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首页> 外文期刊>Environmental Modeling & Assessment >Groundwater Modeling in Agricultural Watershed under Different Recharge and Discharge Scenarios for Quaternary Aquifer Eastern Nile Delta, Egypt
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Groundwater Modeling in Agricultural Watershed under Different Recharge and Discharge Scenarios for Quaternary Aquifer Eastern Nile Delta, Egypt

机译:埃及东尼罗河三角洲第四纪含水层不同补给与灌溉情景下农业流域地下水模拟

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摘要

Different scenarios of recharge and discharge were assessed for sustainable management of groundwater in Quaternary aquifer east of Nile Delta. MODFLOW was utilized to investigate the effect of land use change and damming construction in the upstream of the Nile River on the current and short-term groundwater management strategies. The interpretive transient simulation was performed between 2004 and 2016 after steady-state calibration in 2004, and transient state from 2004 to 2013 with different irrigation recharges associated with land use change in this period. Sensitivity analysis was performed for hydraulic conductivities, recharge, and conductance parameters. The predictive transient simulation was run till 2023 under three scenarios of increasing pumping rates by 15, 30, and 50% for agriculture expansion and specified head reduction of Port Said Canal by 0.2, 0.4, and 0.6 m associated with the reduction of Nile water levels after Grand Ethiopian Residence Dam, GERD operation in 2017. Results from the in- and out-flow budgets showed that groundwater aquifer is stable at the current rate of pumping till 2023. Groundwater heads decreased by 0.2 and 0.42 m in the southern section, and a slight increase in the northern part was noticed for the first and second scenarios, respectively. When additional pumping stress is applied (50% increase), groundwater head dropped by 0.66 m, and the storage is no longer able to maintain the aquifer capacity after 2020 (worst-case scenario).
机译:评估了尼罗河三角洲东部第四纪含水层中地下水的可持续管理的各种补给和排泄方案。 MODFLOW用于调查尼罗河上游土地利用变化和筑坝工程对当前和短期地下水管理策略的影响。在2004年进行稳态校准之后,在2004年至2016年之间进行了解释性的瞬态模拟,在此期间,2004年至2013年的瞬态具有不同的灌溉补给量,这与土地利用的变化有关。对水力电导率,补给量和电导率参数进行了敏感性分析。预测性瞬态模拟一直运行到2023年,在三种情况下,农业扩张将抽水率提高15%,30%和50%,并且与尼罗河水位降低相关的塞得港运河的总压头降低0.2、0.4和0.6m继大埃塞俄比亚人居大坝之后,GERD于2017年投入运营。流入和流出预算的结果表明,以目前的抽水速度,到2023年,地下水含水层是稳定的。南部的地下水头下降了0.2和0.42 m,并且在第一种和第二种情况下,北部地区略有增加。当施加额外的抽水压力(增加50%)时,地下水水头下降了0.66 m,并且在2020年之后存储不再能够保持含水层容量(最坏的情况)。

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