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Article

Effects of Weir Operation on Seasonal Groundwater Use: A Case Study of the Han River, South Korea

by
Hyeonju Lee
1,
Eunhee Lee
1,
Yongcheol Kim
1,
Soo-Hyoung Lee
1 and
Min-Ho Koo
2,*
1
Groundwater Environment Research Center, Climate Change Response Division, Korea Institute of Geoscience and Mineral Resources, Daejeon 34132, Korea
2
Department of Geoenvironmental Sciences, Kongju National University, Kongju 32588, Korea
*
Author to whom correspondence should be addressed.
Water 2022, 14(4), 646; https://doi.org/10.3390/w14040646
Submission received: 11 January 2022 / Revised: 14 February 2022 / Accepted: 15 February 2022 / Published: 18 February 2022
(This article belongs to the Section Hydrogeology)
Browse Figures
Review Reports Versions Notes

Abstract

:
During the cold dry season, a large amount of groundwater is pumped for water-curtain cultivation in agricultural fields mostly located near the four major rivers of South Korea. Several weirs, installed previously to secure sufficient water resources from these rivers, were opened in 2017 for restoring the riverine environment. Weir-controlled river level fluctuations have altered stream–aquifer interactions, leading to groundwater drawdown. In this study, changes in stream–aquifer interaction caused by seasonal pumping and weir opening were investigated, using Visual MODFLOW. Two indexes that considered the pump type and aquifer characteristics—the pumping available thickness (PAT) and aquifer productivity index (API)—were used to analyze the effects of weir opening on seasonal groundwater use. Our simulations indicated that weir opening had a large impact on seasonal groundwater use due to groundwater drawdown, especially with respect to centrifugal pumps located in low transmissivity areas where the API decreased after the weir was opened. The resulting decrease in groundwater pumping rates would lower the thermal effect of the water-curtain greenhouse process. This indicates that water supply alternatives are needed so that the weirs can be operated efficiently and field requirements can be met, while the deleterious effects on groundwater are avoided.

1. Introduction

In South Korea, a significant amount of groundwater is used in many agricultural areas for ‘water-curtain cultivation’ during the cold winters. This is a facility cultivation technique, whereby relatively warm groundwater is sprayed onto greenhouse roofs for heating during the cold season. Water-curtain cultivation is mostly practiced in alluvial areas near the four major rivers, which have abundant groundwater resources. The areas involved in water-curtain cultivation have expanded recently from 39.71 km2 in 2010 to 74.09 km2 by 2017, representing an increase of approximately 87% [1]. Water-curtain cultivation comes in two forms: circulating and non-circulating systems. Non-circulating systems, which were employed in 72% of the total area under water-curtain cultivation in 2017, are mostly used in agricultural fields where the groundwater used for greenhouse heating is discharged into nearby streams [2]. Water-curtain cultivation is a useful technology which replaces the need for oil energy and brings significant economic benefits. However, it uses a lot of groundwater during the cold dry season, perhaps exceeding aquifer recharge capacity [3]. For example, the annual precipitation recharge is only 11% of the total groundwater withdrawal in large agricultural fields of Miryang [4]. This could lead to long-term groundwater depletion along with associated changes to the riverine environment [4,5]. River flows can also be affected by changes in stream–aquifer interactions in cases where they depend on groundwater discharge [6,7].
Groundwater in the agricultural areas has been affected by weir construction and river maintenance. Sixteen weirs were constructed in the four major rivers in 2012, affecting both the river environments and nearby groundwater flows, particularly in areas where many water-curtain greenhouse facilities were located. Numerous studies have been conducted on the impacts of weir construction on stream–aquifer interactions. The increased river levels caused by weir construction increased nearby groundwater levels, resulting in abundant water resources; in some areas groundwater flooding has been reported [8,9]. The presence of the weirs also decreased the seasonal influence of rainfall on river flows. It prevented flooding during the wet season and increased river flows during the dry season [10,11]. The associated river environment changes also affected groundwater flow and quality, owing to stream–aquifer interactions, which in turn affected groundwater use near the river [12,13].
It was found that restricting river flows deteriorated river water quality, adversely affecting the river ecosystem [14,15]. In response to this, nine weirs have been opened since 2017 to improve river water quality and restore aquatic ecosystems. The rivers and aquifers were monitored to assess the impact of these openings, and it was found that the increased river flows improved the water quality and environmental conditions [16,17], whereas water levels in the upstream rivers decreased. These river level declines reduced groundwater levels, and as a result, groundwater yield was also affected in some areas [18,19]. These decreased groundwater pumping rates led to some crops suffering cold damage as water-curtain greenhouse temperatures became lower in winter. In anticipation of these issues, several studies assessed how opening of the weir would affect stream–aquifer interactions, although few looked into groundwater use during the dry season [17,20].
This study aims to investigate the effect of weir operation on the stream–aquifer interactions and seasonal groundwater use for water-curtain cultivation. In this work, Yeoju greenhouse cultivation area on the riverside upstream of Ipo Weir was studied, and changes in groundwater flow and storage caused by seasonal pumping and weir operation were analyzed using Visual MODFLOW Classic (Waterloo Hydrogeologic Inc., v. 4.6.0.169, Waterloo, ON, Canada), which is a three-dimensional (3-D) finite difference model. This study considered the cases of a management level (closure of the water gate) and a minimum level (opening of the water gate) of the Ipo Weir. We also analyzed the impacts of weir operation on groundwater pumping rate and seasonal groundwater use, using two indexes that considered the pump type and aquifer characteristics. The results of this study will be helpful in establishing efficient water resource management plans by quantitatively evaluating the effects of weir opening on seasonal groundwater use. In addition, the methodology demonstrated in this study can also provide a basis for further quantifying stream–aquifer interactions affected by anthropogenic activities in other agricultural areas.

