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首页> 外文期刊>Journal of Hydrology: Regional Studies >Observations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii
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Observations of nearshore groundwater discharge: Kahekili Beach Park submarine springs, Maui, Hawaii

机译:近岸地下水排放观测:夏威夷毛伊岛的Kahekili海滩公园海底温泉

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Study region The study region encompasses the nearshore, coastal waters off west Maui, Hawaii. Here abundant groundwater—that carries with it a strong land-based fingerprint—discharges into the coastal waters and over a coral reef. Study focus Coastal groundwater discharge is a ubiquitous hydrologic feature that has been shown to impact nearshore ecosystems and material budgets. A unique combined geochemical tracer and oceanographic time-series study addressed rates and oceanic forcings of submarine groundwater discharge at a submarine spring site off west Maui, Hawaii. New hydrological insights for the region Estimates of submarine groundwater discharge were derived for a primary vent site and surrounding coastal waters off west Maui, Hawaii using an excess 222 Rn ( t 1/2 = 3.8 d) mass balance model. Such estimates were complemented with a novel thoron ( 220 Rn, t 1/2 = 56 s) groundwater discharge tracer application, as well as oceanographic time series and thermal infrared imagery analyses. In combination, this suite of techniques provides new insight into the connectivity of the coastal aquifer with the near-shore ocean and examines the physical drivers of submarine groundwater discharge. Lastly, submarine groundwater discharge derived constituent concentrations were tabulated and compared to surrounding seawater concentrations. Such work has implications for the management of coastal aquifers and downstream nearshore ecosystems that respond to sustained constituent loadings via this submarine route.
机译:研究区域研究区域包括夏威夷毛伊岛西部的近岸沿海水域。在这里,丰富的地下水(带有很强的陆上指纹)排入沿海水域和珊瑚礁。研究重点沿海地下水排放是普遍存在的水文特征,已显示出会影响近岸生态系统和物质预算。一项独特的地球化学示踪剂和海洋学时序研究相结合的研究解决了夏威夷毛伊岛西部海底春季站点的海底地下水排放速率和海洋强迫。该地区的新水文见解使用过量的222 Rn(t 1/2 = 3.8 d)质量平衡模型,得出了夏威夷毛伊岛西部主要海底排放场地和周围沿海水域的海底地下水排放量估算值。此类估算得到了新的(220 Rn,t 1/2 = 56 s)地下水排放示踪剂的应用,以及海洋学时间序列和热红外图像分析的补充。结合起来,这套技术可以为沿海含水层与近岸海洋之间的连通性提供新的见解,并研究海底地下水排放的物理驱动因素。最后,将海底地下水排放产生的成分浓度制成表格,并与周围的海水浓度进行比较。这项工作对沿海水层和下游近海生态系统的管理产生了影响,这些管理系统通过这种海底路线应对持续的组成负荷。

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