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伊朗伊斯法罕北部的水文地球化学研究与地下水质量评估。

Hydrogeochemistry study and groundwater quality assessment in the north of Isfahan, Iran.

机构信息

Department of Mining and Metallurgy Engineering, Amirkabir University of Technology, Tehran, Iran.

出版信息

Environ Geochem Health. 2018 Apr;40(2):583-608. doi: 10.1007/s10653-017-0003-x. Epub 2017 Jun 29.

Abstract

This study presents the groundwater quality assessment in the north of Isfahan, Iran. In the study area, assessment and measurement of groundwater hydrochemical parameters such as pH, total dissolved solids (TDS), electrical conductivity (EC), sodium absorption ratio (SAR), total hardness, major cations (K, Na, Ca and Mg) and major anions (Cl, [Formula: see text] and [Formula: see text]) concentrations were performed. Accordingly, the 66 water samples from different locations were collected during April and May 2015. Water samples collected in the field were analyzed in the laboratory for cations and anions using the standard methods. In this research, the analytical results of physiochemical parameters of groundwater were compared with the standard guideline values as recommended by the world health organization (WHO) for drinking and public health purposes. The pH values of groundwater samples varied from 7.05 to 8.95 with a mean of 7.78, indicating a neutral to slightly alkaline water. TDS values showed that 14% of the samples exceeds the desirable limit given by WHO. EC values varied from 213 to 4320 µS/cm, while 23% of the samples were more than the standard limit. Gibbs diagram had shown that 90% of the samples in the study area fall in the rock weathering zone, and this means that chemical weathering of rock-forming minerals is the main factor controlling the water chemistry in the study area. Irrigation suitability and risk assessment of groundwater are evaluated by measuring EC, %Na, SAR and RSC. According to the dominant cations and anions, five types of water were identified in the water samples: Ca-HCO, Ca-SO, Na-Cl, Na-HCO and Na-SO. The results show that the majority of samples (30 samples, 45%) belongs to the mixed Na-SO water type. Correlation analysis and principal component analysis was used to identify the relationship between ions and physicochemical parameters. Results indicated that 18 stations of the study area had the best quality and can be used for irrigation and drinking purposes in the future.

摘要

本研究对伊朗伊斯法罕北部的地下水质量进行了评估。在研究区域,对地下水水化学参数如 pH 值、总溶解固体(TDS)、电导率(EC)、钠吸收比(SAR)、总硬度、主要阳离子(K、Na、Ca 和 Mg)和主要阴离子(Cl、[Formula: see text] 和 [Formula: see text])浓度进行了评估和测量。相应地,在 2015 年 4 月和 5 月期间,从不同地点采集了 66 个水样。现场采集的水样在实验室中使用标准方法对阳离子和阴离子进行分析。在本研究中,将地下水理化参数的分析结果与世界卫生组织(WHO)推荐的饮用水和公共卫生标准指导值进行了比较。地下水样品的 pH 值范围为 7.05 至 8.95,平均值为 7.78,表明水呈中性至弱碱性。TDS 值显示,有 14%的样品超过了 WHO 给出的理想限值。EC 值变化范围为 213 至 4320 µS/cm,而有 23%的样品超过了标准限值。Gibbs 图表明,研究区域 90%的样品位于岩石风化带,这意味着岩石成矿物质的化学风化是控制研究区域水化学的主要因素。通过测量 EC、%Na、SAR 和 RSC,对地下水的灌溉适用性和风险进行了评估。根据主要阳离子和阴离子,在水样中确定了五种水类型:Ca-HCO、Ca-SO、Na-Cl、Na-HCO 和 Na-SO。结果表明,大多数样品(30 个样品,占 45%)属于混合 Na-SO 水类型。相关分析和主成分分析用于确定离子与理化参数之间的关系。结果表明,研究区域的 18 个站点水质最好,未来可用于灌溉和饮用水。

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