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Evaluation of Artificial Recharge on Groundwater Using MODFLOW Model (Case Study: Gotvand Plain-Iran)

机译:使用MODFLOW模型评估地下水的人工补给(案例研究:Gotvand Plain-Iran)

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Themanaged recharge of groundwater is a stable and newfound technique which hasalready produced successful results and is expected to solve many of theproblems of water resources, particularly in arid and semiarid areas. Theaquifer artificial recharge is considered as a strategy for the improvement anddevelopment of groundwater resources and their storage to compensate for thedamage to them. In this regard, the advanced models of groundwater offersuitable tools for the management and assessment of aquifers. The mainobjective of this research is Simulation of Gotvand Plain aquifer using MODFLOWcode of GMS software is the primary objective of this research. The otherobjective is assessing the artificial recharge project of Abbid-Sarbishelocated in north of Gotvand. For this purpose, the studyarea was discretized in GMS software and the initial and boundary conditionswere specified. Then, the model was calibrated from September 2009 to August2010 in an unsteady state during 12 stress periods. After the optimization of hydrogeologicparameters, the model was validated from September 2009 to August 2010 and thenit was used to assess the artificial recharge. By analyzing the water budgetmodel, the behavior of piezometers and the observed data, the hydraulic ofgroundwater was evaluated. The results indicate that artificial recharge hasbeen effective in the western parts of the project and the most effectiverecharge has occurred during 2005-2006 and 2006-2007 around the piezometer G19.This project has a positive effect on the aquifer, but due to seasonalwater-flood spreading, sedimentation, and drought in the past years, its effectis not sufficient.
机译:地下水的有序补给是一项稳定的新技术,已经取得了成功的成果,有望解决许多水资源问题,特别是在干旱和半干旱地区。含水层人工补给被认为是改善和开发地下水资源及其存储以弥补对地下水的损害的一种策略。在这方面,先进的地下水模型为含水层的管理和评估提供了合适的工具。本研究的主要目的是使用GMS软件的MODFLOWcode模拟Gotvand平原含水层是本研究的主要目的。另一个目标是评估位于戈特万德北部的Abbid-Sarbishehe的人工补给工程。为此,在GMS软件中将研究区域离散化,并指定了初始条件和边界条件。然后,从2009年9月至2010年8月在12个应力周期的不稳定状态下对模型进行了校准。优化水文地质参数后,从2009年9月至2010年8月对该模型进行了验证,并使用了尼尼特模型来评估人工补给。通过分析水预算模型,压力计的性能和观测数据,评估了地下水的水力。结果表明,人工补给在该项目的西部已经有效,最有效的补给发生在压强仪G19周围的2005-2006年和2006-2007年之间。该项目对含水层产生了积极影响,但由于季节性水淹在过去的几年中,由于扩散,沉积和干旱,其效果还不够。

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