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Assessment of Water Quality of a Tropical River with Special Reference to Ions

机译:评估热带河水的水质及特殊参考离子

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The role of ions in a tropical river water (Neyyar, Kerala) was assessed. Rock weathering is the dominating mechanism controlling the major ion chemistry of Neyyar river. The dominance of Cl-HCO_(3)-Na during monsoon indicates that geology plays a major role in controlling water chemistry. The presence of mineral varieties of quartz, feldspars, pyroxene, biotite, etc., in the Pre-Cambrian crystalline namely Khondalite and Charnockites, could be the source of major ions. The major ion chemistry of Neyyar river waters show that Na is the dominant cation with lower proportions of Mg and Ca, with HCO_(3) and Cl as the dominant anions. It belongs to the HCO_(3) group with significant amounts of Na and Cacations. The dominance of Cl-HCO_(3)-Ca and Ca-HCO_(3)-Cl during post monsoon and pre monsoon respectively indicates that besides geology, the land drainage and anthropogenic activities also control river water. The change in water type observed during monsoon from Na-Cl-HCO_(3) to Na-Ca-Cl-HCO_(3) almost from the middle portion may be attributed to anthropogenic pollution. Hence attention is to be paid to take the control measures to prevent the pollution in this stretch of the river.
机译:离子在热带河水中的作用(Neyyar,Kerala)进行了评估。岩石风化是控制Neyyar河主要离子化学的主导机制。季风期间Cl-HCO_(3)-NA的优势表明地质在控制水化学方面发挥着重要作用。在寒武纪晶体中,在寒武纪结晶中,矿物品种的石英,长石,辉石,生物烟灰等的存在可能是主要离子的来源。 Neyyar River Waters的主要离子化学表明,NA是较低比例的Mg和Ca,HCO_(3)和CL作为主要阴离子的主导阳离子。它属于HCO_(3)组,具有大量NA和消耗。在季风和前季风期间Cl-HCO_(3)-CA和CA-HCO_(3)-CL的优势分别表明除了地质,土地排水和人为的活动也控制河水。从中间部分的Na-Cl-HCO_(3)到Na-Ca-Cl-HCO_(3)中观察到的水类型的变化可能归因于人为污染。因此,要注意采取控制措施,以防止在这段河流中的污染。

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