• Title/Summary/Keyword: groundwater change

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Prediction of Groundwater Level in Chojung Area (초정지역의 지하수 유동해석)

  • 안상도;김경호;정영훈
    • Journal of the Korean Society of Groundwater Environment
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    • v.7 no.3
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    • pp.133-140
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    • 2000
  • The area of Chojung is famous for its mineral water quality. Because of this reason, massive groundwater development was induced in the area. As a result of excessive pumping. the depletion of the groundwater resources is expected seriously. This study was conducted to analyse groundwater flow in Chojung using a numerical model. Simulation results show the groundwater level change slowly in the mountain area but steep groundwater drawdown occurred in the pumping area in the downstream. This steep groundwater drawdown is due to excessive pumping in the hilly region. Because of this excessive, desiccation of water resources were predicted and proper countermeasure is in great demand.

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Analysis of Groundwater Level Changes Near the Greenhouse Complex Area Using Groundwater Monitoring Network (지하수관측망을 이용한 강변 시설재배지역 지하수위 변화 특성 분석)

  • Baek, Mi Kyung;Kim, Sang Min
    • Journal of The Korean Society of Agricultural Engineers
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    • v.64 no.6
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    • pp.13-23
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    • 2022
  • The purpose of this study was to analyze the impact of greenhouse cultivation area and groundwater level changes due to the water curtain cultivation in the greenhouse complexes, which are mainly situated along rivers where water resources are easy to secure. The groundwater observation network in Miryang, Gyeongsangnam-do, located downstream of the Nakdong River, was selected for the study area. We classified the groundwater monitoring well into the greenhouse (riverside) and field cultivation areas (plain and mountain) to compare the groundwater impact of water curtain cultivation in the greenhouse complex. The characteristics of groundwater level changes classified by terrain type were analyzed using the observed data. Riverside wells have significant permeability coefficients and are close to rivers, so they are greatly affected by river flow and precipitation changes so that water level shows a specific pattern of annual changes. Most plain wells do not show a constant annual change, but observation wells near small rivers and small-scale greenhouse cultivation areas sometimes show annual and daily changes in which the water level drops during winter. Compared to other observation wells, mountain wells do not show significant yearly changes in water level and show general characteristics of bedrock aquifer well with a low permeability coefficient.

Development of a Groundwater Source Heat Pump in a Fractured Rock Aquifer (암반 대수층에서 개방형 지열 시스템의 개발 및 적용)

  • Shim, Byoung Ohan;Kim, Seong-Kyun;Choi, Hanna;Lee, Soo-Hyoung;Ha, Kyoochul;Kim, Yongchul
    • New & Renewable Energy
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    • v.17 no.3
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    • pp.32-41
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    • 2021
  • A groundwater source heat pump (GWHP) was developed in this study by adapting a borehole heat exchanger with closed-loop and open-loop systems in a new building. In the pilot test building, the air-conditioning on the second floor was designed to employ a closed-loop system and that on the third floor had an open-loop system. The GWHP design is based on the feasibility of groundwater resources at the installation site. For the hydrogeological survey of the study site, pumping and injection tests were conducted, and the feasibility of GWHP installation was evaluated based on the air-conditioning load demand of the building. The site was found to be satisfactory for the design capacity of the thermal load and water quality. In addition, the effect of groundwater movement on the performance of the closed-loop system was tested under three different operational scenarios of groundwater pumping. The performance of the system was sustainable with groundwater flow but declined without appropriate groundwater flow. From long-term observations of the operation, the aquifer temperature change was less than 2℃ at the observation well and 5℃ at the injection well with respect to the initial groundwater temperature. This pilot study is expected to be of guidance for developing GWHPs at fractured rock aquifers.

Development of vulnerable period assessment method for efficient groundwater resources management in upstream of Nakdong river basin using entropy method (엔트로피 방법을 이용한 낙동강 상류 지역의 지하수자원 관리 취약시기 평가 방법 개발)

  • Kim, Il Hwan;Lee, Jae-Beom;Yang, Jeong-Seok
    • Journal of Korea Water Resources Association
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    • v.51 no.9
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    • pp.761-768
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    • 2018
  • Groundwater resources are becoming depleted due to climate change factors and non climate change factors. In order to effectively groundwater resources management, we developed a method for evaluating vulnerable periods of groundwater resource management in watershed areas. The watershed based vulnerability assessment was conducted independently of the evaluation of vulnerable areas and vulnerable periods for sub watersheds. The vulnerable area evaluation index was standardized and applied to the independent vulnerable period index each region. It was applied to Bonghwa-gun, Andong-si, Yecheon-gun, Mungyeong-si and Sangju-si in the upstream of the Nakdong river basin. As a result, the Sangju-si's August was the most vulnerable at 0.278, and Andong-si was assessed to be vulnerable to groundwater resource management during 8 months of the year in study area. Using the developed method, we can find efficient management method considering the time and regional of groundwater resources.

