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Spatial variation and availability of nutrients at an oyster reef in relation to submarine groundwater discharge

机译:与海底地下水排放有关的牡蛎礁养分的空间变化和有效性

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Submarine groundwater discharge (SGD) is often an overlooked component of the solute budgets in coastal em-bayments and is not considered in oyster restoration, conservation, and management plans. A combination of spatial and temporal geochemistry (nutrients, trace metals, alkalinity components, stable isotopes, and major ions) of porewater and surface water combined with SGD-derived solute fluxes and turnover times was used to examine the significance of SGD in delivering nutrients to paleovalley systems in coastal embayments, thus sustaining the health and productivity of oyster reefs. A 1-km~2 area encompassing a paleovalley system, in Copano Bay, Texas, exhibited significant differences in the spatial and temporal hydrogeochemical characteristics (major ions, stable isotopes and nutrients) along the reef when compared to the other environments (i.e., paleovalley, estuary-wide). Solute fluxes (i.e., dissolved organic carbon (DOC), dissolved inorganic nitrogen (DIN), total alkalinity, DIC, etc.) are slightly larger at the reef, followed by the margin and shoreline. During dry conditions, SGD from the 1-km~2 area was estimated to supply anywhere between two-fold to one order of magnitude more nitrogen (in the form of DIN) than the riverine inputs to Copano Bay. During a wet year SGD equates the river input in the form of DIN. In addition, SGD-based turnover times, averaging <11 days for all nutrients, are significantly shorter than the average estuary flushing time (i.e., 38 days). Results from this study suggest that SGD within a paleovalley system is an important component in the estuarine nutrient budget through significant inputs and cycling processes between the subsurface and water column, particularly during low surface flows. Thus, estuarine environments such as paleovalley margins and interfluves provide favorable conditions to oysters through preferably enhanced SGD solute fluxes and should be considered in oyster restoration efforts.
机译:海底地下水排放(SGD)通常是沿海河床溶质预算中被忽略的组成部分,在牡蛎修复,保护和管理计划中并未考虑。将孔隙水和地表水的时空地球化学(养分,微量金属,碱度成分,稳定同位素和主要离子)与SGD衍生的溶质通量和周转时间相结合,以检验SGD在将养分输送到土壤中的重要性。沿海沿岸的古卵系统,从而维持了牡蛎礁的健康和生产力。与其他环境(即古卵)相比,得克萨斯州科帕诺湾的一个包含古卵系统的1 km〜2区域沿珊瑚礁的时空水文地球化学特征(主要离子,稳定的同位素和养分)表现出​​显着差异。 ,整个河口)。珊瑚礁的溶质通量(即,溶解有机碳(DOC),溶解无机氮(DIN),总碱度,DIC等)稍大,其次是边缘和海岸线。在干旱条件下,估计从1 km〜2区域的SGD提供的氮量比向Copano湾的河流输入量多两倍到一个数量级(以DIN形式)。在雨季,SGD等于DIN形式的河流输入。此外,以SGD为基础的周转时间,所有营养素平均<11天,大大少于平均河口冲水时间(即38天)。这项研究的结果表明,通过大量输入和地下与水柱之间的循环过程,尤其是在地表流量较低的情况下,古卵系统中的SGD是河口养分收支的重要组成部分。因此,河口环境(如古河谷边缘和间隙)通过优选增强的SGD溶质通量为牡蛎提供了有利条件,应在牡蛎修复工作中予以考虑。

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