To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India

Thirumanimuttar River is the only ephemeral stream passing through the heart of the Salemcity and flows towards southwest and joins river Cauvery in the southern region of Kuduthurai at near Paramathi Vellur forms the spinal cord for urban development. A number of industrial units including dyeing/b...

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Main Authors: Vasanthavigar, M., Srinivasamoorthy, K., Prasanna, Mohan, Poovalinga Ganesh, B.
Format: Journal Article
Published: NORTH UNIV BAIA MARE, FACULTY MINERAL RESOURCES & ENVIRONMENT, DR VICTOR BABES 62-A,, BAIA MARE, 430083, ROMANIA 2012
Subjects:
Online Access:http://www.ubm.ro/sites/CJEES/viewTopic.php?topicId=245
http://hdl.handle.net/20.500.11937/20943
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author Vasanthavigar, M.
Srinivasamoorthy, K.
Prasanna, Mohan
Poovalinga Ganesh, B.
author_facet Vasanthavigar, M.
Srinivasamoorthy, K.
Prasanna, Mohan
Poovalinga Ganesh, B.
author_sort Vasanthavigar, M.
building Curtin Institutional Repository
collection Online Access
description Thirumanimuttar River is the only ephemeral stream passing through the heart of the Salemcity and flows towards southwest and joins river Cauvery in the southern region of Kuduthurai at near Paramathi Vellur forms the spinal cord for urban development. A number of industrial units including dyeing/bleaching and sago industries were located within the core zone. The industrial effluent and sewage water disposal by conversion of natural streams and water bodies as sewer drains. An attempt has been made to study the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin. Hence, thirty-four groundwater samples were collected for stable isotope [Oxygen (18O), Hydrogen (2H or Deuterium)] and trace element studies. The study reveals that the groundwater samples undergone some evaporation prior to infiltration. The d-excess of the groundwater were varied between -4.89 to 10.08 ‰ indicating that the water undergone strong evaporation during recharge into the local groundwater system. The trace element study indicates that some trace metals such as Al, Ni and Pb exceeds the acceptable limit. The spatial distribution map shows higher concentration of Cr is increased from north to south due to the textile dyeing units were located around in the region.
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institution Curtin University Malaysia
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publishDate 2012
publisher NORTH UNIV BAIA MARE, FACULTY MINERAL RESOURCES & ENVIRONMENT, DR VICTOR BABES 62-A,, BAIA MARE, 430083, ROMANIA
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spelling curtin-20.500.11937-209432017-01-30T12:22:17Z To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India Vasanthavigar, M. Srinivasamoorthy, K. Prasanna, Mohan Poovalinga Ganesh, B. groundwater recharge industrial effluent trace element stable isotope Thirumanimuttar Thirumanimuttar River is the only ephemeral stream passing through the heart of the Salemcity and flows towards southwest and joins river Cauvery in the southern region of Kuduthurai at near Paramathi Vellur forms the spinal cord for urban development. A number of industrial units including dyeing/bleaching and sago industries were located within the core zone. The industrial effluent and sewage water disposal by conversion of natural streams and water bodies as sewer drains. An attempt has been made to study the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin. Hence, thirty-four groundwater samples were collected for stable isotope [Oxygen (18O), Hydrogen (2H or Deuterium)] and trace element studies. The study reveals that the groundwater samples undergone some evaporation prior to infiltration. The d-excess of the groundwater were varied between -4.89 to 10.08 ‰ indicating that the water undergone strong evaporation during recharge into the local groundwater system. The trace element study indicates that some trace metals such as Al, Ni and Pb exceeds the acceptable limit. The spatial distribution map shows higher concentration of Cr is increased from north to south due to the textile dyeing units were located around in the region. 2012 Journal Article http://hdl.handle.net/20.500.11937/20943 http://www.ubm.ro/sites/CJEES/viewTopic.php?topicId=245 NORTH UNIV BAIA MARE, FACULTY MINERAL RESOURCES & ENVIRONMENT, DR VICTOR BABES 62-A,, BAIA MARE, 430083, ROMANIA restricted
spellingShingle groundwater
recharge
industrial effluent
trace element
stable isotope
Thirumanimuttar
Vasanthavigar, M.
Srinivasamoorthy, K.
Prasanna, Mohan
Poovalinga Ganesh, B.
To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title_full To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title_fullStr To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title_full_unstemmed To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title_short To understand the characteristics of stable isotopes and trace elements in groundwater of Thirumanimuttar sub-basin, Tamil Nadu, India
title_sort to understand the characteristics of stable isotopes and trace elements in groundwater of thirumanimuttar sub-basin, tamil nadu, india
topic groundwater
recharge
industrial effluent
trace element
stable isotope
Thirumanimuttar
url http://www.ubm.ro/sites/CJEES/viewTopic.php?topicId=245
http://hdl.handle.net/20.500.11937/20943