Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India

Study region: The Chaliyar river basin, Kerala State, India. Study focus: Detailed understanding about spatio-temporal variation in the interaction and exchange of water between surface and sub-surface reservoirs is important for effective watershed management. Spatio-temporal variations in the oxyg...

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Main Authors: A. Shahul Hameed, T.R. Resmi, S. Suraj, C. Unnikrishnan Warrier, M. Sudheesh, R.D. Deshpande
Format: Article
Language:English
Published: Elsevier 2015-09-01
Series:Journal of Hydrology: Regional Studies
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S221458181500004X
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author A. Shahul Hameed
T.R. Resmi
S. Suraj
C. Unnikrishnan Warrier
M. Sudheesh
R.D. Deshpande
author_facet A. Shahul Hameed
T.R. Resmi
S. Suraj
C. Unnikrishnan Warrier
M. Sudheesh
R.D. Deshpande
author_sort A. Shahul Hameed
collection DOAJ
description Study region: The Chaliyar river basin, Kerala State, India. Study focus: Detailed understanding about spatio-temporal variation in the interaction and exchange of water between surface and sub-surface reservoirs is important for effective watershed management. Spatio-temporal variations in the oxygen isotopic composition (δ18O) were used to understand the interaction between groundwater and river water, and to estimate the groundwater recharge from river water in the Chaliyar river basin. New hydrological insights for the region: Based on the spatio-temporal variation in δ18O values of river and groundwater and fluctuation in ground water levels, following important inferences are made: (1) estimated river water contribution to post-monsoon groundwater recharge is ∼16% in the lowland coastal area of the Chaliyar river basin and 29% in midland region; (2) northeast winter monsoon rains contribute to the groundwater of Chaliyar river basin only in an insignificant manner, and with a delayed response; (3) unlike river water samples which exhibit both seasonal and spatial variation of more than 3‰, the groundwater samples vary only marginally (∼1‰) between the seasons and across the physiographic zones; (4) groundwater samples exhibit inverse altitude gradient in δ18O values in the highland zone, in all the three seasons. This may be due to flow of the isotopically depleted groundwater down the gradient and evaporation of residual water in the upper reaches of the basin.
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spelling doaj.art-427b2f0abced4dab94722b76018337162022-12-21T19:30:28ZengElsevierJournal of Hydrology: Regional Studies2214-58182015-09-014PA485810.1016/j.ejrh.2015.01.003Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, IndiaA. Shahul Hameed0T.R. Resmi1S. Suraj2C. Unnikrishnan Warrier3M. Sudheesh4R.D. Deshpande5Isotope Hydrology Division, Centre for Water Resources Development and Management, Kunnamangalam, Kozhikode 673 571, IndiaIsotope Hydrology Division, Centre for Water Resources Development and Management, Kunnamangalam, Kozhikode 673 571, IndiaIsotope Hydrology Division, Centre for Water Resources Development and Management, Kunnamangalam, Kozhikode 673 571, IndiaIsotope Hydrology Division, Centre for Water Resources Development and Management, Kunnamangalam, Kozhikode 673 571, IndiaIsotope Hydrology Division, Centre for Water Resources Development and Management, Kunnamangalam, Kozhikode 673 571, IndiaGeosciences Division, Physical Research Laboratory, Navrangpura, Ahmedabad 380 009, IndiaStudy region: The Chaliyar river basin, Kerala State, India. Study focus: Detailed understanding about spatio-temporal variation in the interaction and exchange of water between surface and sub-surface reservoirs is important for effective watershed management. Spatio-temporal variations in the oxygen isotopic composition (δ18O) were used to understand the interaction between groundwater and river water, and to estimate the groundwater recharge from river water in the Chaliyar river basin. New hydrological insights for the region: Based on the spatio-temporal variation in δ18O values of river and groundwater and fluctuation in ground water levels, following important inferences are made: (1) estimated river water contribution to post-monsoon groundwater recharge is ∼16% in the lowland coastal area of the Chaliyar river basin and 29% in midland region; (2) northeast winter monsoon rains contribute to the groundwater of Chaliyar river basin only in an insignificant manner, and with a delayed response; (3) unlike river water samples which exhibit both seasonal and spatial variation of more than 3‰, the groundwater samples vary only marginally (∼1‰) between the seasons and across the physiographic zones; (4) groundwater samples exhibit inverse altitude gradient in δ18O values in the highland zone, in all the three seasons. This may be due to flow of the isotopically depleted groundwater down the gradient and evaporation of residual water in the upper reaches of the basin.http://www.sciencedirect.com/science/article/pii/S221458181500004XOxygen isotopeMass balanceGroundwater rechargeRiver-connected aquiferHumid tropicIndia
spellingShingle A. Shahul Hameed
T.R. Resmi
S. Suraj
C. Unnikrishnan Warrier
M. Sudheesh
R.D. Deshpande
Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
Journal of Hydrology: Regional Studies
Oxygen isotope
Mass balance
Groundwater recharge
River-connected aquifer
Humid tropic
India
title Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
title_full Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
title_fullStr Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
title_full_unstemmed Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
title_short Isotopic characterization and mass balance reveals groundwater recharge pattern in Chaliyar river basin, Kerala, India
title_sort isotopic characterization and mass balance reveals groundwater recharge pattern in chaliyar river basin kerala india
topic Oxygen isotope
Mass balance
Groundwater recharge
River-connected aquifer
Humid tropic
India
url http://www.sciencedirect.com/science/article/pii/S221458181500004X
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AT cunnikrishnanwarrier isotopiccharacterizationandmassbalancerevealsgroundwaterrechargepatterninchaliyarriverbasinkeralaindia
AT msudheesh isotopiccharacterizationandmassbalancerevealsgroundwaterrechargepatterninchaliyarriverbasinkeralaindia
AT rddeshpande isotopiccharacterizationandmassbalancerevealsgroundwaterrechargepatterninchaliyarriverbasinkeralaindia