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      가스 하이드레이트의 해리로 인한 해저사면의 붕괴에 관한 연구 = A Study on Submarine Slope Failure due to Gas Hydrate Dissociation

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      https://www.riss.kr/link?id=A104635343

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      The influence of gas hydrate dissociation on submarine slope stability was studied in this paper. Gas hydrates are stable under high pressure and low temperature conditions. Once gas hydrate dissociates due to natural or human activities, it generates large amount of gas and water. During gas hydrate dissociation, a pore pressure between soil particles increases and results in the loss of an effective stress and degradation of soil stiffness and strength. An excess pore pressure generated by gas hydrate dissociation for the Storegga Slide was calculated from two existing pore pressure calculation methods and the proposed method. The proposed method gives at least two times more excess pore pressure than the existing methods. A slope stability analysis for the Storegga Slide using a two dimensional finite difference method was carried out by considering excess pore pressures due to gas hydrate dissociation. Since the excess pore pressure calculated by the proposed method resulted in the considerable loss of stiffness and strength in gas hydrate zone, a submarine slope failure occurred at the Storegga slide was successfully simulated.
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      The influence of gas hydrate dissociation on submarine slope stability was studied in this paper. Gas hydrates are stable under high pressure and low temperature conditions. Once gas hydrate dissociates due to natural or human activities, it generates...

      The influence of gas hydrate dissociation on submarine slope stability was studied in this paper. Gas hydrates are stable under high pressure and low temperature conditions. Once gas hydrate dissociates due to natural or human activities, it generates large amount of gas and water. During gas hydrate dissociation, a pore pressure between soil particles increases and results in the loss of an effective stress and degradation of soil stiffness and strength. An excess pore pressure generated by gas hydrate dissociation for the Storegga Slide was calculated from two existing pore pressure calculation methods and the proposed method. The proposed method gives at least two times more excess pore pressure than the existing methods. A slope stability analysis for the Storegga Slide using a two dimensional finite difference method was carried out by considering excess pore pressures due to gas hydrate dissociation. Since the excess pore pressure calculated by the proposed method resulted in the considerable loss of stiffness and strength in gas hydrate zone, a submarine slope failure occurred at the Storegga slide was successfully simulated.

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      참고문헌 (Reference)

      1 허대기, "가스하이드레이트 기술개발 현황" 한국자원공학회 42 (42): 206-213, 2005

      2 Popenoe, P., "“The Cape Fear Landslide: slope failure associated with salt diapirism and gas hydrate decomposition,” Submarine landslides: Selected studies in the US exclusive economic zone"

      3 Bondevik, S., "Tsunami sedimentary facies deposited by the Storegga tsunami in shallow marine basins and coastal lakes, western Norway" 44 : 115-1131, 1997

      4 Nixon, M.F., "Submarine slope failure due to gas hydrate dissociation: a preliminary quantification" 44 : 314-325, 2007

      5 Geo-Slope, "Slope/w" Geo-Slope International 2001

      6 Kayen R.E., "Slope stability in regions of sea-floor gas hydrate: Beaufort Sea continental slope in:Submarine landslides: selected studies in the US exclusive economic zone" 97-103, 1993

      7 Leynaud, D., "Slope stability assessment of the Helland Hansen area offshore the mid-Norwegian margin" 213 : 457-480, 2004

      8 McIver, R.D., "Role of naturally occurring gas hydrates in sediment transport" 66 : 789-792, 1982

      9 Kvenvolden, K.A., "Potential effects of gas hydrate on human welfare" 96 : 3420-3426, 1999

      10 Mienert, J., "Ocean warming and gas hydrate stability on the mid-Norwegian margin at the storegga slide" 22 : 233-244, 2005

      1 허대기, "가스하이드레이트 기술개발 현황" 한국자원공학회 42 (42): 206-213, 2005

      2 Popenoe, P., "“The Cape Fear Landslide: slope failure associated with salt diapirism and gas hydrate decomposition,” Submarine landslides: Selected studies in the US exclusive economic zone"

      3 Bondevik, S., "Tsunami sedimentary facies deposited by the Storegga tsunami in shallow marine basins and coastal lakes, western Norway" 44 : 115-1131, 1997

      4 Nixon, M.F., "Submarine slope failure due to gas hydrate dissociation: a preliminary quantification" 44 : 314-325, 2007

      5 Geo-Slope, "Slope/w" Geo-Slope International 2001

      6 Kayen R.E., "Slope stability in regions of sea-floor gas hydrate: Beaufort Sea continental slope in:Submarine landslides: selected studies in the US exclusive economic zone" 97-103, 1993

      7 Leynaud, D., "Slope stability assessment of the Helland Hansen area offshore the mid-Norwegian margin" 213 : 457-480, 2004

      8 McIver, R.D., "Role of naturally occurring gas hydrates in sediment transport" 66 : 789-792, 1982

      9 Kvenvolden, K.A., "Potential effects of gas hydrate on human welfare" 96 : 3420-3426, 1999

      10 Mienert, J., "Ocean warming and gas hydrate stability on the mid-Norwegian margin at the storegga slide" 22 : 233-244, 2005

      11 Seed, H. B., "Moduli and damping factors for dynamic analyses of cohesionless soils" 112 (112): 1016-1032, 1986

      12 Kvenvolden, K.A., "Gas hydrates-Geological perspective and global change" 31 (31): 173-187, 1993

      13 Milkov, A.V., "Gas hydrates at minimum stability water depths in the Gulf of Mexico: Significance to Geoharzard Assessment" 217-224, 2000

      14 Kvenvolden, K.A., "Gas hydrate and humans" 912 : 17-22, 2000

      15 USGS, "Gas (Methane) Hydrates-A New Frontier"

      16 Itasca, "FLAC" Minneapolis 2000

      17 Dillon, W.P., "Evidence of faulting related to dissociation of gas hydrate and release of methane off the southeastern U.S in:Gas hydrates: Relevance to World Margin stability and climate change, Geological Society" Special Publications 293-302, 1998

      18 Sultan, N., "Effect of gas hydrates melting on seafloor slope instability" 213 : 379-401, 2004

      19 Jung, W.Y., "Effect of bottom water warming and sea level rise on Holocene hydrate dissociation and mass wasting along the Norweigian-Barents Continental Margin" 109 : 18-, 2004

      20 Grantz, A., "Constraints of geologic processes on western Beaufort Sea oil developments" 78 (78): 304-319, 1980

      21 Field, M.E., "A submarine landslide associated with shallow seafloor gas hydrates off northern California in:Submarine landslides: selected studies in the US exclusive economic zone" 151-157, 1993

      22 Bugge, T., "A giant three-stage submarine slide off Norway" 7 : 191-198, 1987

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2022 평가예정 계속평가 신청대상 (등재유지)
      2017-01-01 평가 우수등재학술지 선정 (계속평가)
      2013-06-13 학술지명변경 한글명 : 한국지구시스템공학회지 -> 한국자원공학회지
      외국어명 : Journal of the Korean society for geosystem engineering -> Journal of the Korean Society of Mineral and Energy Resources Engineers
      KCI등재
      2013-06-13 학회명변경 한글명 : 한국지구시스템공학회 -> 한국자원공학회
      영문명 : The Korean Society For Geosystem Engineering -> The Korean Society of Mineral and Energy Resources Engineers
      KCI등재
      2013-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2010-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2008-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2004-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2001-07-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      1999-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.13 0.13 0.15
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.17 0.19 0.278 0.07
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