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Deterioration of coastal groundwater quality in Island and mainland regions of Ramanathapuram District, Southern India
Authors:Venkataramann Sivasankar  Thiagarajan Ramachandramoorthy  A Chandramohan
Institution:1. Department of Chemistry, Thiagarajar College of Engineering (Autonomous), Madurai, 625 015, Tamil Nadu, India
2. PG & Research Department of Chemistry, Bishop Heber College (Autonomous), Tiruchirappalli, 620 017, Tamil Nadu, India
3. PG & Department of Environmental Sciences, Bishop Heber College (Autonomous), Tiruchirappalli, 620 017, Tamil Nadu, India
Abstract:A study was carried out in the Island and mainland regions of Ramanathapuram District to characterize the physico-chemical characteristics of 87 groundwater samples in Island and 112 groundwater samples in mainland which include pH, EC, TDS, salinity, total alkalinity, calcium hardness, magnesium hardness, total hardness, chloride and fluoride. Heavy inorganic load in majority of the groundwater samples has been estimated due to the salinity, TDS, TH and chloride beyond the threshold level which substantiates the percolation of sea water into the freshwater confined zones. Although the groundwater sources are available in plenty, the scarcity of potable water is most prevalent in this coastal area. The Water Quality Index (WQI) and Langeleir Saturation Index (LSI) have also been calculated to know the potable and corrosive/incrusting nature of the water samples. The statistical tools such as principal component analysis, box plots and correlation matrix have also been used to explain the influence of different physico-chemical parameters with respect to one another among the groundwater samples. The percentage of groundwater samples in mainland was more than that in Island with respect to the acceptable limit of WHO drinking standard, especially in TDS, CH, TH and chloride but the converse is observed in the case of fluoride. About 8 % of the mainland aquifers and 42 % of Island aquifers were identified to have fluoride greater than 1.5 mg/l. The signature of salt-water intrusion is observed from the ratio of Cl/CO 3 2? ?+?HCO3 and TA/TH. A proper management plan to cater potable water to the immediate needs of the people is to be envisaged.
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