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伊朗地下水资源盐度评估的全面回顾

A comprehensive review of the salinity assessment in groundwater resources of Iran

作者:Seyyed Mohammad Shoaei,

发表时间:2024年

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摘要

本研究的主要目的是利用评估伊朗地下水资源盐度的 116 篇论文提出一个综合态度。全国不同地区地下水水质状况。本研究主要对理化参数值进行测量,其中电导率(EC)作为地下水盐度测定的基本参数,通过与标准进行比较,并采用Wilcox图,得出分别评估饮用水和农业用水的质量。前期文献研究表明,仅西部和西北地区地下水水质适宜饮用,大部分省份EC值均超过推荐限值。中部省份EC浓度最高,导致地下水水质恶化,盐分比例最大,水质不适合饮用。此外,使用威尔科克斯图对灌溉用地下水质量进行的评估显示,研究区域大部分地区的盐度都很高或非常高。西北省份C3-S1级水平相对最低,中部地区C4-S4级水平最高。降雨不足、地下水开采率高、盐湖咸水入侵是研究区中部地区地下水水质恶化的主要原因。


Abstract

The main purpose of the present research is to propose a comprehensive attitude of the salinity in groundwater resources of Iran using 116 papers in the assessment of groundwater quality in different areas of the country. The conducted study contains the measurement of the values of physicochemical parameters of which electrical conductivity (EC), as the fundamental parameter for salinity determination of groundwater, was considered mostly, and by comparing it with standards, as well as employing the Wilcox diagram, the quality of water was assessed for drinking and agricultural purposes, respectively. Study of the previous papers revealed that in only the west and northwest of the country, the groundwater quality was suitable for drinking, and in the majority of provinces, EC values exceeded the recommended limits. The highest EC level was seen in central provinces which led to the aggravation of groundwater and the largest proportion of salinity, putting the quality of water in an unsuitable class for drinking. Additionally, the assessment of groundwater quality for irrigation uses using the Wilcox diagram showed high and very high salinity rates in most areas of the study area. Northwestern provinces relatively had the lowest level putting in C3–S1 class, while central areas reached the highest with C4–S4 classification. Deficiency of rainfall, high rate of groundwater exploitation, and the intrusion of saltwater from Salt Lake were the principal reasons for groundwater deterioration in central parts of the study area.