Hydraulic characterization of Pwales aquifer in Malta Island preparatory for planning managed aquifer recharge (MAR) pilot plant

M. C. Caputo, Lorenzo De Carlo, A. C. Turturro, M. Sapiano, Julian Mamo, Oriana Balzan, Luke Galea, M. Schembri
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Abstract

Whitin the aim to reduce the water demand by increasing water use efficiency and providing alternative water resources, and mainly to meet the demand of good quality irrigation water for agriculture, the Energy and Water Agency of Malta is planning to develop a Managed Aquifer Recharge pilot plant in Pwales Valley to improve the quantitative and qualitative status of the groundwater body. For this reason a detailed hydraulic characterization of the valley was carried out. Specifically, hydraulic properties of the rocks that constitute strata atop of the Pwales aquifer were determined by means of both laboratory measurements on samples and field test carried out in the studied area. The water retention and hydraulic conductivity functions, which relate the matric potential, ψ, and hydraulic conductivity, K, to the water content, θ, respectively, were measured using three experimental methods because each of them allows to obtain data points in a specific wet range. The water retention and hydraulic conductivity functions were measured on samples extracted from blocks of Upper Coralline Limestone formation, that hosts the aquifer, collected in three different quarries: Ghian Tuffieha, Mellieha and San Martin areas. The measured water retention and hydraulic conductivity data were fitted with LABROS SoilView Analysis software that allows to describe the functions and obtain the parameters which are crucial for modelling the water flow and transport processes in the critical zone. In addition, large ring infiltrometer test was carried out to determine the field saturated hydraulic conductivity, Kfs, and the average infiltration rate. Knowledge of the hydraulic characteristics of the Upper Coralline Limestone, completely missing in the scientific literature, allows developing a local groundwater-flow numerical model in order to better describe and understand how the water flows from the soil to the groundwater of the valley and visualize different environmental scenarios such as the potential effects of Managed Aquifer Recharge plant in the Pwales Coastal Groundwater Body.
马耳他岛 Pwales 含水层的水力特征,为规划有管理的含水层补给 (MAR) 试点工厂做准备
为了通过提高用水效率和提供替代水资源来减少对水的需求,主要是为了满足农业对优质灌溉用水的需求,马耳他能源和水务局计划在普瓦尔斯山谷开发一个含水层管理补给试点工厂,以改善地下水体的数量和质量状况。为此,对山谷进行了详细的水力特征描述。具体而言,通过在研究区域对样本进行实验室测量和实地测试,确定了构成普瓦尔斯含水层顶部地层的岩石的水力特性。保水性和水力传导性函数(分别将母势 ψ 和水力传导性 K 与含水量 θ 联系起来)使用三种实验方法进行测量,因为每种方法都可以获得特定湿度范围内的数据点。在三个不同的采石场采集的含水层所在的上珊瑚石灰岩地层岩块中提取的样本测量了保水性和水导率函数:Ghian Tuffieha、Mellieha 和 San Martin 地区。用 LABROS SoilView 分析软件对测量到的保水性和水力传导性数据进行了拟合,该软件可以描述功能并获得对临界区水流和传输过程建模至关重要的参数。此外,还进行了大型环形渗透仪测试,以确定实地饱和导水率 Kfs 和平均渗透率。对科学文献中完全缺失的上珊瑚灰岩水力特征的了解,有助于开发当地地下水流数值模型,从而更好地描述和了解水是如何从土壤流向山谷地下水的,并可视化不同的环境情景,如普瓦尔斯沿海地下水体中管理性含水层补给站的潜在影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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