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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Sea-water/groundwater interactions along a small catchment of the European Atlantic coast
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Sea-water/groundwater interactions along a small catchment of the European Atlantic coast

机译:欧洲大西洋沿岸小流域的海水/地下水相互作用

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摘要

The geochemistry and isotopic composition of a karstic coastal aquifer in western Ireland has shed light on the effect of sea-water/groundwater interactions on the water quality of Ireland's Atlantic coastal zone. The use of stable isotope data from the IAEA precipitation station in Valentia, located in SW Ireland has facilitated the characterization of groundwater recharge conditions in the western part of Ireland and suggests that groundwater is mostly replenished by the isotopically light winter precipitation. The dissolved SO42- in the karstic groundwater that was collected during baseflow conditions with δ ~(34)S values between 4.6‰ and 18‰ may be composed of S stemming from three principal sources: SO42- derived from precipitation which is composed of both sea-spray S (δ ~(34)S: 20‰) and an isotopically light anthropogenic source (δ ~(34)S: 1-5‰), SO42-stemming from animal slurries (δ ~(34)S: ~5‰), and intruding sea-water SO42- (δ ~(34)S: 20.2‰). The isotopic composition of δ ~(18)O in dissolved groundwater SO42- collected during baseflow conditions is interpreted as reflecting sea-water intrusion to the karstic coastal groundwater system. The highest δ ~(18)O values in dissolved groundwater SO42- were in samples collected near the coast (4.8±0.4‰) and the lowest (2±0.5‰) were collected further inland. The δ ~(15)N and δ ~(18)O values of groundwater NO3- were between 3.4‰ and 11.4‰ and approximately 7.7‰, respectively, and reflect geochemical conditions in the aquifer that do not promote attenuation of NO3- through denitrification. As a result N loading to Kinvara Bay that is controlled by submarine groundwater discharge (SGD) was calculated as 5tons/day on average compared to an estimated N-input that derives from precipitation of approximately 2.5tons/a. SGD into the bay may result in near coastal sea-water quality changes. These results represent one of the first studies addressing the effect of groundwater quality in Ireland on the European Atlantic coastal zone.
机译:爱尔兰西部岩溶海岸带含水层的地球化学和同位素组成揭示了海水/地下水相互作用对爱尔兰大西洋沿岸带水质的影响。利用位于爱尔兰西南部的瓦伦西亚国际原子能机构降水站的稳定同位素数据,有助于表征爱尔兰西部地区的地下水补给条件,并表明大部分同位素是由冬季的轻度降水补充的。 δ〜(34)S值为4.6‰至18‰的基流条件下在岩溶地下水中溶解的SO42-可能由源自以下三个主要来源的S组成:SO42-来源于降水,由两个海组成-喷洒S(δ〜(34)S:〜20‰)和同位素轻的人为来源(δ〜(34)S:1-5‰),从动物粪便中提取SO42(δ〜(34)S:〜5 ‰),并侵入海水SO42-(δ〜(34)S:20.2‰)。在基流条件下收集的溶解的地下水SO42-中的δ〜(18)O同位素组成被解释为反映了海水对岩溶沿海地下水系统的入侵。溶解的地下水SO42-中的最高δ〜(18)O值是在附近海岸采集的样品中(4.8±0.4‰),而最低的(2±0.5‰)则是在内陆采集的。地下水NO3-的δ〜(15)N和δ〜(18)O值分别在3.4‰和11.4‰之间以及大约7.7‰,反映了含水层中的地球化学条件,这些条件不会促进反硝化作用对NO3-的衰减。 。结果,与从大约2.5吨/年的降水量得出的估计氮输入量相比,受海底地下水排放(SGD)控制的金瓦拉湾的N负荷平均计算为5吨/天。 SGD进入海湾可能会导致近海岸海水水质变化。这些结果代表了针对爱尔兰地下水质量对欧洲大西洋沿岸地区的影响的首批研究之一。

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