Seasonal Assessment of Water Quality by Statistical Analysis in the Coastal Area of Sindh, Pakistan

M. Nasir, H. Abbasi, A. Zubair, W. Ahmad
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引用次数: 1

Abstract

Monitoring of groundwater is very important because of climatic and demographic patterns along the coastline of Sindh Province, Pakistan. Seventy representative groundwater samples were collected during pre-monsoon and post-monsoon seasons for the investigation of physico-chemical variables to understand the groundwater chemistry of the coastal belt. Multivariate statistical techniques were applied to interpret the data to reveal the pollution sources in the groundwater samples. The normalized charge balance index (NCBI) was computed on the data set and the STzand STz+ were analyzed in the collected groundwater samples. Cations were in excess and alkalinity in the aquifer of the study area was balanced by Ca+ + Mg+ ions. The contribution of ions was insignificant for charge balance. Mg+2 and Ca+2 were in huge concentration and alkaline hardness was maintained by the alkaline rocks formation. Majority of the charge was balanced by SO4 -2 and Cl. In groundwater ionic composition is used to categorize it into ionic types of groundwater based on the dissolved cation and anion. The ionic reaction is likely regulated by domestic geological formation. The sample location illustrates Na–SO4 -2 and Na+–Cl nature of groundwater. The groundwater with Na–SO4 and Na+–Cldominancy generally shows saline characteristics that make groundwater unfit to use for irrigation and drinking purposes.
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巴基斯坦信德省沿海地区水质的季节性统计分析
由于巴基斯坦信德省沿海地区的气候和人口模式,监测地下水非常重要。在季风前和季风后采集了70个具有代表性的地下水样本,进行了理化变量调查,以了解海岸带地下水的化学性质。应用多元统计技术对数据进行解释,揭示地下水污染来源。计算了该数据集的归一化电荷平衡指数(NCBI),并对所采集的地下水样品进行了STzand STz+分析。研究区含水层阳离子过剩,碱度由ca2 + + Mg+离子平衡。离子对电荷平衡的贡献不显著。Mg+2和Ca+2浓度高,碱性岩石形成维持了碱性硬度。大部分电荷被SO4 -2和Cl平衡。在地下水中,离子组成是根据溶解的阳离子和阴离子来划分地下水的离子类型。离子反应可能受国内地质构造的调控。样品位置说明了地下水的Na - SO4 -2和Na+ - Cl性质。Na - SO4和Na+ -为主的地下水一般表现为含盐特征,不适合灌溉和饮用。
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