Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios

The basaltic aquifers of the Upper Bhima River basin in southern India are heavily utilized for small-scale agriculture but face increasing demand-related pressures along with uncertainty associated with climate change impacts. To evaluate likely groundwater resource impacts over the coming decades,...

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Main Authors: L. Surinaidu, C. G. D. Bacon, P. Pavelic
Format: Article
Language:English
Published: Copernicus Publications 2013-02-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/17/507/2013/hess-17-507-2013.pdf
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spelling doaj-992d1a7713084e2ab97ce8ff376451362020-11-24T23:05:12ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382013-02-0117250751710.5194/hess-17-507-2013Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenariosL. SurinaiduC. G. D. BaconP. PavelicThe basaltic aquifers of the Upper Bhima River basin in southern India are heavily utilized for small-scale agriculture but face increasing demand-related pressures along with uncertainty associated with climate change impacts. To evaluate likely groundwater resource impacts over the coming decades, a regional groundwater flow model for the basin was developed. Model predictions associated with different climate change and abstraction scenarios indicate that the continuation of current rates of abstraction would lead to significant groundwater overdraft, with groundwater elevations predicted to fall by −6 m over the next three decades. Groundwater elevations can however be stabilized, but would require 20–30% of the mean surface water discharge from the basin to be recharged to groundwater, along with reductions in pumping (5–10%) brought about by improved water efficiency practices and/or shifts towards lower-water use crops. Modest reductions in pumping alone cannot stabilize groundwater levels; targeted conjunctive use and improved water use efficiency are also needed.http://www.hydrol-earth-syst-sci.net/17/507/2013/hess-17-507-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. Surinaidu
C. G. D. Bacon
P. Pavelic
spellingShingle L. Surinaidu
C. G. D. Bacon
P. Pavelic
Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
Hydrology and Earth System Sciences
author_facet L. Surinaidu
C. G. D. Bacon
P. Pavelic
author_sort L. Surinaidu
title Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
title_short Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
title_full Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
title_fullStr Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
title_full_unstemmed Agricultural groundwater management in the Upper Bhima Basin, India: current status and future scenarios
title_sort agricultural groundwater management in the upper bhima basin, india: current status and future scenarios
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2013-02-01
description The basaltic aquifers of the Upper Bhima River basin in southern India are heavily utilized for small-scale agriculture but face increasing demand-related pressures along with uncertainty associated with climate change impacts. To evaluate likely groundwater resource impacts over the coming decades, a regional groundwater flow model for the basin was developed. Model predictions associated with different climate change and abstraction scenarios indicate that the continuation of current rates of abstraction would lead to significant groundwater overdraft, with groundwater elevations predicted to fall by −6 m over the next three decades. Groundwater elevations can however be stabilized, but would require 20–30% of the mean surface water discharge from the basin to be recharged to groundwater, along with reductions in pumping (5–10%) brought about by improved water efficiency practices and/or shifts towards lower-water use crops. Modest reductions in pumping alone cannot stabilize groundwater levels; targeted conjunctive use and improved water use efficiency are also needed.
url http://www.hydrol-earth-syst-sci.net/17/507/2013/hess-17-507-2013.pdf
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