Applying the Principal Component Analysis for a deeper understanding of the groundwater system: case study of the Bacchiglione Basin (Veneto, Italy)

IF 0.8 Q4 WATER RESOURCES
Mara Meggiorin, P. Bullo, Valentina Accoto, Giulia Passadore, A. Sottani, A. Rinaldo
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引用次数: 1

Abstract

In hydrogeology, it is often difficult to fully understand the hydraulic factors affecting the recharge of groundwater systems. Particularly, at a regional scale, the groundwater system can have different drivers depending on the considered area, i.e., soil permeability, paleochannels, and precipitation. Chemicalphysical (i.e. temperature) or hydrogeochemical data can help such understanding. However, this type of information is usually sparse at the regional scale, whereas extended groundwater piezometric head monitoring is more common. This study aims at exploiting these longitudinal observations of the hydraulic head to validate (and possibly bring more insights into) the geological structural model of aquifer systems. Clustering control points based on the piezometric head average annual variations can help the system conceptualization in two ways: (i) clusters can geographically identify areas with similar hydrogeological behavior; and (ii) the typical cluster annual variation with its ups and downs can bring insights on the recharge component of an aquifer system. Nevertheless, visual clustering can be a long and subjective procedure, thus this study suggests the use of the Principal Component Analysis to cluster the control points with a similar average annual variation of their recorded time series. This study supports the proposed analysis by applying it to the monitoring data of the Bacchiglione basin resulting in (i) clusters identified based on the number, moment, and lengths of groundwater level peaks and minima, (ii) wellgathered clusters in space, underpinning the groundwater hydrograph dependence on local driving factors. Furthermore, the investigation of clustering anomalies highlighted the relevance of the presence of time series with different recording periods pinpointing, however, the method’s capacity to spot a change in the hydrogeological cycle over the years.
应用主成分分析加深对地下水系统的理解:以意大利威尼托巴奇里奥内盆地为例
在水文地质学中,通常很难充分了解影响地下水系统补给的水力因素。特别是,在区域尺度上,地下水系统可能有不同的驱动因素,这取决于所考虑的区域,即土壤渗透性,古河道和降水。化学物理(即温度)或水文地球化学数据有助于这种理解。然而,这类信息在区域尺度上通常是稀疏的,而扩展的地下水水压水头监测则更为常见。本研究旨在利用这些水头的纵向观测来验证(并可能带来更多的见解)含水层系统的地质结构模型。基于压头年平均变化的聚类控制点可以在两个方面帮助系统概念化:(i)聚类可以在地理上识别具有相似水文地质行为的区域;(2)典型的集群年变化及其起伏可以提供对含水层系统补给成分的见解。然而,视觉聚类可能是一个漫长而主观的过程,因此本研究建议使用主成分分析对其记录时间序列具有相似平均年变化的控制点进行聚类。本研究通过将其应用于Bacchiglione流域的监测数据来支持所提出的分析,得出(i)基于地下水水位峰值和最低点的数量、时刻和长度确定的集群;(ii)在空间上聚集良好的集群,支持地下水水文对当地驱动因素的依赖。此外,聚类异常的调查突出了不同记录时期的时间序列存在的相关性,然而,该方法在多年来发现水文地质循环变化的能力。
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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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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