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      표준지하수위지수(SGI)를 이용한 농촌지역 지하수계의 가뭄 영향 평가 = Assessment of Drought Effects on Groundwater System in Rural Area using Standardized Groundwater Level Index(SGI)

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      https://www.riss.kr/link?id=A105477560

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      This study is aimed to quantitatively evaluate the effects of drought on groundwater system in rural areas. For this purpose, the standardized groundwater level index (SGI) was used for 68 groundwater monitoring wells. To determine accumulation period (AP) which represents the month with the highest correlation coefficient between SGI and SPI, correlation analysis between the two for 68 wells were peformed. The results indicated the AP values ranged in 1~3 months for most of the well, but it was 7~10 months in some wells. These results can be interpreted such that the total amount of groundwater will not decrease significantly in long-term drought situations unlikely the reservoirs with the high AP values. The nationwide maximum AP values were 4.1 and 4.0 in Chungbuk-do and Gyeongnam-do, while the minimum AP values were 1.8 and 2.0 in Gangwon-do and Chungnam-do, respectively. The maximum and minimum values of correlation coefficient were 0.623 and 0.459 in Gyeongnam-do and Chungnam-do/Chungbuk-do, respectively. Consequently, it could be concluded that the wells with low AP value tend to respond to short-term drought, but it has little effect on groundwater system when the long drought occurs.
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      This study is aimed to quantitatively evaluate the effects of drought on groundwater system in rural areas. For this purpose, the standardized groundwater level index (SGI) was used for 68 groundwater monitoring wells. To determine accumulation period...

      This study is aimed to quantitatively evaluate the effects of drought on groundwater system in rural areas. For this purpose, the standardized groundwater level index (SGI) was used for 68 groundwater monitoring wells. To determine accumulation period (AP) which represents the month with the highest correlation coefficient between SGI and SPI, correlation analysis between the two for 68 wells were peformed. The results indicated the AP values ranged in 1~3 months for most of the well, but it was 7~10 months in some wells. These results can be interpreted such that the total amount of groundwater will not decrease significantly in long-term drought situations unlikely the reservoirs with the high AP values. The nationwide maximum AP values were 4.1 and 4.0 in Chungbuk-do and Gyeongnam-do, while the minimum AP values were 1.8 and 2.0 in Gangwon-do and Chungnam-do, respectively. The maximum and minimum values of correlation coefficient were 0.623 and 0.459 in Gyeongnam-do and Chungnam-do/Chungbuk-do, respectively. Consequently, it could be concluded that the wells with low AP value tend to respond to short-term drought, but it has little effect on groundwater system when the long drought occurs.

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      참고문헌 (Reference)

      1 송성호, "변동유형 분석법을 이용한 해수침투 관측망 자료 평가" 한국지구과학회 28 (28): 478-490, 2007

      2 송성호, "기후변화를 고려한 제주지역의 권역별 가뭄 평가 및 농업용수에의 영향 고찰" 한국환경과학회 22 (22): 625-638, 2013

      3 Shukla, S., "Use of a standardized runoff index for characterizing hydrologic drought" 35 : L02405-, 2008

      4 Wilhite, D.A., "Understanding the drought phenomenon: The role of definition" 10 (10): 111-120, 1985

      5 McKee, T. B., "The relationship of drought frequency and duration time scales" 179-184, 1993

      6 "NDMC (National Drought Mitigation Center)"

      7 Kumar, R, "Multiscale evaluation of the standardized precipitation index as a groundwater drought indicator" 20 : 1117-1131, 2016

      8 Vincente-Serrano, S.M., "Hydrological response to different time scales of climatological drought: an evaluation of the Standardized Precipitation Index in a mountainous Mediterranean basin" 9 : 523-533, 2005

      9 Todd, D.K., "Groundwater Hydrology" John Wiley & Sons 535-, 1980

      10 Sheffield, J., "Global and continental drought in the second half of the twentieth century: Severity-Area-Duration analysis and temporal variability of large-scale events" 22 : 1962-1981, 2008

      1 송성호, "변동유형 분석법을 이용한 해수침투 관측망 자료 평가" 한국지구과학회 28 (28): 478-490, 2007

      2 송성호, "기후변화를 고려한 제주지역의 권역별 가뭄 평가 및 농업용수에의 영향 고찰" 한국환경과학회 22 (22): 625-638, 2013

      3 Shukla, S., "Use of a standardized runoff index for characterizing hydrologic drought" 35 : L02405-, 2008

      4 Wilhite, D.A., "Understanding the drought phenomenon: The role of definition" 10 (10): 111-120, 1985

      5 McKee, T. B., "The relationship of drought frequency and duration time scales" 179-184, 1993

      6 "NDMC (National Drought Mitigation Center)"

      7 Kumar, R, "Multiscale evaluation of the standardized precipitation index as a groundwater drought indicator" 20 : 1117-1131, 2016

      8 Vincente-Serrano, S.M., "Hydrological response to different time scales of climatological drought: an evaluation of the Standardized Precipitation Index in a mountainous Mediterranean basin" 9 : 523-533, 2005

      9 Todd, D.K., "Groundwater Hydrology" John Wiley & Sons 535-, 1980

      10 Sheffield, J., "Global and continental drought in the second half of the twentieth century: Severity-Area-Duration analysis and temporal variability of large-scale events" 22 : 1962-1981, 2008

      11 RRI (Rural Research Institute, KRC), "Development of Assessment Technology for Agricultural Drought using the Analysis of Real-time Groundwater Data" 263-, 2017

      12 Bloomfield, J.P., "Analysis of groundwater drought building on the standardised precipitation index approach" 17 : 4769-4787, 2013

      13 McEvoy, D. J., "An evaluation of multiscalar drought indices in Nevada and eastern California" 16 : 1-8, 2012

      14 Mishra, A. K., "A review of drought concepts" 391 : 202-216, 2010

      15 Vincente-Serrano, S.M., "A multiscalar drought index sensitive to global warming: The standardized precipitation evapotranspiration index" 23 : 1696-1718, 2010

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2026 평가예정 재인증평가 신청대상 (재인증)
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.3 0.3 0.35
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.35 0.36 0.568 0.05
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