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      북동태평양 한국 망간단괴 광구해역에서 환경충격 시험지역과 보존지역간의 수층환경 및 침강입자 플럭스 유사성 비교 = Evaluation of Similarity of Water Column Properties and Sinking Particles between Impact and Preserved Sites for Environmental Impact Assessment in the Korea Contracted Area for Manganese Nodule Development, NE Pacific

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      https://www.riss.kr/link?id=A103775615

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      다국어 초록 (Multilingual Abstract)

      Verifying the similarity of environmental characteristics between an artificial impact site and a preserved or reference site is necessary to quantitatively and qualitatively evaluate the environmental impact of mining activity. Although an impact site (BIS station) and a preserved site (called KOMO station) that have been selected in the Korea manganese nodule contract area may share similar environmental characteristics, similarities in terms of the water column environment between both sites has not been investigated. In this study, we compared the chemical properties of the water columns and sinking particle fluxes between BIS and KOMO stations through two observations (August 2011 and September 2012). Additionally, we observed particle fluxes at the KOMO station for five years (July 2003~July 2008) to understand long-term natural variability. Vertical distributions of water column properties such as dissolved oxygen, inorganic nutrients (N, P, Si), total organic carbon below surface layer (within the depth range of 200 m) were not considerably different between the two sites. Especially, values of water column parameters in the abyssopelagic zone from 4000 m to bottom layer (~5000 m) were very similar between the BIS and KOMO sites. Sinking particle fluxes from the two sites also showed similar seasonality. However, natural variation of particle flux at the KOMO site varied from 3.5 to 129.9 mg m−2 day−1, with a distinct temporal variation originating from ENSO events (almost forty times higher than a minimum value). These results could provide valuable information to more exactly evaluate the environmental impact of mining activity on water columns.
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      Verifying the similarity of environmental characteristics between an artificial impact site and a preserved or reference site is necessary to quantitatively and qualitatively evaluate the environmental impact of mining activity. Although an impact sit...

      Verifying the similarity of environmental characteristics between an artificial impact site and a preserved or reference site is necessary to quantitatively and qualitatively evaluate the environmental impact of mining activity. Although an impact site (BIS station) and a preserved site (called KOMO station) that have been selected in the Korea manganese nodule contract area may share similar environmental characteristics, similarities in terms of the water column environment between both sites has not been investigated. In this study, we compared the chemical properties of the water columns and sinking particle fluxes between BIS and KOMO stations through two observations (August 2011 and September 2012). Additionally, we observed particle fluxes at the KOMO station for five years (July 2003~July 2008) to understand long-term natural variability. Vertical distributions of water column properties such as dissolved oxygen, inorganic nutrients (N, P, Si), total organic carbon below surface layer (within the depth range of 200 m) were not considerably different between the two sites. Especially, values of water column parameters in the abyssopelagic zone from 4000 m to bottom layer (~5000 m) were very similar between the BIS and KOMO sites. Sinking particle fluxes from the two sites also showed similar seasonality. However, natural variation of particle flux at the KOMO site varied from 3.5 to 129.9 mg m−2 day−1, with a distinct temporal variation originating from ENSO events (almost forty times higher than a minimum value). These results could provide valuable information to more exactly evaluate the environmental impact of mining activity on water columns.

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      참고문헌 (Reference)

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      1 손주원, "북동태평양 적도 Thermocline Ridge 해역에서 영양염(질소, 인, 규소)과 유기탄소(용존 및 입자)의 분포 특성 및 연간 변화" 한국해양과학기술원 33 (33): 55-68, 2011

      2 Van Dover CL, "Tighten regulations on deep-sea mining" 470 : 31-33, 2011

      3 MLTM, "The report of deep sea mineral resources development (3rd level): precision environments" Korea Ocean Research and Development Institute 69-, 2011

      4 Thiel H, "The large-scale environmental impact experiment DISCOL-reflection and foresight" 48 : 3869-3882, 2001

      5 Trueblood DD, "The ecological impacts of the joint US-Russian benthic impact experiment" 139-145, 1997

      6 Glover AG, "The deep-sea floor ecosystem:current status and prospects of anthropogenic change by the year 2025" 30 (30): 219-241, 2003

      7 Brzezinski MA, "The Si:C:N ratio of marine diatoms:interspecific variability and the effect of some environmental variables" 21 : 347-357, 1985

      8 Honjo S, "Sedimentation of biogenic matter in the deep ocean" 29 : 609-625, 1982

      9 Sharma R, "Sediment redistribution during simulated benthic disturbance and its implications on deep seabed mining" 48 : 3363-3380, 2001

      10 Haake B, "Seasonality and interannual variablty of particle fluxes to the deep Arabian Sea" 40 : 1323-1344, 1993

      11 Hyung Jeek Kim, "Seasonal variations of particle fluxes in the northeastern equatorial Pacific during normal and weak El Niño periods" 한국지질과학협의회 14 (14): 415-422, 2010

      12 Schriever G, "Seafloor macrofauna in potential mining areas: Parameters for assessment, recommended techniques and levels of replication" 326-368, 2002

      13 Quan TM, "Redox control of N:P ratios in aquatic ecosystems" 7 : 124-139, 2009

      14 Anderson LA, "Redfield ratios of remineralization determined by nutrient data analysis" 8 : 65-80, 1994

      15 Pennington JT, "Primary production in the eastern tropical Pacific: a review" 69 : 285-317, 2006

      16 Berelson WM, "Particle settling rates increase with depth in the ocean" 49 : 237-251, 2002

      17 Oebius HU, "Parametrization and evaluation of marine environmental impacts produced by deep-sea manganese nodule mining" 48 : 3453-3467, 2001

