary were studied on tidal and seasonal timescales. The RETZ was found to be a conduit for SPM rather than a zone of particle accumulation during spring tides, with complex size fractionation and biogeochemical exchanges of particulate nutrient/FIO compositions. The downstream RETZ was characterised by flood-dominant currents, but with ebb-dominant turbulence due to the suppression of flood tide turbulence by salinity stratification created by lateral convergence; this produced a net seaward mass transport of SPM. Without lateral convergence in the narrower upstream RETZ, flood-dominant currents and flood-dominant turbulence were experienced. Hence the RETZ exported SPM landwards from its upper end and seawards from its lower end - a process observed throughout the year during spring tides and low-to-mean river flows. During neap tides when SPM concentrations were reduced, the RETZ became a zone of minor particle accumulation as its lower end imported SPM landwards from the estuary and its upper end imported SPM seawards from the river. During a river flood event, net SPM flux was significantly increased and was seawards throughout the RETZ. SPM mass concentration and carbon, nitrogen, phosphorous, and FIO concentrations peaked due to local resuspension and advection of an ephemeral estuarine turbidity maximum (ETM). The ETM formed on the advancing flood tide due to entrainment of material from intertidal flats. Flocculation and settling occurred at high slack water. The ETM was reconstituted by entrainment on the ebb and was composed of larger flocs than on the flood. Particulate nutrients and FIOs were associated with flocs in the 10-200 μm range but not with smaller or larger flocs. SPM concentrations in the resuspension component and ETM exceeded microbial water quality standards, emphasising the need for monitoring practices that consider tidal dynamics. The results from this study showing periodic SPM export from, rather than prolonged accumulation in, the RETZ and the influence of particle size fractionation on biogeochemical fluxes in the RETZ, are likely to be transferable to many other embayment-type estuaries on macrotidal coasts.
在潮汐和季节时间尺度上,研究了一个大型浅海潮河口的河口过渡带(RETZ)中悬浮颗粒物(SPM)、颗粒态养分和粪便指示生物(FIOs)的水动力输运控制。研究发现,在大潮期间,RETZ是SPM的输送通道,而非颗粒物质的积累区,在此期间颗粒态养分/FIOs组成存在复杂的粒径分级和生物地球化学交换。RETZ下游以涨潮为主导的水流为特征,但由于横向汇聚产生的盐度分层抑制了涨潮紊流,退潮主导的紊流较为明显;这导致了SPM的净向海物质输运。在较窄的上游RETZ中,没有横向汇聚,水流以涨潮为主导,紊流也以涨潮为主导。因此,RETZ在其上端向陆地输出SPM,在其下端向海洋输出SPM——这一过程在大潮期间以及河流低流量至平均流量时全年都可观察到。在小潮期间,当SPM浓度降低时,RETZ成为一个较小的颗粒积累区,因为其下端从河口向陆地输入SPM,其上端从河流向海洋输入SPM。在河流洪水事件期间,SPM的净通量显著增加,并且在整个RETZ中都是向海的。由于短暂的河口最大浑浊带(ETM)的局部再悬浮和平流作用,SPM质量浓度以及碳、氮、磷和FIO浓度达到峰值。ETM在涨潮推进时由于潮间带物质的夹带而形成。在高平潮时发生絮凝和沉降。ETM在退潮时通过夹带作用重新形成,并且由比涨潮时更大的絮凝体组成。颗粒态养分和FIOs与10 - 200μm范围内的絮凝体相关,但与更小或更大的絮凝体无关。再悬浮组分和ETM中的SPM浓度超过了微生物水质标准,这强调了考虑潮汐动力学的监测实践的必要性。本研究结果表明RETZ存在周期性的SPM输出而非长期积累,以及粒径分级对RETZ中生物地球化学通量的影响,这些结果可能适用于许多其他大型潮控海岸的港湾型河口。