Abstract
The Barind Integrated Area Development Project (BIADP), NW Bangladesh launched in late eighties of last century boosted cropping intensity from 117% in pre-BIADP to about 200% at present. Increasing trend of rainfall for the period 1980–2006 in the southern portion had a positive impact on BIADP, but in the northeastern part, reverse trend is indicated. The groundwater outflow from the central part following the surface gradient is indicative of effluent drainage characteristics. Although rainfall has increased in the southern part, there has been progressive decline in groundwater level due to increase in irrigation demand. In the northern part there has been decline in groundwater level due to less resource potential. The PET, ETcrops and net irrigation requirement generally has decreased from pre- to post-Project implementation stages and rainwater has been the supplementary irrigation resource and thus dependency on groundwater has been reduced with exception in northwestern part. While the southern part is marching towards humid condition, north is creeping towards semi-aridity. Proper groundwater resource management with ecological balance is warranted for the sustainability of BIADP.
Similar content being viewed by others
References
BMDA (2001) Project Proforma (rebound) for the Barind Integrated Area Development Project, Phase-II (4th revision), Barind Multipurpose Development Authority, Rajshahi.
Doorenbos, J. and Pruitt (1977) Crop Water Requirements, Irrigation and Drainage Paper No. 24, FAO, Rome.
Epc and Mpott Macdonald (1994) Study to forecast declining groundwater levels in Bangladesh, Report for UNICEF and DPHE, Engineering and Planning Consultants, Bangladesh.
Hoque, M. (1982) Tectonic set up of Bangladesh and its relation to hydrocarbon accumulation, Phase-I: Center for Policy Research, Dhaka University and Universities Field Staff International (UFSI), USA publication, 177p.
IWM (2006) Project Brief on Groundwater Model Study for Deep Tube Well Installation Project in Barind Area, Draft Final Report, Institute of Water Modeling, Dhaka.
Jahan, C.S. (1997) Origin of groundwater and prospective of its utilization in Barind area, Bangladesh. PhD Thesis, Moscow State Geological Prospecting Academy, Russia.
Kranti Associates Ltd. (2000) Impact Evaluation: Barind Integrated Area Development Project (BIADP), Final report, Ministry of Agriculture, Dhaka.
Michael, A.M. (1978) Irrigation Theory and Practice, Vikas Publishng House Pvt. Ltd. India.
Morgan, J.P. and McIntire, W.G. (1959) Quaternary Geology of Bengal Basin, East Pakistan and India. Geol. Soc. Amer. Bull., v.70, pp.319–342.
Penman, H.L. (1948) Natural evaporation from open water, bare soil and grass. Royal Society, London, Ser. A, v.193, pp.120–146.
Jahan, C.S., ISLAM, M.A., Mazumder, Q.H., Asaduzzaman, M., Islam, M.M., Islam, M.O. and Sultana, A. (2005) Evaluation of Depositional Environment and Aquifer Condition in the Barind Area, Bangladesh, using Gamma Ray Well Log Data. Jour. Geol. Soc. India, v.70, pp.1070–1076.
Pitman, G.T.K. (1981) Aquifer and Recharges Evaluation in Bangladesh, Technical Note No.8 UNDP/UNDTCD Groundwater Survey, BGD/74/009, BWDB, GWC.
Roy, P.K. and Mazumdar, A. (2007) Study on Hydrology and Drought in the Flood Region of Damodar River Basin. Jour. Geol. Soc.f India, v.69, pp.1011–1019.
UNDP (1992) Groundwater Survey, The Hydrogeological Condition of Bangladesh, United Nations Development Project Technical Report, Prepared for the Govt. of the Peoples Republic of Bangladesh.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Jahan, C.S., Mazumder, Q.H., Islam, A.T.M.M. et al. Impact of irrigation in Barind Area, NW Bangladesh — An evaluation based on the meteorological parameters and fluctuation trend in groundwater table. J Geol Soc India 76, 134–142 (2010). https://doi.org/10.1007/s12594-010-0085-x
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s12594-010-0085-x