2. Materials and Methods

2.1. Study Area and Hydrogeological Setting

The study area was located on a 2.1 km2 alluvial aquifer of the Han River, in Yeoju, South Korea (Figure 1), on the plains between 127.570–127.591° E and 37.352–37.370° N surrounded by mountains. This area was selected as one where the groundwater is greatly affected by river fluctuations due to the opening of the weir, as it is located on the riverside upstream of the weir. Average rainfall and temperature measured from 1985 to 2014 were 1336 mm/year and 11.6 °C, respectively. Seasonal variations of rainfall range from 15 mm/year in February (dry season) to 402 mm/year in July (wet season) [21]. The Han River flows from south to west in the southwestern part of the study area, where its width varies from 300–800 m, and it is approximately 4 m deep on average [22]. Ipo Weir is located downstream of the study area, and it has a management level of 28 m. The Goksucheon, a tributary of the Han River, is located in the northern part of the study area. The tributary, with a width of about 45 m near the study area, originates in the mountains located in the hinterland and is discharged into the Han River. The local bedrock consists predominantly of Jurassic igneous rocks, and the sediments in the site consist of Quaternary alluvium which unconformably overlie the bedrock. This alluvium was deposited in a fluvial environment and is generally distributed along the Han River and its tributaries.
The sedimentary structure of the alluvial deposits can be seen in Figure 2. Columnar sections of the three monitoring wells located in the study area were used to analyze sedimentary layer distribution (Figure 2a). We found that the alluvium was composed of silty sand and weathered soil (Figure 2b). The surface elevation at the site varied from 36–43 m, average thickness of the silty sand layer was 13.5 m, and the weathered soil layer was 1.5 m thick. Groundwater was located in the silty sand layer, which was connected to the river.
The study area was characterized by greenhouse cultivation areas, which produce crops of sweet potato, cucumber, eggplant, and pumpkin using the water-curtain cultivation technique during winter. Out of the 348 pumping wells in the study area, we found that 273 were used for water-curtain cultivation (Figure 2a). Centrifugal pumps that pull water up from the land surface and underwater pumps that are used submerged in the well were installed in 93 and 252 pumping wells, respectively (with 3 unidentified wells). The study area was considered to be a typical representative of water-curtain greenhouse cultivation areas near rivers in South Korea.

