• Title/Summary/Keyword: 심해탐사

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Acoustic images of the submarine fan system of the northern Kumano Basin obtained during the experimental dives of the Deep Sea AUV URASHIMA (심해 자율무인잠수정 우라시마의 잠항시험에서 취득된 북 구마노 분지 해저 선상지 시스템의 음향 영상)

  • Kasaya, Takafumi;Kanamatsu, Toshiya;Sawa, Takao;Kinosita, Masataka;Tukioka, Satoshi;Yamamoto, Fujio
    • Geophysics and Geophysical Exploration
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    • v.14 no.1
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    • pp.80-87
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    • 2011
  • Autonomous underwater vehicles (AUVs) present the important advantage of being able to approach the seafloor more closely than surface vessel surveys can. To collect bathymetric data, bottom material information, and sub-surface images, multibeam echosounder, sidescan sonar (SSS) and subbottom profiler (SBP) equipment mounted on an AUV are powerful tools. The 3000m class AUV URASHIMA was developed by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC). After finishing the engineering development and examination phase of a fuel-cell system used for the vehicle's power supply system, a renovated lithium-ion battery power system was installed in URASHIMA. The AUV was redeployed from its prior engineering tasks to scientific use. Various scientific instruments were loaded on the vehicle, and experimental dives for science-oriented missions conducted from 2006. During the experimental cruise of 2007, high-resolution acoustic images were obtained by SSS and SBP on the URASHIMA around the northern Kumano Basin off Japan's Kii Peninsula. The map of backscatter intensity data revealed many debris objects, and SBP images revealed the subsurface structure around the north-eastern end of our study area. These features suggest a structure related to the formation of the latest submarine fan. However, a strong reflection layer exists below ~20 ms below the seafloor in the south-western area, which we interpret as a denudation feature, now covered with younger surface sediments. We continue to improve the vehicle's performance, and expect that many fruitful results will be obtained using URASHIMA.

The Characteristics of Physical Oceanographic Environments and Bottom Currents in the KODOS Study Area of the Northeastern Tropical Pacific (동태평양 KODOS 탐사해역에서의 물리해양환경 및 저층해류 특성)

  • Shin, Hong-Ryeol;Hwang, Sang-Chul;Jeon, Dong-Chull;Kim, Ki-Hyune;Kwak, Chong-Heum;So, Seun-Seup
    • Ocean and Polar Research
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    • v.26 no.2
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    • pp.341-349
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    • 2004
  • Hyrdography and deep currents were measured from 1997 to 1999 to investigate deep-sea environments in the KODOS (Korea Deep Ocean Study) area of the northeastern tropical Pacific. KODOS area is located meridionally from the North Equatorial Current to the boundary between the North Equatorial Current and the Equatorial Counter Current. Strong thermocline exists between 10 m and 120 m depths at the study area. Since that strong thermocline does hardly allow vertical mixing between surface and lower layer waters, vertical distributions of temperature, salinity, dissolved oxygen and nutrients drastically change near the thermocline. Salinity-minimum layer, which indicate the North Pacific Intermediate Water (NPIW) and the Antartic Intermediate Water (AAIW), vertically occupies vertically at the depths from 500 m down to 1400 m. The NPIW and the AAIW horizontally occur to the north and to the south of $7^{\circ}N$, respectively. The near-bottom water shows the physical characteristics of $1.05^{\circ}C$ and 34.70 psu at the depths of 10 m to 110 m above the bottom (approximately 4000-5000 m), which was originated from the Antarctic Circumpolar Water. It flows northeastwards for 2 to 4 months at the study area, and its mean velocity was 3.1-3.7 cm/s. Meanwhile, reverse (southwestward) currents appear for about 15 days with the average of 1.0-6.1 cm/s every 1 to 6 months. Dominant direction of the bottom currents obtained from the data for more than 6 months is northeastward with the average speeds of 1.7-2.1 cm/s. Therefore, it seems that deep waters from the Antarctica flow northwards passing through the KODOS area in the northeastern tropical Pacific.

