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Hydrochemical Characteristics and Quality Assessment of Groundwater in Patuakhali District, Southern Coastal Region of Bangladesh

机译:孟加拉国南部地区Patuakhali区地下水的水化特征及质量评价

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Groundwater quality is important as it is the main factor determining its suitability for drinking, domestic, agricultural, and industrial purposes. Hydrogeochemical characteristics of groundwater in coastal aquifers of Patuakhali district have been investigated based on different indices for assessing its utility and to evaluate the factors influencing groundwater quality. A total of 18 groundwater samples were collected from tube wells having depth between 244 and 365 m and were analyzed for physicochemical parameters, including temperature, pH, electric conductivity (EC), total dissolved solids (TDS), salinity; major ion concentrations such as Na~+, K~+, Ca~(2+),Mg~(2+), Cl~-, SO_4~(2-), NO_3~-, HCO_3~-, Br~-; and trace element concentrations such as As, Pb, Li, Rb, Ba, Be, Co, Mn, Ti, Cd, and Se. The results revealed that the groundwater is slightly alkaline and brackish in nature. The trends of dominant cations and anions are Na~+>Ca~(2+)>Mg~(2+)>K~+ and HCO_3~->Cl~->SO_4~(2-)>NO_3~->Br~-,respectively and Na-Cl-HCO_3 is the dominant groundwater type. Ion exchange and seawater plays a significant role in the geochemistry of the groundwater and signatures of Br~-/Cl~- ratio showed evidence of mixing of seawater in the southern part of study area. The samples analyzed were also classified with different indices, diagram, and permissible limit i.e., EC, TDS, chloride content, soluble sodium percentage or Na %, sodium adsorption ratio, residual sodium carbonate, magnesium adsorption ratio, Kelley's ratio, Wilcox diagram, USSL diagram and results showed that groundwater is not suitable for drinking and irrigation purpose. However, except for Se and As, the trace metals concentration are within permissible limit.
机译:地下水质量很重要,因为它是确定其适用性,国内,农业和工业用途的主要因素。基于不同索引的沿海含水区地下水的水水电站特征进行了调查,以评估其实用性,评价影响地下水质量的因素。从244至365μm的管孔中收集了总共18个地下水样品,并分析了物理化学参数,包括温度,pH,电导率(EC),总溶解固体(TDS),盐度;主要离子浓度,如Na〜+,K〜+,Ca〜(2 +),mg〜(2+),Cl〜 - ,SO_4〜(2-),NO_3〜 - ,HCO_3〜 - ,BR〜 - ;和痕量元素浓度,例如Pb,Li,Rb,Ba,Be,Co,Mn,Ti,Cd和Se。结果表明,地下水在自然界中略微碱性和咸。主导阳离子和阴离子的趋势是Na〜+> Ca〜(2 +)> mg〜(2 +)> K〜+和HCO_3〜 - > CL〜 - > SO_4〜(2 - )> NO_3〜 - > BR 〜 - 分别和NA-CL-HCO_3是主要的地下水型。离子交换和海水在地球化学中发挥着重要作用,BR〜 - / CL〜比率的签名显示出南部的研究区海水混合的证据。分析的样品还分为不同的索引,图和允许的极限,即EC,TDS,氯化物含量,可溶性钠百分比或Na%,吸附率,残留碳酸钠,镁吸附率,Kelley的比例,Wilcox图,USSL图表和结果表明,地下水不适合饮用和灌溉用途。然而,除了SE和AS的外,痕量金属浓度在允许的极限范围内。

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