2.2. Numerical Model

Groundwater flow steady-state simulations were carried out using Visual MODFLOW, a 3-D finite-difference flow model to analyze changes in stream–aquifer interaction following the opening of the weir. The study area is close to 1.4 km from the river and shows a relatively high transmissivity of 642 m2/day compared to the average value of South Korea as a result of the groundwater pumping test [24,25], which means that a new equilibrium state is quickly reached after a hydraulic stress is applied [26,27]. Therefore, the steady-state simulations were performed to simplify the model and compare the stream–aquifer interactions in an equilibrium state before and after the weir operation.
Figure 3 shows the model domain, in which a 20 × 20 m grid was used, covering a 7.8 × 6.4 km area divided into 320 rows and 390 columns. Figure 3a,b show the boundary conditions and spatial distribution of model properties (hydraulic conductivity), respectively. The model domain was designed to include adjacent areas with similar sedimentary structures, because of a scarcity of field data, and topographic limits of hinterland, to minimize boundary uncertainty, including the study area. The sedimentary structure of the alluvial deposits was reflected in the model by applying columnar section data from eight monitoring wells. The model was discretized vertically into three layers, with the upper layer consisting of silty sand, the second layer made up of weathered soil, and the lower layer composed of granite (Figure 2). The top surface elevation of the model was assigned using a digital elevation model (DEM) with the columnar section data, and the bottom elevation of the lower layer was set at a constant 0 m.
The Han River was represented as constant head boundary (Dirichlet condition) because the water level remains constant due to the management level of the weir, and the riverbed and aquifer are well connected (Figure 3a). River levels were set to either the Ipo Weir management level (28 m) or minimum level (25.3 m). The Goksucheon tributary was set as an upper layer river boundary (Cauchy condition) in order to reflect the small rivers where river flow is affected by rainfall. In the river boundary, water flows in direct proportion to the head difference between the river and groundwater levels, and a certain amount of river water flows into the aquifer when the groundwater level is lower than the riverbed. Its water levels were set to values between 27.5–41.0 m, considering both the observed river level and surface altitude, and the river depth was set to 0.5 m. The hinterland was represented by a general head boundary (Cauchy condition) to represent groundwater inflow from mountainous areas, and conductance of both the riverbed and the hinterland were calibrated. In this boundary condition, like the groundwater flow in a high mountain, an infinite flow occurs in proportion to the water level difference with the surrounding groundwater level. Water levels of the general head boundary were set to values between 28.5–50.0 m, considering both the surface altitude and groundwater level contour map estimated by kriging with observation data in 2015, when the only observation data for the hinterland exists [21]. The groundwater recharge rate, which was calculated using average precipitation (1336 mm/year) and recharge factor (0.19) data for the study area [21], was set at 258 mm/year and was applied to the top layer of the model. The hydraulic conductivity of the upper layer, which was estimated using a pumping test [24], was set to 44 m/day, while the hydraulic conductivities of the second and lower layers were calibrated (Figure 3b).
There were 819 pumping wells in the model domain, which were classified based on their use. Out of the wells, 583 were for agricultural use, 223 for living, and 13 for other uses. Daily pumping rates were calculated using the equations for estimating groundwater use according to the purpose of use, which is presented in [28], and annual groundwater use in 2018 [29]. The estimated total pumping rates were 886 m3/day for agricultural use, 258 m3/day for living, and 227 m3/day for other uses, as noted in Table 1. During the seasonal pumping period, the daily pumping rate for each water-curtain cultivation was set to 15 m3/day for 372 groundwater pumping wells out of the 431 wells used for gardening. This pumping rate for water-curtain cultivation was estimated using the average yearly groundwater use by each water-curtain greenhouse (62 m3/day) [30] and the pumping period (90 days).
The model was calibrated using trial and error, with model parameters adjusted until the fit between model outputs and observations was acceptable. Calibration involved changing hydraulic conductivity input values for the weathered and bedrock layers (second and lower layers), and the conductance of the hinterland and Goksucheon tributary. Calibration was achieved by matching the calculated heads with groundwater data obtained from 13 monitoring wells when the river level was at the management level of the Ipo Weir (Figure 3a). Average annual groundwater levels from 5 wells out of the 13 wells were used, while the average value observed in August 2019 was used for the groundwater level in 8 wells out of the 13 wells because of the lack of observation data.
Several trial and error simulations revealed that an acceptable fit was obtained between the observed and simulated heads when the hydraulic conductivity values were 8.6 m/day for the weathered layer (second layer) and 0.3 m/day for the bedrock (lower layer) (Table 2). The final calibrated hinterland conductances were 20 m2/day and 50 m2/day for the bedrock and alluvium, respectively, while the calibrated conductance of the Goksucheon was 10 m2/day. The agreement between the calculated and measured heads and the distribution of the calculated groundwater levels can be seen in Figure 4. The root mean square error (RMSE) and the normalized root mean square error (NRMSE) between the observed and calculated heads were 0.88 m and 6.3% (Figure 4a), respectively, which indicates that the simulated heads matched the observed values reasonably well [31]. Average annual groundwater level showed groundwater was introduced from the hinterland and discharged into the river, showing a distribution similar to the observation data (Figure 4b).

