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Submarine groundwater discharge in the Southeast and Gulf Coast regions of the United States.

机译:美国东南部和墨西哥湾沿岸地区的海底地下水排放。

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Submarine groundwater discharge (SGD) potentially transports significant volumes of water and dissolved geochemical constituents to continental shelf environments. SGD is variable from region to region, and is a function of local hydrogeological characteristics and anthropogenic influences. This work examines SGD at two locations in the Gulf Coast and Southeast regions (Louisiana continental shelf near the Mississippi Delta, and Onslow Bay, NC), and suggests a regional management plan for SGD.; Quantification of SGD on the continental shelf of Louisiana and in Onslow Bay was accomplished using 222Rn, a natural geochemical tracer. A box model approach was employed to quantify sources and sinks of 222Rn, which include: in situ production and decay, horizontal transport into and out of the box model, vertical evasion (across pycnocline or air-sea interface), and benthic advective-diffusive exchange. All sources and sinks were quantified except the benthic advective-diffusive exchange, which was determined by difference. SGD estimates on the Louisiana continental shelf were on the order of 0.01--0.14 cm d-1, which is equivalent to 1% the average discharge of the Mississippi River over the entire study area. Sources of SGD in the study area were primarily from production water, a product of the oil and gas extraction process, and seawater recirculation cells.; SGD estimates in Onslow Bay averaged approximately 0.1 cm d-1 at the regional scale, and estimates decreased from nearshore to offshore in three shore parallel models. Fresh groundwater discharge dominates in the nearshore region while tidal pumping provides most SGD farther offshore. Volumetrically, SGD over the entire study area is approximately 105% the average discharge of the Cape Fear River, the largest river near the study area that discharges directly to the continental shelf. The hydrogeology of Onslow Bay is similar to that of coastal South Carolina and Georgia. Assuming SGD rates are similar throughout in the region, SGD contributes 6--12% that of riverine discharge in the first 15 km offshore between Cape Lookout, NC and the FL/GA border.; Considering the importance of groundwater as a drinking water source and the potential influences of SGD on continental shelf environments, a regional plan is suggested, that is designed to manage groundwater resources in coastal zones. The management plan consists of increased assessment and monitoring of coastal aquifers, and a regional coastal groundwater resources oversight committee. The oversight committee would act as a central organization to collect and disperse groundwater information throughout the region, and mitigate and resolve local and state groundwater issues.
机译:海底地下水排放(SGD)可能将大量的水和溶解的地球化学成分输送到大陆架环境。 SGD在不同地区之间是可变的,并且是当地水文地质特征和人为影响的函数。这项工作研究了墨西哥湾沿岸和东南部地区(密西西比三角洲附近的路易斯安那州大陆架和北卡罗来纳州的昂斯洛湾)的两个地方的SGD,并提出了SGD的区域管理计划。使用天然地球化学示踪剂222Rn对路易斯安那州大陆架和Onslow湾的SGD进行定量。采用盒模型方法对222Rn的源和汇进行定量,其中包括:原位生产和衰减,盒模型的水平进出运输,垂直回避(穿越多克隆线或海气界面)以及底栖对流扩散交换。除底栖对流-扩散交换外,所有源和汇都被量化,这是由差异决定的。路易斯安那州大陆架的SGD估算约为0.01--0.14 cm d-1,相当于整个研究区域密西西比河平均排放量的<1%。研究区的SGD来源主要来自采出水,石油和天然气提取过程的产物以及海水再循环池。在区域尺度上,昂斯洛湾的SGD估算值平均约为0.1 cm d-1,在三个岸上平行模型中,估算值从近岸向近海递减。在近岸地区,新鲜的地下水排放占主导地位,而潮汐抽水在离岸较远的地方提供了大多数SGD。在体积上,整个研究区域的SGD约为Cape Fear河的平均流量的105%,Cape Fear河是研究区域附近最大的河流,直接排放到大陆架。昂斯洛湾的水文地质学与南卡罗来纳州沿海地区和佐治亚州相似。假设整个地区的SGD费率相似,SGD贡献了北卡罗来纳州Cape Lookout和FL / GA边界之间近15公里内河道排放量的6--12%。考虑到地下水作为饮用水源的重要性以及SGD对大陆架环境的潜在影响,建议制定一个区域计划,该计划旨在管理沿海地区的地下水资源。管理计划包括增加对沿海含水层的评估和监测,以及一个区域沿海地下水资源监督委员会。监督委员会将作为一个中央组织,在整个地区收集和散布地下水信息,并减轻和解决当地和州的地下水问题。

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