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Monitoring regional groundwater flow and contaminant transport in Southern Punjab, Pakistan, using numerical modeling approach

机译:利用数值模拟方法监测旁遮普省旁遮普郡南部地下水流量和污染物运输

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A three-dimensional groundwater flow model was developed using Visual MODFLOW to characterize the groundwater regime and simulate groundwater flow behavior in Multan District of Pakistan from 1962 to 2015. The multi-layered model was calibrated in which arsenic concentration was used as a point source for solute transport modeling in the flow domain. The model calibration indicated a close agreement between the simulated and observed head values achieving residual mean value of 0.1 m and a correlation coefficient (R) value of 0.9 during the steady-state condition. The study revealed a gradual rise in groundwater levels from 1972, i.e., at a rate of about 0.08 m/year followed by a gradual decline after 1990 at a rate of about 0.39 m/year likely due to overexploitation of groundwater. The other reasons of depletion of the aquifer may include lesser natural recharge due to reduction in canal command area and increasing water demand and pumpage due to growing urban/rural development. The findings of contaminant transport modeling depicted flow path representation of arsenic movement mostly towards the rivers in the model domain. Overexploitation of groundwater needs to be controlled for effective development of groundwater resource, and proper purifying/filtering techniques have to be adopted to ensure safe groundwater use in the area.
机译:使用视觉模型开发了三维地下水流量模型,从1962年到2015年使用视觉模型来表征地下水制度,并模拟巴基斯坦多区地区的地下水流动。校准多层模型,其中砷浓度被用作点源流动域中的溶质运输建模。模型校准指示在稳态条件下实现剩余平均值0.1μm的剩余平均值和0.9的相关系数(R)值之间的密切一致。该研究揭示了1972年的地下水位逐渐上升,即,约0.08米/年的速度,然后在1990年后逐渐下降,其可能由于地下水的过度曝光而大约0.39米/年。含水层消耗的其他原因可能包括由于运河指挥区的降低以及由于城市/农村发展的日益增长而增加的水需求和振动,较低的自然补给。污染物传输建模的发现描绘了砷运动的流动路径表示主要朝向模型领域的河流。需要控制地下水的过度开发,以便有效地开发地下水资源,并且必须采用适当的净化/过滤技术来确保该地区的安全地下水。

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