2.3. Pumping Available Thickness and Aquifer Productivity Index

Groundwater levels were analyzed to investigate changes in the groundwater flow system caused by seasonal pumping for water-curtain cultivation and weir operations. Areas in which crop cultivation was affected by decreased groundwater pumping rates were analyzed using predicted groundwater levels. Two indexes that considered pump type and aquifer characteristics—pumping available thickness (PAT) and aquifer productivity index (API)—were used to analyze the effects of the opening of the weir on groundwater pumping from the wells.
In centrifugal pumps, groundwater from depths of up to 8 m can be pumped, depending on the suction height capability of the pump. Therefore, groundwater depth from the surface can be used to evaluate the impact of opening the weir on groundwater use in centrifugal pumps. In this study, the minimum PAT from the water table to the critical depth (8 m) was assumed to be 1 m, considering not only the greatest decrease in well water levels due to the cone of depression, but also well loss. In other words, groundwater was considered to be depleted, and could not be pumped by centrifugal pumps, if the PAT values were less than 1 m. The PAT values were calculated using the groundwater level estimated in the model.
In addition, because specific capacity decreases in proportion to transmissivity, the API was applied to show how groundwater pumping rates relatively decreased after opening the weir. The API was calculated as follows:
API = T 2 T 1
where T 1 and T 2 stand for transmissivities before and after opening the weir, respectively. The model assumes that crop cultivation will be damaged due to decreased groundwater pumping rates if the API decreases to 0.8, considering the cone of depression in the wells. This meant that the specific capacity was reduced by 20% owing to the opening of the weir, although actual well pumping rates varied greatly depending on the performance characteristics of individual pumps. The API values were calculated using the hydraulic conductivity of each layer and the groundwater level estimated in the model.

3. Results and Discussion

3.1. Impacts of Opening of the Weir on Stream–Aquifer Interactions

Our model results showed that water level fluctuations played an important role in stream–aquifer interactions, which is consistent with the previous research results [32,33]. Figure 5 and Figure 6 show the spatial variations in groundwater levels and drawdown resulting from opening the weir, which were presented by kriging with calculated values from calibrated model. During the non-seasonal pumping period (Figure 5), the groundwater level was higher than the river level, showing a gaining stream (Figure 5a), while once the river level decreased, the groundwater level fell near the river by approximately 2.7 m (Figure 5b). This groundwater drawdown decreased with distance from the river (Figure 5c).
During the seasonal pumping period (Figure 6), the groundwater level fell and cones of depression formed in areas where there were numerous groundwater pumping wells used for water-curtain cultivation (Figure 6a). In these depression areas, the groundwater level decreased below the weathered soil layer after the opening of the weir, which means that transmissivity also decreased (Figure 6b,c). Overall, we were able to conclude that changes in river level due to the opening of the weir had a greater impact during the seasonal pumping period, because the groundwater levels changed even more when the effect of groundwater pumping and river level decline were combined.
The simulated water balance indicated that, after the river level had decreased, groundwater discharge from the aquifer to the Han River increased by 72%, while discharge to the tributary decreased by 4%. In winter, groundwater pumping accounted for 72% of the total groundwater recharge, and the opening of the weir increased the groundwater discharge to the Han River by 30%. The hydrological condition of the tributary changed from a gaining to a losing stream, which could have strongly affected the quantity and quality of both groundwater and tributary surface water [34,35,36].