U.S.'s Patent Network Analysis and Technology Trends on Underground Water for the Response of Climate Change (기후변화 대응을 위한 미국 지하수 기술 특허네트워크 분석과 주요 특허 기술 동향)

  • Yoon, Soon-Uk;Choi, Hanna;Kim, Minchul
    • Journal of Energy Engineering
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    • v.28 no.3
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    • pp.55-64
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    • 2019
  • This study identified key patents on U.S. underground water technology through patent network analysis. As a result, there were many technologies that used the technology to remove heavy metals to prevent contamination of groundwater. While patents between groundwater technology patents were in charge of intermediaries, the connectivity between groundwater technologies is not high. The patented technologies related to groundwater were largely distinguishable by pumping, monitoring, and decontamination. Monitoring includes techniques that enable identification of physical and biological properties, such as the type of contaminants, as well as geographic characteristics for analysis of groundwater flow, flow or water quality. Pollution purification technology refers to the process of physiochemical and biological purification for soil and groundwater. U.S. technology cases showed that the U.S. had high technology in water treatment area. And patent protection were also needed to cope with water shortages caused by climate change.

Saltwater Intrusion Monitoring Evaluation through Automatic Vertical Line Method in a Costal Aquifer of the Eastern Part of Jeju Island (수직 라인 관측시스템을 이용한 제주 동부 해안대수층에서 해수침투 모니터링 평가)

  • Jang, Hojune;Ha, Kyoochul;Hwang, Inuk;Kim, Gee-Pyo;Park, Won-Bae
    • Journal of Soil and Groundwater Environment
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    • v.26 no.3
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    • pp.1-13
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    • 2021
  • Groundwater monitoring is commonly practiced with real-time sensors placed in several depth spots in aquifer. However, this method only provides monitoring data at the point where the sensors are installed. In this study, we developed a vertical line monitoring system (VLMS) that can provide continuous data of groundwater parameters along the vertical depth. The device was installed in a well located on the coast of the eastern part of Jeju island to monitor electrical conductivity, temperature, salinity, pH, dissolved oxygen, and oxidation-reduction potential over approximately 3 months from September 11 to December 3, 2020. The results indicated that the groundwater levels fluctuated with the tidal change of seawater level, and the upper and lower boundaries of the freshwater and saltwater zone in the groundwater were located at below 16 m and 36 m of mean sea level, respectively. There was a large variation in EC values during the high tide and temperature change was the greatest during flow tide. Although further investigation is needed for improvement of the device to obtain more accurate and reliable data, the device has a potential utility to provide fundamental data to understand the seawater intrusion and transport mechanisms in coastal aquifers.

Groundwater Use and Its Perspective in Haean Basin, Yanggu County of Gangwon Province (강원도 양구군 해안분지의 지하수 사용과 전망)

  • Lee, Jin-Yong;Han, Jiwon
    • Journal of Wetlands Research
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    • v.15 no.2
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    • pp.179-189
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    • 2013
  • The Haean basin is a unique geographical feature formed by differential erosion and it borders the military demarcation line. Recently the basin has become an interest of civilians due to security tour, highland vegetables and wetland. After the civil war, the population decreased but it has increased since 2007. The annual mean air temperature in the basin has increased with a rate of $+0.016^{\circ}C/yr$ and the annual precipitation also has increased with a rate of +10.41 mm/yr. The precipitation occurring in June~August (wet season) occupied most of the total precipitation increase. In addition, recently the number of groundwater wells and its use have gradually increased and most of them are for agriculture including cultivation of rice and highland vegetables. If the air temperature further increases in the future according to the climate change scenarios, the highland vegetables cultivation will be difficult. Furthermore, if the rainstorm in the summer will be enforced, the groundwater recharge and water management will be aggravated. Therefore, an evaluation for sustainable groundwater development in the basin and a reform of the current agriculture (change of cultivating crops) depending on much water are essentially required.

