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利用多元统计分析和地球物理方法对突尼斯东北部一个小型沿海平原的地下水 - 咸水地表水相互作用进行量化

Quantification of Groundwater - Saline Surface Water Interaction in a Small Coastal Plain in North-East Tunisia using Multivariate Statistical Analysis and Geophysical Method.

作者信息

Chekirbane Anis, Tsujimura Maki, Lachaal Fethi, Khadhar Samia, Mlayah Ammar, Kawachi Atsushi, Isoda Hiroko, Tarhouni Jamila, Benalaya Abdallah

机构信息

1 Water Researches and Technologies Center (CERTE), Borj Cedria Technopark, BP 273, Soliman 8020, Nabeul, Tunisia.

出版信息

Water Environ Res. 2016 Dec 1;88(12):2292-2308. doi: 10.2175/106143016X14609975746163. Epub 2016 Apr 8.

Abstract

Amultivariate statistical analysis used with geophysical investigation enabled the assessment of interaction between saline surface water and groundwater in the coastal plain of Wadi Al Ayn and Daroufa in CapBon peninsula, north-east Tunisia. The application of the Principal Component Analysis (PCA) identified the end members which contribute to groundwater recharge: the wastewater infiltrated from Wadi Al Ayn, the oilfield brine infiltrated to the aquifer through the sandy bed of Wadi Al Ayn, the intruded seawater near Wadi Daroufa in the downstream region and the fresh groundwater flowing from the upstream region. The contribution of wastewater in groundwater recharge varies from 1.4% in the upstream region of Wadi Al Ayn to 77% near its downstream part. The fraction of oilfield brine mixed with groundwater in the alluvial aquifer under Wadi Al Ayn varies from 1% to 13%; whereas the fraction of intruded seawater into the coastal part of the aquifer near Daroufa region varies from 2% to 21%.

摘要

在突尼斯东北部邦角半岛的瓦迪艾因和达鲁法沿海平原,将多元统计分析应用于地球物理调查,能够评估咸地表水与地下水之间的相互作用。主成分分析(PCA)的应用确定了对地下水补给有贡献的端元:从瓦迪艾因渗入的废水、通过瓦迪艾因沙质河床渗入含水层的油田卤水、下游地区靠近瓦迪达鲁法处入侵的海水以及从上游地区流入的新鲜地下水。废水对地下水补给的贡献在瓦迪艾因上游地区为1.4%,在其下游附近则为77%。瓦迪艾因下方冲积含水层中与地下水混合的油田卤水比例在1%至13%之间;而达鲁法地区附近含水层沿海部分入侵海水的比例在2%至21%之间。

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