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Elango, L.
- Assessment of Groundwater Quality in a Part of Chinnar Watershed, Perambalur District, Tamil Nadu, India
Abstract Views :91 |
PDF Views:72
Authors
S. Anbarasu
1,
L. Elango
1
Affiliations
1 Department of Geology, Anna University, Chennai-600025, Tamil Nadu, IN
1 Department of Geology, Anna University, Chennai-600025, Tamil Nadu, IN
Source
International Journal of Earth Sciences and Engineering, Vol 9, No 6 (2016), Pagination: 2466-2471Abstract
Hydrochemical studies play a major role in the chemical composition of groundwater. The present study was carried out to assess the groundwater quality in a part of Chinnar watershed located in the western part of Perambalur District, Tamilnadu, India.The dominance of ions present in the groundwater follows the order as Na+,Ca2+,K+ and Mg2+ for cations and HCO3-,Cl- and SO42- for anions. Based on electrical conductivity the groundwater of this region is generally brackish and a few of them are classified as fresh. About 70% of the groundwater samples were in the category of good to permissible based on the recommendation of Bureau of Indian Standards. Ca-HCO3, Na-Cl along with Ca-Mg-Cl are the dominant hydrochemical facies of the study area. The groundwater in general is mostly alkaline with moderate salinity. The groundwater is suitable for drinking and irrigation purposes in most of the areas except for a few locations, where they are unsuitable for drinking purpose.Keywords
Groundwater, Sodium Percent, Irrigation, Drinking Water, Salinity, Perambalur, Tamil Nadu, India.Full Text
- Chemical Character of Detrital Garnet in Cauvery River Sediment and its Provenance, South India
Abstract Views :450 |
PDF Views:137
Authors
Affiliations
1 Department of Geology, Anna University, Chennai-600025, Tamil Nadu, IN
2 Department of Studies in Earth Sciences, University of Mysore, Mysore-570006, Karnataka, IN
1 Department of Geology, Anna University, Chennai-600025, Tamil Nadu, IN
2 Department of Studies in Earth Sciences, University of Mysore, Mysore-570006, Karnataka, IN
Source
International Journal of Earth Sciences and Engineering, Vol 10, No 4 (2017), Pagination: 752-756Abstract
The study attempts to determine the chemical characters of detrital garnets provenance in the Cauvery River Basin. The geochemical results reveal that the detrital garnets are derived from biotite schist, charnockite, and gneisses of intermediate felsic, moderate to strong weathered provenance. The end member composition of the garnets indicates almandine species that are metamorphosed in amphibolite to granulite facies P-T conditions. The angular outline of detrital garnet in the upstream and sub-rounded to rounded grains in the downstream attribute it’s transport from the upstream of the Cauvery River.Keywords
Detrital Garnet, Mineral Chemistry, Provenance, Cauvery River.Full Text
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