• Title/Summary/Keyword: Rural groundwater management network

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Rural Groundwater Monitoring Network in Korea (농어촌지하수 관측망)

  • Lee, Byung Sun;Kim, Young In;Choi, Kwang-Jun;Song, Sung-Ho;Kim, Jin Ho;Woo, Dong Kwang;Seol, Min Ku;Park, Ki Yeon
    • Journal of Soil and Groundwater Environment
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    • v.19 no.4
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    • pp.1-11
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    • 2014
  • Rural groundwater monitoring network has been managed by Korea Rural Community Corporation (KRC) since 1998. The network consists of two kinds of subnetworks; rural groundwater management network (RGMN) and seawater intrusion monitoring network (SIMN). RGMN has been operated to promote a sound and sustainable development of rural groundwater within the concerned area for groundwater quality and quantity. SIMN has been operated to protect the crops against hazards by the saline water in coastal areas in which the shortage of irrigation water become a main problem for agriculture. Currently, a total of 283 monitoring wells has been installed; 147 wells in 79 municipalities for RGMN and 136 wells in 52 ones for SIMN, respectively. Two subnetworks commonly monitor three hydrophysical properties (groundwater level, temperature, and electric conductivity) every hour. Monitored data are automatically transferred to the management center located in KRC. Data are opened to the public throughout website named to be the Rural Groundwater Net (www.groundwater.or.kr). Annual reports involving well logging and hydrochemical data of RGMN and SIMN have been published and distributed to the rural water management office of each municipalities. In addition, anyone who concerns about RGMN an SIMN can freely download these reports throughout the Rural Groundwater Net as well.

Time Series Analysis of Groundwater Level Change in the Chuncheon Area Groundwater Observation Network (시계열 분석을 이용한 춘천 지역 지하수관측망 수위변동 해석)

  • Mok, Jong-Koo;Jang, Bum-Ju;Park, Yu-Chul;Shin, Hye-Soo;Kim, Jin-Ho;Song, Se-Jeong;Hawng, Ga-Young
    • The Journal of Engineering Geology
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    • v.32 no.2
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    • pp.281-293
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    • 2022
  • Time series analysis was performed on data from 2009 to 2018 from the Chuncheon groundwater observation network to understand the characteristics of groundwater level fluctuations in the network. There are five observatories, all of which are installed in rock aquifers, and periodic inspections and management are performed by the relevant operating organization. Auto-correlation, spectral density, and cross-correlation analysis was performed.

An Interpretation of Changes in Groundwater Level and Electrical Conductivity in Monitoring Wells in Jeiu Island (제주도의 지하수 관측망 자료를 이용한 지하수위 및 전기전도도 변화 해석)

  • Lee, Jin-Yong;Lee, Gyu-Sang;Song, Sung-Ho
    • Journal of the Korean earth science society
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    • v.28 no.7
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    • pp.925-935
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    • 2007
  • Water sources in volcanic Jeju Island are almost entirely dependent on groundwater because there are actually no perennial streams or rivers due to the permeable nature of surface soils derived from basaltic or trachytic rocks. Uncontrolled development of groundwater resulted in substantial water-level decline, groundwater pollution, and seawater intrusion in several places of the island. To maintain its sustainable groundwater, the provincial government has declared some parts of the island as the Special Groundwater Conservation/Management Area since 1994. Hence, all the activities for the groundwater development in the area should obtain official permit from relevant authorities. Furthermore, to acquire information on groundwater status, a network of groundwater monitoring was established to cover most of the low land and coastal areas with the installation of automatic monitoring systems since 2001. The analysis of the groundwater monitoring data indicated that the water levels had decreased at coastal area, especially in northern part of the island. Moreover, very high electrical conductivity (EC) levels and their increasing trends were observed in the eastern part, which was ascribable to seawater intrusion by intensive pumping in recent years. Water level decline and EC rise in the coastal area are expected to continue despite the present strict control on additional groundwater development.