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伊朗马哈尔卢湖沿海含水层中地下水的地球化学与金属(类金属)行为

Geochemistry of groundwater and metal(loid) behavior in the costal aquifers of the Maharlu Lake, Iran.

作者信息

Khosravi Roghayeh, Zarei Mehdi, Sracek Ondra, Bigalke Moritz

机构信息

Department of Earth Sciences, Faculty of Sciences, Shiraz University, Adabiat Square, Shiraz, Iran.

Department of Geology, Faculty of Science, Palacky University, Olomouc, Czech Republic.

出版信息

Environ Sci Pollut Res Int. 2022 Oct;29(49):74861-74876. doi: 10.1007/s11356-022-21124-x. Epub 2022 Jun 1.

Abstract

Groundwater in coastal aquifers of the Maharlu Lake, southern Iran, has suffered from quality degradation and salinity increases in recent decades. These aquifers are important sources for drinking and agricultural uses in area around the lake. Hydrogeochemical analyses were carried out to identify the geochemical processes controlling groundwater chemistry and heavy metal concentrations in the coastal aquifer of the Maharlu Salt Lake. A total number of 54 water samples (45 samples from three coastal aquifers and 9 water samples from lake water) were collected for laboratory analysis of major ions and heavy metals three times from November-2014 to July-2015. In addition, physiochemical parameters of temperature, electrical conductivity, pH, and redox potential were measured in the field. The findings indicate three major controls of groundwater chemistry in the coastal aquifers of the Maharlu Lake including (1) lake water intrusions, (2) evaporites and carbonate dissolution-precipitation, and (3) input of organic matter probably linked to the seepage of domestic sewage with resulting sulfate reduction. In contrast, dissolution of minerals in surface sediments and direct evaporation of groundwater in the coastal aquifers seem to be insignificant based on geochemical ratios and water table depth. Concentrations of B, Li, Co, Cr, Cu, Ni, and U increase, but Zn concentrations decrease in groundwater due to the lake water intrusions into the costal aquifers. Gypsum dissolution and consequent carbonate reactions cause B, Co, Cr, Cu, Ni, Zn, and U enrichment in the groundwater samples. These findings can provide water managers and local authorities with a comprehensive framework of the coastal groundwater geochemistry, allowing a better understanding of the effects of current management practices and the implementation of mitigation approaches such as reduction of groundwater extraction to limit further lake saltwater intrusion and water resources deterioration.

摘要

近几十年来,伊朗南部马哈尔卢湖沿海含水层的地下水质量下降,盐度增加。这些含水层是该湖周边地区重要的饮用水和农业用水来源。开展了水文地球化学分析,以确定控制马哈尔卢盐湖沿海含水层地下水化学和重金属浓度的地球化学过程。从2014年11月至2015年7月,共采集了54个水样(来自三个沿海含水层的45个样品和湖水的9个水样),用于实验室分析主要离子和重金属。此外,还在现场测量了温度、电导率、pH值和氧化还原电位等理化参数。研究结果表明,马哈尔卢湖沿海含水层地下水化学受三个主要因素控制,包括:(1)湖水入侵;(2)蒸发岩和碳酸盐的溶解-沉淀;(3)可能与生活污水渗漏相关的有机物输入,导致硫酸盐还原。相比之下,根据地球化学比值和地下水位深度,地表沉积物中矿物的溶解和沿海含水层中地下水的直接蒸发似乎并不显著。由于湖水入侵沿海含水层,地下水中硼、锂、钴、铬、铜、镍和铀的浓度增加,但锌的浓度降低。石膏溶解以及随之发生的碳酸盐反应导致地下水样品中硼、钴、铬、铜、镍、锌和铀富集。这些研究结果可为水资源管理者和地方当局提供沿海地下水地球化学的综合框架,有助于更好地理解当前管理措施的影响,并实施缓解措施,如减少地下水开采,以限制湖水咸水进一步入侵和水资源恶化。

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