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Scenarios to control land subsidence using numerical modeling of groundwater exploitation: Aliabad plain (in Iran) as a case study

机译:使用地下水剥削数值模拟控制土地沉降的情景:Aliabad Plane(伊朗)作为案例研究

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摘要

The unconfined aquifer beneath the Aliabad plain is one of the few freshwater resources in northwestern Qom province in Iran. Land subsidence in the Aliabad plain is primarily the result of extensive overexploitation of groundwater resources and successive droughts. The harmful effects of overexploitation include significant socioeconomic consequences and severe damage to aquifers. The current study proposes an accurate scenario model that reduces the overall land subsidence by assessing different scenarios for future groundwater exploitation in the plain. The quantitative model consists of 120 time-steps over a period of 10 years (2006-2016). Model validation was achieved by comparing the calculated groundwater level variations with the results of piezometric evaluations in modeling. The results of the validated model were used to predict variations in the aquifer hydraulic head caused by changes in exploitation under different scenarios. Modeling of the Aliabad plain revealed that a 10% decrease in pumping will reduce and stabilize the groundwater decline and a 30% reduction will help recharge the aquifer. The model simulation was able to predict critical land subsidence of 35 cm by 2016. The geometric location of maximum land subsidence was predicted by comparing the geometric distribution of predicted land subsidence patterns with subsidence results from radar interferometry. Prediction of land subsidence by 2026 indicated that management of the exploitation of resources and strict aquifer stabilization programs can reduce the damage to the aquifer.
机译:Aliabad Plane下面的无凝结的含水层是伊朗西北Qom省少数淡水资源之一。 Aliabad Plane的土地沉降主要是地下水资源广泛过度的结果和连续干旱。过度开阔的有害影响包括显着的社会经济后果和对含水层的严重损害。目前的研究提出了一种准确的情景模型,通过评估平原中未来的地下水开采的不同情景来减少整体土地沉降。定量模型在10年(2006-2016)的时间内由120个时间步长组成。通过将计算的地下水位变化与建模中的压力评估结果进行比较来实现模型验证。验证模型的结果用于预测由不同场景下剥削变化引起的含水层液压头的变化。 Aliabad Plan的建模显示,泵送10%降低将减少和稳定地下水下降,减少30%,有助于充电含水层。模型模拟能够在2016年之前预测35厘米的临界地沉降。通过比较雷达干涉测量的沉降结果的预测土地沉降模式的几何分布来预测最大地沉降的几何位置。 2026年土地沉降预测表明,管理资源开采和严格的含水层稳定计划的管理可以减少对含水层的损害。

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