3.2. Changes in Groundwater Pumping Rate

Groundwater storage losses can affect groundwater use, with the impact depending on the type of pump used. Groundwater pumping rate changes due to the API depend on the performance characteristics of the pump, and it can be seen in Figure 7 how the pump system curve changed with declining groundwater level after opening the weir. The figure also shows the head generated by the pump over a range of pumping rates, including its efficiency and brake horsepower [37]. The pump system curve depicts the relationship between the head pressure and pumping rates for an actual pump [38].
In the figure, it can be seen that the system curve (operation point) moves up with declining groundwater level ( Δ H W ) after opening the weir (❶); consequently, the groundwater pumping rates decrease. The magnitude of decrease in transmissivity with groundwater drawdown increases the system curve inclination (❷), decreasing pumping rates.
As groundwater drawdown is proportional to groundwater pumping rates, the system curve for the actual lift shows a linear change. However, groundwater pumping rates in actual wells increase nonlinearly with the head pressure due to frictional head losses. The inclination of the system curve, that is, the ratio of pumping rates and groundwater drawdown, decreases with aquifer productivity, that is, transmissivity. The intersection point between the pump performance curve and pump system curve is the operation point, which determines the pumping rate and groundwater level.
Figure 8 shows how groundwater pumping rate changed depending on the type of pump with declining groundwater level after opening the weir. Figure 8a includes performance curves for centrifugal (PH-750W (HANIL Electric Co, Bucheon, Korea)) and underwater (SR4M-0322 (HANIL Electric Co, Bucheon, Korea)) pumps and Figure 8b illustrated pumping rate changes caused by the groundwater drawdown that followed the opening of the weir; they show how the groundwater pumping rates decreased as the groundwater level declined due to opening of the weir, without a change in API (API = 1). With decreasing groundwater level, the pumping rates achieved by centrifugal pumps decreased by a greater magnitude than those achieved by underwater pumps (Figure 8a). It can be seen that the drawdown caused the rates to decrease linearly (Figure 8b). The pumping rates achieved by the centrifugal and underwater pumps decreased by 16% and 2% (Q/Q0 = 0.86 and 0.98), respectively, after the groundwater level decreased by 8 m, following the opening of the weir.
Figure 8c,d show the difference in groundwater pumping rates between the centrifugal pump and underwater pump, with API changes caused when the groundwater level decreased by 4 m after opening the weir. The smaller the transmissivity, the lower the groundwater pumping rate. In the aquifer with a transmissivity of 10 m2/day, the groundwater pumping rates achieved by the centrifugal pump decreased by 43% compared to those before the weir was opened when the API decreased to 0.2 (Figure 8c). On the other hand, the pumping rates achieved by the underwater pump decreased by just 12% under the same conditions (Figure 8d). Consequently, we could see that groundwater would deplete more in areas where centrifugal pumps were used and the transmissivities were low after the decline in groundwater levels and the API due to the opening of the weir.

