Collaborative Research: Oligohaline dispersion: transport processes at the estuary-tidal river transition

合作研究：寡盐分散：河口-潮汐河过渡过程中的传输过程

• 批准号: 2318999
• 负责人: David Ralston
• 金额: $ 44.93万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-09-01 至 2026-08-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2318999&HistoricalAwards=false
• 关键词: Collaborative; Research; Oligohaline; dispersion; transport

Transport processes controlling the salinity distribution in an estuary vary dynamically with the river discharge, tides, and meteorological events. Most of our understanding of the transport processes is based on studies of the central reach of estuaries. The upper reach near the landward limit of the salt intrusion, has distinct physical characteristics that make transport processes different from the central reach. This project will combine in-situ and shipboard observations, dye release studies, and realistic high-resolution modeling to quantify tidal dispersion in the upper reach of the Delaware River estuary. Analysis of the observations and modeling will be closely linked through direct comparisons, and together they will be used to quantify dispersion rates and identify the mechanisms. Bathymetric features like channel constrictions and bends as well as anthropogenic modifications like piers and dredged channels are expected to be particularly important to creating salinity and velocity anomalies that lead to net landward transport. The Delaware is representative of many estuaries around the world where water supplies drawn from tidal rivers are increasingly threatened by landward shifts in the oligohaline reach with sea level rise, changing precipitation, and dredging. Specifically, drinking water intakes for the Philadelphia Water District (PWD) are located just upstream of the study region, and the Delaware River Basin Commission (DRBC) controls river flow conditions regulate the salt intrusion and protect the water supply for millions. This project will build on established relationships between the PIs and colleagues at both PWD and DRBC to identify knowledge gaps and link study findings to management decisions. The PIs will also contribute to a series of workshops bringing together scientists and water resources managers to assess threats to water supplies by salt intrusion globally. The project will support a graduate student at Rutgers who will be involved in all aspects of the study, including observations, modeling, and outreach.The oligohaline reach (0.5-5 psu) is an important transition zone for many ecological and biogeochemical processes, and yet few studies have examined the physical mechanisms of transport. Several key characteristics distinguish the oligohaline from the central estuary. In the asymptote to freshwater, the along-estuary salinity gradient decreases and estuarine exchange flow weakens. Stratification also decreases, reducing the steady salt flux and increasing mixing, which reduces oscillatory shear dispersion. Channel narrowing affects lateral exchange and trapping, particularly in urbanized estuaries with shoreline modification. This project uses multiple, complementary approaches to quantify transport processes in this region. Observations during low river discharge will capture the spatial and temporal evolution of salinity with tidal and meteorological forcing, and dye releases will directly quantify dispersion at the scale of topographic features. Modeling will use a nested-grid approach to represent the bathymetric features driving dispersion, along with a novel analysis approach to isolate sources of non-local salt flux, as put forth by Dronkers and van de Kreeke (1986). A process-based understanding of transport in the oligohaline reach is critical to understanding how conditions there will evolve with climate change and continued development.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

控制河口盐度分布的输运过程随河流流量、潮汐和气象事件的变化而动态变化。我们对运输过程的大部分理解是基于对河口中央河段的研究。靠近盐侵陆缘的上游具有明显的物理特征，使运移过程不同于中部。该项目将结合现场和船上观测、染料释放研究和现实的高分辨率模型来量化特拉华河河口上游的潮汐分散。观测的分析和模拟将通过直接比较紧密地联系在一起，它们将一起用于量化扩散率和确定机制。水深特征，如河道收缩和弯曲，以及人为改变，如码头和疏浚河道，预计对造成盐度和速度异常特别重要，从而导致净向陆地移动。特拉华河是世界上许多河口的代表，在这些河口，由于海平面上升、降水变化和疏浚，从潮汐河流中汲取的水供应日益受到低盐河段向陆地移动的威胁。具体来说，费城水区（PWD）的饮用水取水口位于研究区域的上游，特拉华河流域委员会（DRBC）控制河流流量，调节盐分入侵，保护数百万人的供水。该项目将以pi与PWD和DRBC同事之间的既定关系为基础，确定知识差距，并将研究结果与管理决策联系起来。ppi还将为一系列研讨会做出贡献，这些研讨会汇集了科学家和水资源管理人员，以评估全球盐入侵对供水的威胁。该项目将支持罗格斯大学的一名研究生，他将参与研究的各个方面，包括观察、建模和推广。低盐河段（0.5 ~ 5 psu）是许多生态和生物地球化学过程的重要过渡带，但对其运移的物理机制研究较少。几个关键特征将低盐区与中央河口区区分开来。在淡水区渐近线，沿河口盐度梯度减小，河口交换流减弱。分层也减少了，减少了稳定的盐通量，增加了混合，从而减少了振荡剪切分散。河道变窄影响横向交换和捕获，特别是在海岸线改造的城市化河口。该项目使用多种互补的方法来量化该地区的运输过程。低流量期间的观测将捕捉盐度随潮汐和气象强迫的时空演变，而染料释放将直接量化地形特征尺度上的分散。建模将使用嵌套网格方法来表示驱动色散的水深特征，同时使用Dronkers和van de Kreeke（1986）提出的一种新的分析方法来隔离非局部盐通量的来源。基于过程的对低盐河段运输的理解对于理解气候变化和持续发展如何演变的条件至关重要。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。