최근 우리나라 조선산업의 모습과 장래 전망

  • 김영훈
    • Bulletin of the Society of Naval Architects of Korea
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    • v.32 no.4
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    • pp.64-67
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    • 1995
  • 우리나라 조선산업이 21세기에 명실상부한 선진 조선국으로 발돋움하기 위해서는 단기적으로는 가격경쟁력의 강화가 요구되나 장기적으로는 기술자립화를 통해 과거 가격위주의 경쟁체제에서 기술위주의 경쟁체제로 전환함으로써 질적인 성장을 추구해야 할 것이다. 또한 우리나라의 조 선산업은 세계조선시장을 리드하는 선도국으로서 세계선박수급구조의 안정화에 노력하고 지구 해양환경보호를 위한 국제적인 프로그램에 적극 참여하는 한편, 후발조선국에 대한 기술협력, 기술지도 등 국제협력도 강화하여 명실상부한 선진조선국의 면모를 갖추어야 할 것이다. 이를 효과적으로 추진하기 위해서는 다음과 같은 과제를 해결해야 할 것이다. 첫째, 효율적 기술개발을 통한 건조기술의 재고가 그 무엇보다도 중요하다. 즉 단기적으로는 주요 대체수요 선박이면서 국내 주력건조선박인 탱커, 벌크케리어 등 재래단순형 선박에 대해 성에 너지화, 성인력화 및 표준선형화하고, 선박 생산공정의 개선, 생산성 향상을 통해 가격경쟁력을 지속적으로 확보해야할 것이다. 그러나 중장기적으로는 가스운반선,카페리선, 초고속선 등의 부가가치선박에 대한 건 조기술의 자립화로 이들 선종을 주력선종화하여 해외 수주 경쟁력을 재고시켜야 한다. 이와함께 심해탐사장비, 해양구조부유물 등의 해양개발장비의 개발로 사업영역을 확대해야할 것이다. 상 기의 각종 기술재발을 효율적으로 추진하기 위해서는 범국가적인 연구체제의 구성을 통한 산학연 공동연구형태로 추진하는 것이 바람직하다. 둘째, 핵심 조선기자재의 국산화와 품질 향상이 필 요하다. 향후 조선기자재의 국산화추진은 과거 개발 품목의 확대에서 벗어나 핵심적이고 부가 가치가 높은 품목 위주의 질적 국산화로 전환되어야 할 것이며, 이때 국산화이후 조선소의 적 극적인 구매가 전제되어야 할 것이다. 또한 기자재의 품질, 성능검사기능의 강화와 다수요 품목을 중심으로한 표준화, 규격화의 확대 추진으로 지속적인 품질향상과 원가절감을 도모해야한다. 특히 조선기자재업체의 영세상을 감안하여 조선소 인근지역에 단지화함으로써 생산설비의 현 대화, 자재의 공동구매, 물류비용의 절감 등을 기해 가격경쟁력을 강화해야 할 것이다. 또한 업계 공동의 해외판매망, A/S망의 직수출을 늘려야 할 것이다. 셋째, 국제협력 강화로 통상환경에 적극 대응해야 한다. 다자간조선협정 발효에 따른 제소 가능성에 대비하여 관민차원의 국제협 력을 강화하는 한편, 회계 기준의 통일, 제소사례의 연구 등을 업계 공동으로 추진하는 것이 바 람직하다. 또한 향후 2010년이후에 중국을 비롯한 후발조선국에 대해 조선협정에의 참여를 유도, 세계조선시장의 수급안정화에 노력해야할 것이다. 그외에 국제적으로 추진되는 지구그린화에 주도적 역할을 수행해야 할 것이다. 넷째, 선박금융제도의 개선과 신금융상품의 개발이 요구된다. 내수 수요인 계획조선의 지원조건을 개선하고 연불수출자금을 BBC자금으로 활용토록하여 국내 선주들의 신조를 유도해야 할 것이다. 그 외에 향후 금융개방화에 맞추어 해외자금을 활용한 리스금융, 상사금융 등의 민간신용제도를 더욱 활성화하고 선진국의 선박금융기법에 대한 연구 및 도입 등 선주들에게 다양한 선박건조자금을 제공하여 내수기반 확충에도 노력해야 할 것 이다.

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Assessment of the Structural Collapse Behavior of Between Offshore Supply Vessel and Leg in the Jack-up Drilling Rig (잭업드릴링 리그의 레그와 작업 지원선 충돌에 의한 구조붕괴 거동 평가)

  • Park, Joo-Shin;Seo, Jung-Kwan
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.28 no.4
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    • pp.601-609
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    • 2022
  • Jack-up drilling rigs are mobile offshore platforms widely used in the offshore oil and gas exploration industry. These are independent, three-legged, self-elevating units with a cantilevered drilling facility for drilling and production. A typical jack-up rig includes a triangular hull, a tower derrick, a cantilever, a jackcase, living quarters and legs which comprise three-chord, open-truss, X-braced structure with a spudcan. Generally, jack-up rigs can only operate in water depths ranging from 130m to 170m. Recently, there has been an increasing demand for jack-up rigs for operating at deeper water levels and harsher environmental conditions such as waves, currents and wind loads. All static and dynamic loads are supported through legs in the jack-up mode. The most important issue by society is to secure the safety of the leg structure against collision that causes large instantaneous impact energy. In this study, nonlinear FE -analysis and verification of the requirement against collision for 35MJ recommended by DNV was performed using LS-Dyna software. The colliding ship used a 7,500ton of shore supply vessel, and five scenarios of collisions were selected. From the results, all conditions do not satisfy the class requirement of 35MJ. The loading conditions associated with chord collision are reasonable collision energy of 15M and brace collisions are 6MJ. Therefore, it can be confirmed that the identical collision criteria by DNV need to be modified based on collision scenarios and colliding members.

A Study on the Hydrothermal Vent in the Mariana Trench using Magnetic and Bathymetry Data (지자기자료 및 정밀해저지형자료를 이용한 마리아나 해구 해저 열수광상 연구)

  • Kim, Chang-Hwan;Kim, Ho;Jeong, Eui-Young;Park, Chan-Hong;Go, Young-Tak;Lee, Seung-Hoon
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.14 no.1
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    • pp.22-40
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    • 2009
  • Detailed bathymetry and magnetic survey data for NW Rota-1 and Esmeralda Bank obtained by R/V Onnuri of Korea Ocean Research & Development Institute in September 2007 were analyzed to investigate bathymetry and magnetic characteristics of the study area and to estimate the locations of possible hydrothermal vents. The shape of NW Rota-1 is corn type, and the depth of the summit is about 500 meter b.s.l. NW Rota-1 shows irregular topographic expression in the southeastern part. The shape of Esmeralda Bank is caldera type opened in the western part. The summit is very shallow, about 50 meter b.s.l. The western part of Esmeralda Bank is more steeper and topographic irregular than the eastern part, and have the valley made by erosion or collapse. The magnetic anomaly patterns of NW Rota-1 and Esmeralda Bank show low anomalies over the north and high anomalies over the south. The magnetic anomalies are steep over the summits and gently smooth over the deep bottom. The low magnetization zone occurs over the summit of NW Rota-1 and is surrounded by the high zones correlated with its crater. Two low magnetization zones are located in the summit and westside of Esmeralda Bank. The low magnetization zones of the summits of NW Rota-1 and Esmeralda Bank suggest the possible existence of hydrothermal vent.