日本地球惑星科学連合2025年大会

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[E] 口頭発表

セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW25] Near Surface Investigation and Modeling for Groundwater Resources Assessment and Conservation

2025年5月25日(日) 15:30 〜 17:00 103 (幕張メッセ国際会議場)

コンビーナ:Tsai Jui-Pin(National Taiwan University, Taiwan)、谷口 真人(総合地球環境学研究所)、Yu Hwa-Lung(Taiwan Society of Groundwater resources and hydrogeology)、徳永 朋祥(東京大学大学院新領域創成科学研究科環境システム学専攻)、Chairperson:CHANG PINGYU(National Central University, Taiwan)、Jui-Pin Tsai(National Taiwan University, Taiwan)、Bo-Tsen Wang(Department of Bioenvironmental Systems Engineering, National Taiwan University)、Ying-Fan Lin(国立交通大学)、Shih-Jung Wang(National Central University)

16:00 〜 16:15

[AHW25-09] Performance of Managed Aquifer Recharge Due to Geological Heterogeneityː Insights from Experimental and Numerical Modeling

*Uttam Singh1、Alok Kumar1 (1.Malaviya National Institute of Technology Jaipur)

キーワード:Geological heterogeneity, MAR, Numerical modeling, Clay lense

The influence of geological heterogeneity on the effectiveness of managed aquifer recharge (MAR) is a key consideration in the design of the MAR system in terms of groundwater storage. A physical Sandbox setup and numerical modeling framework are developed to analyze how geological features such as clay lenses, and anticlines, as well as artificial structures like recharge wells, pumping wells, and recharge basins, influence groundwater flow patterns under MAR conditions to investigate the spatial and temporal distribution of recharged water in heterogeneous aquifers. To evaluate MAR performance in terms of groundwater storage and recovery potential by simulating hydraulic responses to artificial recharge and stress scenarios within diverse geological settings. By quantifying the impacts of aquifer heterogeneity on recharge rates, storage capacity, and recovery efficiency, the study aims to identify key factors that affect MAR outcomes. Heterogeneous aquifer systems shorten groundwater ages compared with homogeneous aquifer systems and decrease the artificially recharged water lens thickness thus, the stagnation point shifted to the downstream. The presence of the clay lens increases the groundwater residence time compared to the homogeneous layer. However, it showed little effect on the spatial flow pattern due to the shifting of the stagnation point in the flow direction.