Submarine Groundwater Discharge at a Mega-Tidal Beach

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-11-10 DOI:10.1002/hyp.15319
Raymond D. Craddock, Aaron A. Mohammed, Joseph J. Tamborski, Barret L. Kurylyk
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Abstract

Tidally influenced groundwater systems in coastal environments represent important mixing zones of fresh groundwater and circulating seawater, manifesting as submarine groundwater discharge (SGD). Water circulation induced by tidal pumping enhances the exchange of chemicals between aquifers and coastal waters and thereby influences the biogeochemistry of coastal zones. Here, we report the results of an SGD field study conducted at a steep, mega-tidal sand and gravel beach along the Canadian coast of the Bay of Fundy, a region with the world's highest tides (semi-diurnal tidal ranges exceeding 10 m). Several physical and geochemical measurement techniques were employed to document the spatiotemporal SGD variability. SGD was directly sampled from seepage meters installed over multiple tidal cycles and two summer campaigns. SGD rates were estimated from tracer mass balances for radon (August 2020) and radium isotopes (July 2021) over multiple tidal cycles. Tidally averaged SGD estimates from seepage meters ranged from 12 to 87 cm d−1, with an average of 42 cm d−1, while radon tracing yielded a tidally averaged rate of 86 cm d−1. SGD estimates from radium tracing ranged from 23 to 43 cm d−1 along the shoreline and 6 to 71 cm d−1 offshore, depending on the estimated residence times. Radionuclide analyses of seepage meter waters suggest that the residence time of seawater circulation through the aquifer is less than 1 day. SGD measurements in mega-tidal settings are rare, and the results suggest that the combination of the steep slopes, highly permeable sediments and high tidal range drive very high seepage rates for diffusive SGD. Salinity gradients in the intertidal zone demonstrate that SGD is primarily comprised of circulated seawater with negligible fresh groundwater. Although the freshwater proportion of SGD is relatively low, the large volumetric rates of total SGD can still contribute large amounts of terrestrially derived and remineralized nutrients to coastal waters.

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巨潮海滩的海底地下水排放
沿海环境中受潮汐影响的地下水系统是淡水和循环海水的重要混合区,表现为海底地 下水排放(SGD)。潮汐抽水引起的水循环加强了含水层和沿岸水域之间的化学物质交换,从而影响了沿岸地区的生物地球化学。在此,我们报告了在加拿大芬迪湾沿岸的一个陡峭的大潮汐砂石海滩进行的 SGD 实地研究的结果,该地区是世界上潮汐最高的地区(半昼夜潮差超过 10 米)。为了记录 SGD 的时空变化,采用了多种物理和地球化学测量技术。在多个潮汐周期和两次夏季活动中,通过安装的渗流计直接采集 SGD 样本。在多个潮汐周期内,通过氡(2020 年 8 月)和镭同位素(2021 年 7 月)的示踪质量平衡来估算 SGD 的速率。根据渗流计估算的潮汐平均 SGD 为 12 到 87 cm d-1,平均为 42 cm d-1,而氡示踪得出的潮汐平均 SGD 为 86 cm d-1。根据估计的停留时间,镭追踪得出的 SGD 估计值在沿岸为 23 到 43 cm d-1,离岸为 6 到 71 cm d-1。对渗表水的放射性核素分析表明,海水在含水层中的循环停留时间小于 1 天。在特大潮汐环境中进行的海水渗漏测量非常罕见,测量结果表明,陡坡、高渗透性沉积物和大潮差等因素共同作用,使扩散性海水渗漏的渗漏率非常高。潮间带的盐度梯度表明,SGD 主要由循环海水组成,地下淡水微乎其微。虽然 SGD 中淡水所占比例相对较低,但 SGD 总量的巨大容积率仍能为沿岸水域提供大量的陆源营养盐和再矿化营养盐。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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