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Numerical Simulations for Artificial Recharge of Takaoka Groundwater Basin, Tosa City, Japan

机译:日本土佐市高冈地下水盆地人工补给的数值模拟

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The lowering of groundwater levels in the Takaoka basin poses a significant threat to sustainable utilization of its scarce ground-water resource. A transient, two-dimensional groundwater flow model was developed for a single-layered unconfined aquifer system and was solved by the finite-element method (FEM), Using this numerical model, present and future groundwater scenarios for dry periods are presented by simulating various groundwater management strategies. The response of the Takaoka basin to some artificial recharge techniques was also investigated, and two techniques are proposed for its rehabilitation. The model estimated recharge from the Niyodo River to be about 22.24 × 10~3 m~3/d in a no-pumping situation. A decline equal to or greaterthan 0.5 m in the Niyodo River water level considerably lowers the basin's groundwater levels. Any increase in pumping from the present rate will aggravate the overdraft problem. Modeling results suggest a cutback of about 30% in pumping as a preliminarymeasure to mitigate groundwater mining. The worst groundwater scenario during drought years emphasizes the immediate rehabilitation of the basin. Further, simulation results of two artificial recharge techniques—viz., groundwater barrier and Niyodo River modification—indicated promising potential for rehabilitating the depleting aquifer, While the influence of the proposed barrier is limited, a weir of height 4.5 m from the dry period water level in the Niyodo River is sufficient to meet the presentgroundwater demand and thereby stabilize the aquifer.
机译:高冈盆地地下水位的下降对其稀缺地下水资源的可持续利用构成了重大威胁。针对单层无限制含水层系统建立了一个瞬态二维地下水流模型,并通过有限元方法(FEM)对其进行了求解。利用该数值模型,通过模拟各种地下水,得出了目前和未来干旱时期的地下水情景。地下水管理策略。还研究了高冈盆地对某些人工补给技术的响应,并提出了两种修复方法。该模型估计在不抽水的情况下,二淀河的补给量约为22.24×10〜3 m〜3 / d。 Niyodo河水位下降等于或大于0.5 m会大大降低流域的地下水位。从目前的速度增加抽水将加剧透支问题。模拟结果表明,抽水量可减少约30%,作为减轻地下水开采的初步措施。干旱年份最糟糕的地下水情境强调了该流域的即时恢复。此外,两种人工补给技术的模拟结果,即地下水屏障和二渡河改造,表明修复枯竭含水层的潜力很大,尽管该屏障的影响是有限的,但距离干旱期水高4.5 m Niyodo河的水位足以满足目前的地下水需求,从而稳定含水层。

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