      18 Karstensen J, "Oxygen minimum zones in the eastern tropical Atlantic and Pacific ocean" 77 : 331-350, 2008

      19 Paulmier A, "Oxygen minimum zones (OMZs) in the modern ocean" 80 : 113-128, 2009

      20 Hill JK, "Organic carbon and nitrogen in the northern California current system: Comparison of offshore, river plume and coastally upwelled waters" 53 : 369-387, 2002

      21 Doval MD, "Organic carbon and apparent oxygen utilization in the western south and the central Indian Ocean" 68 : 249-264, 2000

      22 Yamazaki T, "Optical determination of the JET deep sea sediment disturbance" 153-168, 1997

      23 Wada E, "Nitrogen in the sea: Forms, Abundances and Rate processes" CRC Press 71-75, 1991

      24 Nath BN, "Monitoring the sedimentary carbon in an artificially disturbed deepsea sedimentary environment" 184 : 2829-2844, 2012

      25 Romero-Centeno R, "Midsummer gap winds and low-level circulation over the Eastern Tropical Pacific" 20 : 2007

      26 El-Sayed SZ, "Marine Geology and Oceanography of the Pacific Manganese Nodule Province" 241-286, 1979

      27 SPC, "Manganese nodules, a physical, biological, environmental, and technical review, Vol 1B" Secretariat of the Pacific Community (SPC) 2013

      28 Yamada H, "Japan's ocean test of the nodule mining system" 13-19, 1998

      29 Kim HJ, "Influence of ENSO variability on sinking-particle fluxes in the northeastern equatorial Pacific" 58 : 865-874, 2011

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      32 Kim HJ, "Impact of strong ElNiño events (1997/98 and 2009/10) on sinking particle fluxes in the 10oN thermocline ridge area of the northeastern equatorial Pacific" 67 : 111-120, 2012

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      39 Ozturgut E, "Environmental investigation during manganese nodule mining tests in the North Equatorial Pacific in November 1978" NOAA 50-, 1980

      40 Chung JS, "Effect of particle size and concentration on pressure gradient in two-phase vertically upward transport" 132-138, 2001

      41 Karl DM, "Ecosystem changes in the North Pacific subtropical gyre attributed to the 1991-92 El Nino" 373 : 230-234, 1995

      42 Yang EJ, "Distribution and structure of heterotrophic protest communities in the northeast equatorial Pacific Ocean" 146 : 1-15, 2004

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      45 Schriever G, "DISCOL-precautionary large scale environmental impact studies for future polymetallic nodule mining from the deep sea" 1311-1319, 1992

      46 Schriever G, "DISCOL-precautionary environmental impact studies for future manganese nodule mining and first results on meiofauna abundance" 4 : 47-57, 1991

      47 Yamada A, "Combined analysis of ecology and economy of manganese nodule mining" 73-79, 2009

      48 Millero FJ, "Chemical oceanography" CRC Press 266-277, 2006

      49 Bostock HC, "Characterising the intermediate depth waters of the Pacific Ocean using δ13C and other geochemical tracers" 57 : 847-859, 2010

      50 Chavez FP, "Biological and chemical response of the equatorial Pacific ocean to the 1997-1998 El Nino" 286 : 2126-2131, 1999

      51 Dymond J, "Biogenic particle fluxes in the equatorial Pacific: evidence for both high and low productivity during the 1982-83 El Nino" 2 : 129-137, 1988

      52 Amador JA, "Atmospheric forcing of the eastern tropical Pacific: a review" 69 : 101-142, 2006

      53 Talley LD, "An Okhotsk Sea-water anomaly-implications for ventilation in the North Pacific" 38 : 171-190, 1991

      54 Jiang MS, "A nitrate and silicate budget in the equatorial Pacific Ocean: a couple physical-biological model study" 50 : 2971-2996, 2003

      55 Parsons TR, "A manual of chemical and biological methods for seawater analysis" Pergamon Press 173-, 1984

      56 Sugimura Y, "A high-temperature catalytic oxidation method for the determination of non-volatile dissolved organic carbon in seawater by direct injection of a liquid sample" 24 : 105-131, 1988

      57 Mengerink KJ, "A call for deep-ocean stewardship" 344 : 696-698, 2014

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2023 평가예정 해외DB학술지평가 신청대상 (해외등재 학술지 평가)
      2020-01-01 평가 등재학술지 유지 (해외등재 학술지 평가) KCI등재
      2014-03-31 학회명변경 한글명 : 한국해양연구원 -> 한국해양과학기술원
      영문명 : Korea Ocean Research and Development Institute -> Korea Institute of Ocean Science & Technology
      KCI등재
      2014-01-01 평가 SCOPUS 등재 (등재유지) KCI등재
      2011-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2009-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2007-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2005-06-28 학술지등록 한글명 : Ocean and Polar Research
      외국어명 : Ocean and Polar Research
      KCI등재
      2005-06-28 학술지등록 한글명 : Ocean Science Journal
      외국어명 : Ocean Science Journal
      KCI등재
      2005-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2002-07-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2000-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.38 0.38 0.43
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.39 0.35 0.749 0.1
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