3.3. Effects of Opening of the Weir on Seasonal Groundwater Use

The areas in which groundwater pumping was difficult using centrifugal pumps were analyzed with respect to the PAT value, and the modeling results obtained when spatial and temporal PAT value variations were applied can be seen in Figure 9. During non-seasonal pumping period, the groundwater could not be accessed by centrifugal pumps in high surface altitude areas at the management level of the Ipo Weir (Figure 9a). The depletion area increased from 0.13 to 0.29 km2 after opening the weir, and the number of depleted wells increased from 7 to 12 out of the 93 applicable wells in the study area (Table 3 and Figure 9b).
During the seasonal pumping period, depletion began in the central 0.66 km2 area of the study site, where several groundwater pumping wells for water-curtain cultivation were located (Figure 9c); it expanded to 1.04 km2 after the weir was opened (Figure 9d). At this time, the number of depleted wells increased from 54 to 72 due to opening of the weir (Table 3). It was predicted that groundwater pumping rates would also decrease outside the depleted area because the operating abilities of the centrifugal pumps were significantly affected by groundwater drawdown.
In Figure 10, it can be seen how aquifer productivity was reduced after the weir was opened. Any area with API values of less than 0.8 can be regarded as being an area in which crop cultivation will be damaged due to decreased groundwater pumping rates. Specific capacity usually decreased near the river during the non-seasonal pumping period (Figure 10a), where the minimum API was estimated at 0.41, and 61 groundwater wells were contained in the area that had an API ≤0.8 (Table 4). During the seasonal pumping period, this area expanded, with the minimum API reaching 0 in areas where numerous groundwater pumping wells for water-curtain cultivation were located (Figure 10b). At this time, the specific capacity of 234 groundwater pumping wells was reduced by >20% (Table 4). Based on both PAT and API indexes, groundwater pumping rates in most of the study area decreased, which is expected to significantly reduce the thermal benefit applied to water-curtain greenhouses by groundwater pumping [39,40].
Water supply alternatives are needed if weirs are to be operated efficiently in areas concerned with difficult groundwater use. Countermeasures—which could include using alternative pumping wells, managed aquifer recharge (MAR), and surface water—should be established in the field by investigating groundwater levels and use.
Using alternative pumping wells, the most effective countermeasure, could restore the total amount of groundwater use levels before the opening of the weir, although the possibility of local groundwater depletion occurring in some areas cannot be ignored. Therefore, the sustainable development yield and the impact of alternative pumping wells on groundwater should be evaluated. The MAR option could lead to additional groundwater availability, especially in areas where the API has been significantly decreased due to the opening of the weir or areas where groundwater use has exceeded the sustainable development yield. Successful MAR, which requires feasibility evaluation, including identifying methods suited to regional hydrological characteristics, should be performed together with quantitative analysis of the managed aquifer recharge effect. Lastly, surface water can be used as an alternative water source in areas with groundwater depletion where alternative well development would be difficult.

4. Summary and Conclusions

Water-curtain cultivation areas are located mostly on alluvium near the four major rivers in South Korea, where groundwater levels can be directly influenced by river level variations, including those brought about by weir operations. The effect of Ipo Weir opening on stream–aquifer interactions and seasonal groundwater use have been analyzed using numerical simulations, and the resulting conclusions have been summarized below.
Our modeling predicted that opening of the weir led to changes in the stream–aquifer interaction with the groundwater flow system. A decline in river level due to opening of the weir led to groundwater drawdown, especially in areas where large amounts of groundwater were used. Changes in groundwater flow affected the hydrological conditions of the adjacent river tributary, decreasing groundwater discharge by 4%, to the extent that its ecosystem could have been affected by the decreased river flows. In water-curtain cultivation areas, where the groundwater level is reduced below that of the river level, opening of the weir leads to a decrease in the induced groundwater recharge, increasing groundwater discharge by 30%.
Opening of the weir had significant impacts on seasonal groundwater use for water-curtain cultivation. Groundwater pumping rates decreased with the change in the aquifer transmissivity caused by groundwater drawdown, and the areas where the groundwater could not be pumped increased during the seasonal pumping period. Locations where difficulty was experienced by groundwater users in operating centrifugal pumps were first seen in the central part of study area, while groundwater pumping rates by underwater pumps were affected by the largest magnitude near the river. The areas where the groundwater could not be accessed by centrifugal pumps increased by 1.6 times after opening the weir, and as a result, the depleted wells increased by 1.3 times. At this time, the specific capacity in wells, equivalent to 64% of all wells, was reduced by 20%. Consequently, groundwater use was most likely affected in low transmissivity areas where the API decreased after the weir was opened, especially with respect to centrifugal pumps. The decreased groundwater pumping rates could also lower the thermal effect of water-curtain greenhouses in winter, thus reducing crop cultivation efficiency. This indicates that water supply alternatives such as alternative pumping wells, MAR, and surface water are needed so that the weirs can be operated efficiently and field requirements can be met, while the deleterious effects on groundwater can be avoided.
The results of this research can be useful to predict the changes to groundwater systems caused by seasonal pumping and opening of the weir in South Korean greenhouse cultivation areas, thus providing a means of establishing strategies for more efficient water resource management.

