Implications of the Melamchi water supply project for the Kathmandu Valley groundwater system

被引:5
|
作者
Thapa, Bhesh Raj [1 ,2 ]
Ishidaira, Hiroshi [1 ]
Gusyev, Maksym [3 ]
Pandey, Vishnu Prasad [2 ]
Udmale, Parmeshwar [4 ]
Hayashi, Masaki [5 ]
Shakya, Narendra Man [6 ]
机构
[1] Univ Yamanashi, Interdisciplinary Res Ctr River Basin Environm IC, Takeda 4-3-11, Kofu, Yamanashi 4008511, Japan
[2] Int Water Management Inst, Nepal Off, Pulchowk 3, Lalitpur, Nepal
[3] Publ Works Res Inst, Int Ctr Water Hazard & Risk Management ICHARM, Tsukuba, Ibaraki, Japan
[4] Kyoto Univ, Dept Civil & Earth Resources Engn, Kyoto 6158540, Japan
[5] Univ Calgary, Dept Geosci, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada
[6] Tribhuvan Univ, Inst Engn, Dept Civil Engn, Pulchowk, Lalitpur, Nepal
关键词
Groundwater management; Groundwater modeling; Kathmandu Valley; Melamchi; MODEL; QUALITY; TRITIUM; NEPAL; AGES;
D O I
10.2166/wp.2019.084
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
To meet the demand deficit in Kathmandu Valley, the Government of Nepal has planned to supply an additional 510 million liters per day (mld) of water by implementing the Melamchi Water Supply Project (MWSP) in the near future. In this study, we aim to assess the spatial distribution of groundwater availability and pumping under five scenarios for before and after the implementation of the MWSP using a numerical groundwater flow model. The data on water demand, supply infrastructure, changes in hydraulic head, groundwater pumping rates, and aquifer characteristics were analyzed. Results showed that groundwater pumping from individual wells ranges from 0.0018 to 2.8 mld and the average hydraulic head declined from 2.57 m below ground level (bgl) (0.23 m/year) to 21.58 m bgl (1.96 m/year). Model simulations showed that changes in average hydraulic head ranged from +2.83 m to +5.48 m at various stages of the MWSP implementation, and -2.97 m for increased pumping rates with no implementation of the MWSP. Regulation in pumping such as monetary instruments (groundwater pricing) on the use of groundwater along with appropriate metering and monitoring of pumping amounts depending on the availability of new and existing public water supply could be interventions in the near future.
引用
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页码:120 / 137
页数:18
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