Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers

The composition of soils in aquifers is typically not homogeneous, and soil layers may be cracked or displaced due to geological activities. This heterogeneity in soil distribution within aquifers affects groundwater flow and water level variations. In the present study, we established a two-dimensi...

Full description

Bibliographic Details
Main Authors: Ming-Chang Wu, Ping-Cheng Hsieh
Format: Article
Language:English
Published: AIMS Press 2023-11-01
Series:AIMS Mathematics
Subjects:
Online Access:https://www.aimspress.com/article/doi/10.3934/math.20231540?viewType=HTML
_version_ 1797508531159564288
author Ming-Chang Wu
Ping-Cheng Hsieh
author_facet Ming-Chang Wu
Ping-Cheng Hsieh
author_sort Ming-Chang Wu
collection DOAJ
description The composition of soils in aquifers is typically not homogeneous, and soil layers may be cracked or displaced due to geological activities. This heterogeneity in soil distribution within aquifers affects groundwater flow and water level variations. In the present study, we established a two-dimensional (2D) mathematical model that considers the influence of surface recharge on groundwater flow in heterogeneous sloping aquifers. By considering temporal variations in surface recharge, slope angle and aquifer heterogeneity, the simulated results are expected to better reflect real conditions in natural aquifers. The effects of aquifer heterogeneity on groundwater flow and water levels are particularly significant in sloping aquifers. The study's findings indicate that even when the soil composition remains constant, variations in groundwater level and flow may be considerable, depending on factors such as soil alignment, slope angle of the aquifer's base layer and the direction of water flow.
first_indexed 2024-03-10T05:06:20Z
format Article
id doaj.art-ac22829f34064d28816b2695d7e5db5f
institution Directory Open Access Journal
issn 2473-6988
language English
last_indexed 2024-03-10T05:06:20Z
publishDate 2023-11-01
publisher AIMS Press
record_format Article
series AIMS Mathematics
spelling doaj.art-ac22829f34064d28816b2695d7e5db5f2023-11-23T01:21:14ZengAIMS PressAIMS Mathematics2473-69882023-11-01812301203014110.3934/math.20231540Influence of nonuniform recharge on groundwater flow in heterogeneous aquifersMing-Chang Wu0Ping-Cheng Hsieh 1Department of Soil and Water Conservation, National Chung Hsing University, Taichung 40227, TaiwanDepartment of Soil and Water Conservation, National Chung Hsing University, Taichung 40227, TaiwanThe composition of soils in aquifers is typically not homogeneous, and soil layers may be cracked or displaced due to geological activities. This heterogeneity in soil distribution within aquifers affects groundwater flow and water level variations. In the present study, we established a two-dimensional (2D) mathematical model that considers the influence of surface recharge on groundwater flow in heterogeneous sloping aquifers. By considering temporal variations in surface recharge, slope angle and aquifer heterogeneity, the simulated results are expected to better reflect real conditions in natural aquifers. The effects of aquifer heterogeneity on groundwater flow and water levels are particularly significant in sloping aquifers. The study's findings indicate that even when the soil composition remains constant, variations in groundwater level and flow may be considerable, depending on factors such as soil alignment, slope angle of the aquifer's base layer and the direction of water flow.https://www.aimspress.com/article/doi/10.3934/math.20231540?viewType=HTML2d boussinesq equationheterogeneous aquiferrechargeanisotropy
spellingShingle Ming-Chang Wu
Ping-Cheng Hsieh
Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
AIMS Mathematics
2d boussinesq equation
heterogeneous aquifer
recharge
anisotropy
title Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
title_full Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
title_fullStr Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
title_full_unstemmed Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
title_short Influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
title_sort influence of nonuniform recharge on groundwater flow in heterogeneous aquifers
topic 2d boussinesq equation
heterogeneous aquifer
recharge
anisotropy
url https://www.aimspress.com/article/doi/10.3934/math.20231540?viewType=HTML
work_keys_str_mv AT mingchangwu influenceofnonuniformrechargeongroundwaterflowinheterogeneousaquifers
AT pingchenghsieh influenceofnonuniformrechargeongroundwaterflowinheterogeneousaquifers