Water Distribution from Artificial Recharge via Infiltration Basin under Constant Head Conditions

Tiansong Qi,Hu Li,Xiaobo Wang,Yanqing Men,Longcang Shu,Portia Annabelle Opoku

doi:10.3390/w13081052

Tiansong Qi, Hu Li + Show 4 more

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https://doi.org/10.3390/w13081052

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Abstract

The vadose zone plays a significant role during artificial recharge via the infiltration basin. Its thickness, lithology, heterogeneity, among others greatly affect the recharge efficiency. The main objective of this research is to establish the role of the vadose zone and the impacts of infiltration basin features and vadose zone factors on water distributions. In this work, an ideal conceptual model was considered, and mathematical models were built using HYDRUS (2D/3D) software package version 2.05. A total of 138 numerical experiments were implemented under seven types of experimental conditions. The experimental data were analyzed with the aid of correlation and regression analysis. The results showed that infiltration basin features and vadose zone factors had various impacts on water distribution, low permeability formation had various effects on evaporation depending on its depth, and there were consistent, similar, or different variation trends between infiltration and recharge. In conclusion, it is recommended that when the vadose zones are to be chosen as an infiltration basin site, the trade-off among the infiltration, recharge, storage, and evaporation should be seriously considered. This paper may contribute to a better understanding of the vadose zone as a buffer zone for artificial recharge.

Highlights

Groundwater is a vital resource for life forms, which caters for billions of populations [1]
This research deals with the impacts of vadose zone factors on artificial recharge via the infiltration basin using modeling exercises
This chapter details the results from the numerical experiments and the data analysis. They are categorized into homogenous domain experimental conditions and heterogenous domain experimental conditions

Summary

Introduction

Groundwater is a vital resource for life forms, which caters for billions of populations [1]. On the other hand, managed aquifer recharge can be utilized to increase water resources [4], to alleviate seawater intrusion and land subsidence, both derived from groundwater overexploitation [5,6,7] This technology can be used to improve the quality of reclaimed water and desalinated water [8,9,10,11,12,13,14] and could even serve as a water conveyance system [15]. This research deals with the impacts of vadose zone factors on artificial recharge via the infiltration basin using modeling exercises. This is because the thickness, lithology, antecedent water content, etc. Spreading methods are more common than well, shaft and borehole recharge whereas more modeling studies identified were conducted for the latter [21]

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