Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan

The landforms and human activities play important roles in quantifying surface water and groundwater interactions (SGIs) for water resources management. The study uses the groundwater and surface-water FLOW model (GSFLOW) model to quantify the dynamics of SGIs in the Pingtung Plain groundwater basin...

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Main Authors: Quoc-Dung Tran, Chuen-Fa Ni, I-Hsien Lee, Minh-Hoang Truong, Chien-Jung Liu
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/10/20/7152
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spelling doaj-4debed3dd3e448b1a049d5fdf69b68e02020-11-25T04:00:26ZengMDPI AGApplied Sciences2076-34172020-10-01107152715210.3390/app10207152Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, TaiwanQuoc-Dung Tran0Chuen-Fa Ni1I-Hsien Lee2Minh-Hoang Truong3Chien-Jung Liu4Graduate Institute of Applied Geology, National Central University, Taoyuan City 32001, TaiwanGraduate Institute of Applied Geology, National Central University, Taoyuan City 32001, TaiwanGraduate Institute of Applied Geology, National Central University, Taoyuan City 32001, TaiwanDepartment of Geology, University of Science Ho Chi Minh City, Ho Chi Minh City 700000, VietnamInstitute of Water Resources Development, Feng Chia University, Taichung City 40724, TaiwanThe landforms and human activities play important roles in quantifying surface water and groundwater interactions (SGIs) for water resources management. The study uses the groundwater and surface-water FLOW model (GSFLOW) model to quantify the dynamics of SGIs in the Pingtung Plain groundwater basin (PPGB) in southern Taiwan. Specifically, the study uses a physical-based numerical model to quantify the spatial and seasonal variations of water cycles influenced by complex fluvial landform conditions and human activities. Results of the model calibrations show good agreement with the data obtained from the available groundwater monitoring network and the selected stream stations. The basin-scale water budgets show highly nonuniform precipitation in the study area, and over 80% annual precipitation is from wet seasons in the PPGB. With high permeable surficial deposits in the PPGB, the year-averaged surface runoff and infiltration are approximately 57% and 40% of the total precipitation. The fluvial landforms with the high slope in the PPGB lead to 70% of annual surface runoff that becomes the streamflow, and the interflow dominates water interactions near streambeds. Results show that the interflow rate in the wet seasons is 200% more than that in the dry seasons. The net groundwater discharge to the streams is relatively small as compared to the interflow. Only 10% of the river flow is from the net groundwater discharge. In the PPGB, The pumping-induced variations of groundwater levels are insignificant as compared with the factor of the natural landforms. Because of the relatively small area of the proposed artificial lake, the contribution of the artificial lake on the local water budgets is insignificant, indicating the low impact of the artificial recharge lake on the surface water environment.https://www.mdpi.com/2076-3417/10/20/7152GSFLOWsurface water and groundwater interactionnumerical modelartificial lakewater budgets
collection DOAJ
language English
format Article
sources DOAJ
author Quoc-Dung Tran
Chuen-Fa Ni
I-Hsien Lee
Minh-Hoang Truong
Chien-Jung Liu
spellingShingle Quoc-Dung Tran
Chuen-Fa Ni
I-Hsien Lee
Minh-Hoang Truong
Chien-Jung Liu
Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
Applied Sciences
GSFLOW
surface water and groundwater interaction
numerical model
artificial lake
water budgets
author_facet Quoc-Dung Tran
Chuen-Fa Ni
I-Hsien Lee
Minh-Hoang Truong
Chien-Jung Liu
author_sort Quoc-Dung Tran
title Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
title_short Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
title_full Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
title_fullStr Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
title_full_unstemmed Numerical Modeling of Surface Water and Groundwater Interactions Induced by Complex Fluvial Landforms and Human Activities in the Pingtung Plain Groundwater Basin, Taiwan
title_sort numerical modeling of surface water and groundwater interactions induced by complex fluvial landforms and human activities in the pingtung plain groundwater basin, taiwan
publisher MDPI AG
series Applied Sciences
issn 2076-3417
publishDate 2020-10-01
description The landforms and human activities play important roles in quantifying surface water and groundwater interactions (SGIs) for water resources management. The study uses the groundwater and surface-water FLOW model (GSFLOW) model to quantify the dynamics of SGIs in the Pingtung Plain groundwater basin (PPGB) in southern Taiwan. Specifically, the study uses a physical-based numerical model to quantify the spatial and seasonal variations of water cycles influenced by complex fluvial landform conditions and human activities. Results of the model calibrations show good agreement with the data obtained from the available groundwater monitoring network and the selected stream stations. The basin-scale water budgets show highly nonuniform precipitation in the study area, and over 80% annual precipitation is from wet seasons in the PPGB. With high permeable surficial deposits in the PPGB, the year-averaged surface runoff and infiltration are approximately 57% and 40% of the total precipitation. The fluvial landforms with the high slope in the PPGB lead to 70% of annual surface runoff that becomes the streamflow, and the interflow dominates water interactions near streambeds. Results show that the interflow rate in the wet seasons is 200% more than that in the dry seasons. The net groundwater discharge to the streams is relatively small as compared to the interflow. Only 10% of the river flow is from the net groundwater discharge. In the PPGB, The pumping-induced variations of groundwater levels are insignificant as compared with the factor of the natural landforms. Because of the relatively small area of the proposed artificial lake, the contribution of the artificial lake on the local water budgets is insignificant, indicating the low impact of the artificial recharge lake on the surface water environment.
topic GSFLOW
surface water and groundwater interaction
numerical model
artificial lake
water budgets
url https://www.mdpi.com/2076-3417/10/20/7152
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