Author Contributions

Conceptualization, H.L., E.L., Y.K. and M.-H.K.; investigation, H.L., E.L. and S.-H.L.; data analysis, H.L.; methodology, H.L., E.L. and M.-H.K.; writing—original draft, H.L. and M.-H.K.; writing—review and editing, H.L., E.L., Y.K., S.-H.L. and M.-H.K.; project administration, Y.K.; supervision, Y.K. and M.-H.K. All authors have read and agreed to the published version of the manuscript.

Funding

This research was funded by Korea Ministry of Science and ICT (MSIT): Basic Research Project (GP2020-012) of the Korea Institute of Geoscience and Mineral Resources (KIGAM), and Korea Ministry of Environment (MOE): Research Project (IP2019-009).

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

Not applicable.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Location and geology of the study area in Han River Basin, South Korea (modified from [23]).
Figure 1. Location and geology of the study area in Han River Basin, South Korea (modified from [23]).
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Figure 2. (a) Location of pumping wells with cross-section line and (b) generalized geological cross-section showing sedimentary structure of the alluvial deposits analyzed using columnar sections of the three monitoring wells (black lines).
Figure 2. (a) Location of pumping wells with cross-section line and (b) generalized geological cross-section showing sedimentary structure of the alluvial deposits analyzed using columnar sections of the three monitoring wells (black lines).
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Figure 3. (a) Conceptual model showing boundary conditions and locations of 13 monitoring wells (circles) with the study area near the river (polygon) and (b) spatial distribution of hydraulic conductivity.
Figure 3. (a) Conceptual model showing boundary conditions and locations of 13 monitoring wells (circles) with the study area near the river (polygon) and (b) spatial distribution of hydraulic conductivity.
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Figure 4. Calibration results: (a) comparisons between calculated and measured groundwater levels; (b) calculated groundwater level distributions.
Figure 4. Calibration results: (a) comparisons between calculated and measured groundwater levels; (b) calculated groundwater level distributions.
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Figure 5. Changes in calculated groundwater levels due to opening of the weir during the non-seasonal pumping period, when the river level is (a) at the Ipo Weir management level (28 m), (b) at the minimum weir level (25.3 m), and (c) groundwater drawdown.
Figure 5. Changes in calculated groundwater levels due to opening of the weir during the non-seasonal pumping period, when the river level is (a) at the Ipo Weir management level (28 m), (b) at the minimum weir level (25.3 m), and (c) groundwater drawdown.
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Figure 6. Changes in calculated groundwater levels due to opening of the weir during the seasonal pumping period, when the river level is (a) at the Ipo Weir management level (28 m), (b) at the minimum weir level (25.3 m), and (c) groundwater drawdown.
Figure 6. Changes in calculated groundwater levels due to opening of the weir during the seasonal pumping period, when the river level is (a) at the Ipo Weir management level (28 m), (b) at the minimum weir level (25.3 m), and (c) groundwater drawdown.
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Figure 7. Change in the pump system curve owing to the decline in groundwater level (❶), decrease in transmissivity (❷) experienced after opening the weir, and frictional head losses (sky blue dashed line).
Figure 7. Change in the pump system curve owing to the decline in groundwater level (❶), decrease in transmissivity (❷) experienced after opening the weir, and frictional head losses (sky blue dashed line).
