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Spatial and temporal variations of Groundwater quality of phreatic aquifers in Central Kerala River Basin, India

机译:印度喀拉拉河流域中部潜水层地下水水质的时空变化

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The paper f ocusses on spatial and temporal distribution of pH, electrical conductivity (EC), total hardness, total iron and fluoride content of groundwater samples collected from phreatic aquifers of Bharathapuzha river basin, Kerala, India. The spatial and temporal distribution of non ionic substances like pH, EC & total hardness are within the permissible limit of Bureau of Indian Standards (BIS) and World Health Organization (WHOfstandards. Total iron concentration during both the seasons revealsthat majority of the area falls within the 0.3mg/L to 1 mg/L category which is of desirable limit of BIS. In the Bharathapuzha river basin the fluoride content of groundwater during pre monsoon ranges from 0.01 mg/L to 1.2 mg/L, whereas in post monsoonit varies from O.Olmg/L to 1.45 mg/L. The geological characteristics of the region plays a vital role in increased fluoride content at high fluoride zones.
机译:本文的重点是从印度喀拉拉邦巴拉塔普扎河流域的潜水含水层采集的地下水样品的pH值,电导率(EC),总硬度,总铁和氟含量的时空分布。 pH,EC和总硬度等非离子物质的时空分布在印度标准局(BIS)和世界卫生组织(WHOf标准)的允许范围内。两个季节的总铁浓度表明,大部分区域都在0.3mg / L到1 mg / L的类别是BIS的理想限值。在巴拉沙拉普扎河流域,季风前地下水的氟化物含量在0.01 mg / L至1.2 mg / L范围内,而季风后0.01 mg / L到1.45 mg / L。该区域的地质特征在高氟化物区增加氟化物含量方面起着至关重要的作用。

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