阿尔及利亚下塞豪斯含水层系统海水入侵的数值模拟

IF 0.8 Q4 WATER RESOURCES
Samir Hani, Fayçal Toumi, N. Bougherira, I. Shahrour, A. Hani
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引用次数: 0

摘要

海水入侵对阿尔及利亚东北部下塞豪斯地区的供水、农业和工业活动构成了很高的风险。为了分析这一风险,利用MODFLOW和MT3DMS软件建立了沿海含水层海水入侵的三维模型。该模型的应用表明,地下水抽取导致水位不断下降,氯离子浓度不断升高。此外,盐锋可以在陆地上推进300 ~ 2500 m。这些结果表明了采取适当措施保护含水层的必要性。对2045年的数值预测表明,考虑到地下水采取量增加20%,水位将显著下降,相对于平均海平面将下降至-6米,内陆约10公里处的Cl-浓度将增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical simulation of seawater intrusion in the lower Seybouse aquifer system, Algeria
Seawater intrusion represents a high risk for the water supply, the agriculture and industry activities in the lower Seybouse region of North-Eastern Algeria. In order to analyze this risk, a three-dimensional model was developed using the MODFLOW and MT3DMS codes to predict seawater intrusion in the coastal aquifer. The application of this model indicates that the groundwater withdrawals result in a continuous decrease of the water level and in an increase of chloride concentration. Moreover, the salt front could progress by 300 to 2500 m in the land. These results show the necessity of adequate measures for the protection of the aquifer. Numerical predictions for 2045, considering an increase of groundwater withdrawals by 20%, show a fairly significant decrease in water levels, up to -6 m with respect to the mean sea level, and an increase of Cl- concentrations up to about 10 km inland.
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来源期刊
CiteScore
1.80
自引率
50.00%
发文量
36
审稿时长
8 weeks
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