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估算拉普拉塔河口中部滨海平原的淡水透镜体储量(阿根廷)。

Estimating the freshwater-lens reserve in the coastal plain of the middle Río de la Plata Estuary (Argentina).

机构信息

Centro de Investigaciones Geológicas (CIG). Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET-UNLP), diagonal 113 N°275, B1904DPK La Plata, Argentina.

Institute of Marine Sciences, National Research Council, Arsenale Tesa 104, Castello 2737/F, 30122 Venezia, Italy.

出版信息

Sci Total Environ. 2018 Jul 15;630:357-366. doi: 10.1016/j.scitotenv.2018.02.236. Epub 2018 Feb 23.

Abstract

Drinking-water supply is one of the main issues that populations face in many coastlands. Shallow coastal aquifers are often characterized by the presence of lens-shaped freshwater floating on the saline groundwater plume of marine origin. These groundwater lenses are commonly associated with landforms, such as littoral ridges and dunes and in many cases they represent the main source of water supply in remote coastal areas. At the right side of the middle Río de la Plata estuary (Argentina) the aquifer system is generally saline. Elongated and thin sandy beach ridge systems emerging from the general flat morphology of the marsh-flood plain are capable of storing precipitations forming freshwater lenses, which to date are the main freshwater supply for inhabitants. The aim of this study is to identify and delimitate the presence of such valuable freshwater reserves in order to provide the first necessary guidelines for the water management plan in this area, which has never been implemented since, to the Authors' knowledge, no specific investigation had been carried out before this study. To achieve this goal, Vertical Electrical Sounding, groundwater electrical conductivity measurements, water balances and groundwater chemical analyses were performed and interpreted together. The whole dataset was processed to define the electro-stratigraphic model of the study area and to produce the map of the electrical conductivity of the shallow aquifer. In addition, a three-dimensional model of the fresh water reservoir has been implemented for a better understanding of the relationship between geomorphology and groundwater. Results point out that a total freshwater volume of 78,259,700m is stored into a continuous lens and the annual average recharge from precipitation amounts to 6,303,500m. Although preliminary, this work provides the basic knowledge on the potential fresh groundwater lenses and provides important information for addressing a sustainable use of the freshwater resource.

摘要

饮用水供应是许多沿海地区居民面临的主要问题之一。浅沿海含水层的特点通常是存在透镜状的淡水浮在海洋起源的咸地下水羽流上。这些地下水透镜通常与地貌有关,例如滨岸脊和沙丘,在许多情况下,它们代表了偏远沿海地区的主要供水源。在拉普拉塔河口(阿根廷)的中间右侧,含水层系统通常是咸的。从沼泽泛滥平原的一般平坦形态中出现的细长而薄的砂质海滩脊系统能够储存形成淡水透镜的降水,迄今为止,这些淡水透镜是居民的主要淡水供应源。本研究的目的是识别和划定这些有价值的淡水储量的存在,以便为该地区的水资源管理计划提供第一批必要的指导方针,据作者所知,由于在此之前从未实施过具体的调查,因此该地区从未实施过水资源管理计划。为了实现这一目标,进行了垂直电测深、地下水电导率测量、水量平衡和地下水化学分析,并一起进行了解释。整个数据集经过处理,以确定研究区的电地层模型,并生成浅层含水层电导率图。此外,还实施了一个三维淡水水库模型,以便更好地理解地貌和地下水之间的关系。结果表明,总共储存了 7825.97 万立方米的淡水,形成了一个连续的透镜,年平均降水补给量为 630.35 万立方米。尽管这是初步的,但这项工作提供了有关潜在淡水透镜的基本知识,并为解决淡水资源的可持续利用提供了重要信息。

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