Assessment of Future Climate Change Impact on Groundwater recharge, Baseflow and Sediment in Steep Sloping Watershed (미래 기후변화에 따른 급경사지 유역에서의 지하수 함양, 기저유출 및 토양유실 평가)

  • Lee, Ji Min;Jung, Younghun;Park, Younshik;Kang, Hyunwoo;Lim, Kyoung Jae;Kim, Hungsoo
    • Journal of Wetlands Research
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    • v.16 no.2
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    • pp.173-185
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    • 2014
  • Climate change has caused detrimental phenomena such as heavy rainfall which could aggravate soil erosion. Accordingly, it is needed to evaluate the groundwater recharge, baseflow, and soil erosion for the efficient management of water resources and quality. In this study, future climate change scenarios were applied to the H aean-myeon watershed which is a steep sloping watershed in South Korea to analyze groundwater recharge, baseflow, sediment. Also, the variation of groundwater recharge, baseflow, sediment was analyzed according to the change of slope (5 %). Simulated periods were divided into three terms (2013 ~ 2040 years, 2041 ~ 2070 years, 2071 ~ 2100 years). As a result of this study, average groundwater recharge and baseflow increased by 50 %, 42 %, and sediment decreased by 72 %, respectively. In these regards, the suggested method will positively contribute to hydro-ecosystem and reduction of muddy water at a steep sloping watershed.

Evaluation of Drought Effect on Groundwater System using Groundwater Level Data in Jeju Island (지하수위 자료를 이용한 제주도 지하수계의 가뭄 영향 평가)

  • Song, Sung-Ho;Lee, Byung-Sun;Choi, Kwang-Jun;Kim, Jin-Sung;Kim, Gi-Pyo
    • Journal of Environmental Science International
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    • v.23 no.4
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    • pp.637-647
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    • 2014
  • Quantitative assessment of groundwater level change under extreme event is important since groundwater system is directly affected by drought. Substantially, groundwater level fluctuation reveals to be delayed from several hours to few months after raining according to the aquifer characteristics. Groundwater system in Jeju Island would be also affected by drought and almost all regions were suffered from a severe drought during summer season (July to September) in 2013. To estimate the effect of precipitation to groundwater system, monthly mean groundwater levels in 2013 compared to those in the past from 48 monitoring wells belong to be largely affected by rainfall(Dr) over Jeju Island were analyzed. Mean groundwater levels during summer season recorded 100 mm lowered of precipitation compared to the past 30 years became decreased to range from 2.63 m to 5.42 m in southern region compared to the past and continued to December. These decreasing trends are also found in western(from -1.21 m to -4.06 m), eastern(-0.91 m to -3.24 m), and northern region(from 0.58 m to -4.02 m), respectively. Moreover, the response of groundwater level from drought turned out to be -3.80 m in August after delaying about one month. Therefore, severe drought in 2013 played an important role on groundwater system in Jeju Island and the effect of drought for groundwater level fluctuation was higher in southern region than other ones according to the regional difference of precipitation decrease.

Seasonal Variation of Hydraulic Gradient according to Rainfall in Unconfined Aquifer : Hyogyo-ri (자유면 대수층에서 강우량에 따른 수리경사 계절 변동 분석 : 효교리)

  • Kyoung-deok Park;Dong-hwan Kang;Won Gi Jo;In-Kyu Shin;Yun-Yeong Oh;MoonSu Kim;Hyun-Koo Kim
    • Journal of Environmental Science International
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    • v.32 no.5
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    • pp.303-313
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    • 2023
  • In this study, the hydraulic gradient was calculated using the groundwater level and rainfall observed in the Hyogyo-ri area for a year, and the change in the hydraulic gradient according to the rainfall was analyzed. It was found that the groundwater level increased as the rainfall increased in all groundwater wells in the research site, and the groundwater level rise decreased as the altitude of the groundwater well increased. The hydraulic gradient in the research site ranged from 0.016 to 0.048, decreasing during rainfall and increasing after the end of the rainfall. As the rainfall increased, the groundwater level rise in the low-altitude area was more than the high-altitude area, and the hydraulic gradient decreased due to the difference in groundwater level rise according to the altitude. Through this study, it was found that the influence of rainfall is dominant for the fluctuation of the hydraulic gradient in the unconfined aquifer.