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利用地下水主要成分(Sr 和 B 同位素)评估高度人为影响下干旱海岸含水层中的海水入侵。

Assessing seawater intrusion in an arid coastal aquifer under high anthropogenic influence using major constituents, Sr and B isotopes in groundwater.

机构信息

Centro del Agua para América Latina y el Caribe, Tecnológico de Monterrey, Mexico.

Centro del Agua para América Latina y el Caribe, Tecnológico de Monterrey, Mexico.

出版信息

Sci Total Environ. 2017 Jun 1;587-588:282-295. doi: 10.1016/j.scitotenv.2017.02.137. Epub 2017 Feb 24.

Abstract

The La Paz aquifer system (Baja California Sur, Mexico) is under severe anthropogenic pressure because of high groundwater abstraction for urban supply (city of La Paz, around 222,000 inhabitants) and irrigated agriculture (1900ha). In consequence, seawater has infiltrated the aquifer, forcing the abandonment of wells with increased salinity. The objective of this study was to assess seawater intrusion, understand the hydrogeochemical processes involved and estimate the contribution of seawater in the wells tested. The aquifer comprises mainly the alluvial filling and marine sediments of a tectonic graben oriented north-south, in contact with the Gulf of California. Groundwater samples were collected in 47 locations and analyzed for major constituents. A subset of 23 samples was analyzed for strontium and boron concentrations and isotopic signatures (Sr/Sr and δB). Results were interpreted using standard hydrochemical plots along with ad hoc plots including isotopic data. Seawater intrusion was confirmed by several hydrogeochemical indicators, such as the high salinity in areas of intense pumping or the Na-Ca exchange occurring in sediments that were previously in chemical equilibrium with fresh water. However, seawater contribution was not sufficient to explain the observed concentrations and isotopic signatures of Sr and B. According to the isotopic data, desorption processes triggered by a modification in chemical equilibrium and an increase in ionic strength by seawater intrusion significantly increased Sr and probably B concentrations in groundwater. From a calculation of seawater contribution to the wells, it was estimated that one-third of the sampled abstraction wells were significantly affected by seawater intrusion, reaching concentrations that would limit their use for human supply or even irrigated agriculture. In addition, significant agricultural pollution (nitrates) was detected. Planned management of the aquifer and corrective measures are needed in order to invert the salinization process before it severely affects water resources in the long term.

摘要

拉巴斯含水层系统(墨西哥下加利福尼亚州南部)由于城市供水(拉巴斯市,约 222000 名居民)和灌溉农业(1900 公顷)的大量地下水抽取,正承受着严重的人为压力。因此,海水已经渗透到含水层中,迫使盐分增加的水井被迫废弃。本研究的目的是评估海水入侵,了解所涉及的水文地球化学过程,并估计测试井中海水的贡献。含水层主要由构造地堑的冲积填充物和海洋沉积物组成,呈南北向延伸,与加利福尼亚湾接壤。在 47 个地点采集了地下水样本并进行了主要成分分析。选择了 23 个样本子集进行锶和硼浓度及同位素特征(Sr/Sr 和 δB)分析。使用标准水文地球化学图以及包括同位素数据的特定图来解释结果。通过多种水文地球化学指标证实了海水入侵,例如在强烈抽水区域的高盐度,或在先前与淡水处于化学平衡的沉积物中发生的 Na-Ca 交换。然而,海水的贡献不足以解释观察到的 Sr 和 B 的浓度和同位素特征。根据同位素数据,化学平衡的改变和海水入侵导致的离子强度增加触发的解吸过程,显著增加了地下水 Sr 和可能还有 B 的浓度。从对井中海水贡献的计算来看,估计有三分之一的抽样抽取水井受到海水入侵的严重影响,其浓度达到限制其用于人类供应甚至灌溉农业的程度。此外,还检测到了大量农业污染(硝酸盐)。需要对含水层进行计划管理和采取纠正措施,以便在长期内严重影响水资源之前,扭转盐化过程。

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