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(Location: IWMI-HQ Call no: PER Record No: H026847)
(Location: IWMI-HQ Call no: PER Record No: H029699)
(Location: IWMI-HQ Call no: PER Record No: H035695)
4 Malano, H. M.; George, B. A.; Davidson, B. 2005. Asset management modeling framework for irrigation and drainage systems: Principles and case study application. Irrigation and Drainage Systems, 19:107-127.
(Location: IWMI-HQ Call no: P 7401 Record No: H037462)
5 Davidson, B.; Malano, H. M.; George, B. A.. 2005. The financial viability of irrigation management companies: A case study of Cu Chi Irrigation System, Vietnam. Irrigation and Drainage Systems, 19:129-143.
(Location: IWMI-HQ Call no: P 7402 Record No: H037463)
(Location: IWMI-HQ Call no: PER Record No: H034449)
7 George, B. A.; Huang, J.; Malano, H.M. 2006. Improving quality and sustainability of irrigation delivery services in China: The case of the Zhanghe Irrigation System. In Willett, I. R.; Gao, Z. (Eds.) Agricultural water management in China: Proceedings of a workshop held in Beijing, China, 14 September 2005. Canberra, Australia: ACIAR. pp.111-124.
(Location: IWMI-HQ Call no: 631.7 G592 WIL Record No: H039225)
(Location: IWMI HQ Call no: e-copy only Record No: H046196)
(1.08 MB)
Since the 1990s, Indian farmers, supported by the government, have partially shifted from surface-water to groundwater irrigation in response to the uncertainty in surface-water availability. Water-management authorities only slowly began to consider sustainable use of groundwater resources as a prime concern. Now, a reliable integration of groundwater resources for water-allocation planning is needed to prevent aquifer overexploitation. Within the 11,000-km2 Musi River sub-basin (South India), human interventions have dramatically impacted the hard-rock aquifers, with a water-table drop of 0.18m/a over the period 1989–2004. A fully distributed numerical groundwater model was successfully implemented at catchment scale. The model allowed two distinct conceptualizations of groundwater availability to be quantified: one that was linked to easily quantified fluxes, and one that was more expressive of long-term sustainability by taking account of all sources and sinks. Simulations showed that the latter implied 13% less available groundwater for exploitation than did the former. In turn, this has major implications for the existing waterallocation modelling framework used to guide decision makers and water-resources managers worldwide.
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