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Figure 8. (a) Pump performance curves for centrifugal-type (PH-750W) and underwater-type (SR4M-0322) pumps; changes in pumping rates due to the decline in groundwater level after opening the weir: (b) without a change in API (API = 1); and due to a decreased API at (c) the centrifugal pump, and (d) the underwater pump.
Figure 8. (a) Pump performance curves for centrifugal-type (PH-750W) and underwater-type (SR4M-0322) pumps; changes in pumping rates due to the decline in groundwater level after opening the weir: (b) without a change in API (API = 1); and due to a decreased API at (c) the centrifugal pump, and (d) the underwater pump.
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Figure 9. Areas where groundwater pumping by centrifugal pump was difficult, incorporating the spatial variation of PAT values less than 1 m (shaded area) with river levels during (a,b) non-seasonal pumping; (c,d) seasonal pumping, at (a,c) the Ipo Weir management level (28 m), and (b,d) at the minimum weir level (25.3 m).
Figure 9. Areas where groundwater pumping by centrifugal pump was difficult, incorporating the spatial variation of PAT values less than 1 m (shaded area) with river levels during (a,b) non-seasonal pumping; (c,d) seasonal pumping, at (a,c) the Ipo Weir management level (28 m), and (b,d) at the minimum weir level (25.3 m).
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Figure 10. Areas in which aquifer productivity decreased due to opening of the weir, incorporating spatial variations of API values less than 0.8 (shaded area), during (a) non-seasonal and (b) seasonal pumping periods.
Figure 10. Areas in which aquifer productivity decreased due to opening of the weir, incorporating spatial variations of API values less than 0.8 (shaded area), during (a) non-seasonal and (b) seasonal pumping periods.
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Table
Table 1. Estimated groundwater pumping rates (m3/day).
Table 1. Estimated groundwater pumping rates (m3/day).
ClassificationNumber of WellsPumping RatesTotal Pumping Rates
Agricultural useField crop
(non-rice)		734478861371
Rice field79250
Gardening431189
LivingHousehold200160258
General purpose2286
School112
Other usesIndustrial use6192227
Others735
Table
Table 2. Hydraulic parameter values used in the model.
Table 2. Hydraulic parameter values used in the model.
Alluvium
Upper UnitMiddle UnitBedrockRiverbed
Hydraulic conductivity (m/day)448.60.3-
Conductance of boundary (m2/day)502010
Table
Table 3. Number of centrifugal pumps that became ineffective due to the opening of the weir (PAT ≤ 1).
Table 3. Number of centrifugal pumps that became ineffective due to the opening of the weir (PAT ≤ 1).
River Water Level (m)Area (km2)Number of Centrifugal Pumps
Non-seasonal pumping period280.137
25.30.2912
Seasonal
pumping period		280.6654
25.31.0472
Table
Table 4. Number of groundwater pumping wells experiencing difficulty due to the opening of the weir (API ≤ 0.8).
Table 4. Number of groundwater pumping wells experiencing difficulty due to the opening of the weir (API ≤ 0.8).
PeriodArea (km2)Number of Groundwater Pumping Wells (API ≤ 0.8)
Centrifugal PumpUnderwater PumpUnidentified Pump Type Total
Non-seasonal pumping period0.48754061
Seasonal
pumping period		1.02461862234
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Lee, H.; Lee, E.; Kim, Y.; Lee, S.-H.; Koo, M.-H. Effects of Weir Operation on Seasonal Groundwater Use: A Case Study of the Han River, South Korea. Water 2022, 14, 646. https://doi.org/10.3390/w14040646

AMA Style

Lee H, Lee E, Kim Y, Lee S-H, Koo M-H. Effects of Weir Operation on Seasonal Groundwater Use: A Case Study of the Han River, South Korea. Water. 2022; 14(4):646. https://doi.org/10.3390/w14040646

Chicago/Turabian Style

Lee, Hyeonju, Eunhee Lee, Yongcheol Kim, Soo-Hyoung Lee, and Min-Ho Koo. 2022. "Effects of Weir Operation on Seasonal Groundwater Use: A Case Study of the Han River, South Korea" Water 14, no. 4: 646. https://doi.org/10.3390/w14040646

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