• Title/Summary/Keyword: Deep sea exploration

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A Study of a Method for Detecting Marine Pollution Using X-band Radar (X-Band 레이더를 이용한 해양오염 관측기법에 관한 연구)

  • Park, Seung-Geun;Yang, Young-Jun;Park, Jun-Soo;Kwon, Sun-Hong
    • Journal of Ocean Engineering and Technology
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    • v.24 no.2
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    • pp.53-56
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    • 2010
  • Oil spills and red tide can be very damaging to the environment and fishery farming. These catastrophic accidents must be detected as quickly as possible. In this paper, we report the results of applying the wavelet transform to SAR or marine radar images for the detection of the boundaries of an oil spill or red tide. The application of the wavelet transform to these phenomena looks quite promising in detecting the boundaries of oil spills and red tide areas.

Design and Implementation of A Hovering AUV with A Rotatable-Arm Thruster (회전팔 추진기를 가진 시험용 HAUV의 설계 및 구현)

  • Shin, Dong H.;Bae, Seol B.;Joo, Moon G.;Baek, Woon-Kyung
    • IEMEK Journal of Embedded Systems and Applications
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    • v.9 no.3
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    • pp.165-171
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    • 2014
  • In this paper, we propose the hardware and software of a test-bed of a hovering AUV (autonomous underwater vehicle). Test-bed to develop as the underwater robot for the hovering -type is planning to apply for marine resource development and exploration for deep sea. The RTU that controls a azimuth thruster and a vertical thruster of test-bed is a intergrated-type thruster. The main control unit that collects sensor's data and performs high-speed processing and controls a movement of test-bed is a underwater hybrid navigation system. Also it transfers position, posture, state information of test-bed to the host PC of user using a wireless communication. The host PC checks a test-bed in real time by using a realtime monitoring system that is implemented by LabVIEW.

Strain Distribution of Transition Zone in a Nail Wall (네일로 보강된 구조물에서의 변이영역과 변형률 분포)

  • Chang, Ki-Tae;NamGung, Han;Yoo, Byung-Sun
    • Journal of the Korean Geophysical Society
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    • v.8 no.1
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    • pp.39-43
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    • 2005
  • For the calculation of internal stability, the hypothesis in conventional design is on the basis of two distinct zones, which are 'active zone' and 'passive zone'. This means that there is an abrupt discontinuous transition from active to passive states across a potential failure line. The existence of a discontinuity of this nature appears physically unreasonable, especially from kinematic considerations. A series of pull-out model tests was undertaken from a wall being rotated about the toe to find the strain istribution mobilized from near the wall face into the deep, stable zone through the centre plane. With this finding of transition zone, the objective of study is aiming at identifying the likely effect of this zone in designing method by comparing with the prevailing design method.

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Development of Underwater Vehicle Position Tracking Algorithm by using a Gyro-Doppler Sensor and Ultra Short Base Line (자이로 도플러 센서와 USBL을 통한 수중체 위치추적 알고리즘개발)

  • Kim, Deok-Jin;Park, Dong-Won;Park, Yeon-Sic
    • Journal of the Korea Institute of Information and Communication Engineering
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    • v.10 no.11
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    • pp.1973-1977
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    • 2006
  • This paper reports the absolute position tracking algorithm of underwater vehicles such as ROV, AUV in global region by fusing sensor informations of IMU, DVL, USBL, DGPS etc. This algorithm is to be used in the position tracking of the 6,000m class deep-sea unmanned underwater vehicle, HEMIRE for scientific exploration.

A Study on Characteristics of Magnetism from Hydrothermal Vent Area on Esmeralda Bank in Mariana Arc (Mariana 해령 Esmeralda Bank 해저열수분출 지역에서의 지자기 특성 연구)

  • Kim, Ho;Kim, Chang-Hwan;Jeong, Eui-Young;Park, Chan-Hong;Kim, Jong-Uk;Park, Chung-Hwa
    • 한국지구물리탐사학회:학술대회논문집
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    • 2008.10a
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    • pp.27-32
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    • 2008
  • Detailed bathymetry and magnetic survey data for Esmeralda Bank obtained by R/V Onnuri of Korea Ocean Research & Development Institute in September 2007 were analyzed to estimate the locations of possible hydrothermal vents. The shape of Esmeralda Bank is caldera type opened in the western part. The summit is very shallow, about 50 meter b.s.l. and the bottom is about 1300 meter b.s.l. The western part of Esmeralda Bank is more steeper and topographic irregular than eastern part, and showed the valley made by erosion or collapse. The magnetic anomaly patterns of Esmeralda Bank located 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. Two low magnetization zones are located in the summit and westside of Esmeralda Bank. The low magnetization zones of the summits of Esmeralda Bank suggest the possible existence of hydrothermal vent.

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A Study of STEAM Education for Elementary Science Subject with Robots (교육용 로봇을 활용한 초등학교 과학교과의 STEAM교육 수업 방안)

  • Hong, Ki-Cheon;Shim, Jae-Kuk
    • Journal of The Korean Association of Information Education
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    • v.17 no.1
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    • pp.83-91
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    • 2013
  • The Ministry of Education issues STEAM education as a part of convergence. Most important is "How to achieve goals of STEAM education". The goal of this paper searches possibilities that robot is a good tool for STEAM education. The main topic is photosynthesis unit as circumstantiation and "Deep sea exploration robot", is creative activity, in elementary science subject. Students complete 13 basic course about robot, then accomplish subject-oriented 10 robot application course about above topic. Basic course contains math and science elements that students learn in regular curriculum. Application course is organized following steps, photosynthesis with oxygen sensors, brainstorming, idea derivation, robot design, robot construction, demo and presentation and so on. These courses have elements of STEAM. Finally teacher has face-to-face meeting with parents and students. Most have positive aspects about this process in terms of creativity, study attitude, and school life. Specially low-ranking students win a prize in robot competition. So they can gain confidence and accomplishment. This paper don't show statistic chart, but we surely knew that robot education for STEAM education seriously affect creativity huminity and job search.

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Processing Underwater Images for Information Extraction of Deep Seabed Manganese Nodules as New Energy Resource (미래 에너지 자원탐사를 위한 수중카메라 영상처리에 의한 심해저 망간단괴 정보추출)

  • Lee, Dong-Cheon;Yun, Seong-Goo;Lee, Young-Wook;Ko, Young-Tak;Park, Cheong-Kee
    • Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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    • v.27 no.6
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    • pp.679-688
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    • 2009
  • Worldwide exploring and research for manganese nodules, as new energy resource, distributed on the deep seabed have progressed recently. Korea Ocean Research & Development Institute(KORDI) is a central organization to exploit the manganese nodules in the Pacific Ocean with 5,000m depth. Precise exploration is required for estimating amount of recoverable deposit, and this task could be accomplished by processing digital image processing techniques to the images taken by underwater camera system. Image processing and analysis provide information about characteristics of distribution of the manganese nodules. This study proposed effective methods to remove vignetting effect to improve image quality and to extract information. The results show more reliable information could be obtained by removing the vignetting and feasibility of utilizing image processing techniques for exploring the manganese nodules.

S-wave Relative Travel Time Tomography for East Asia (동아시아 S파 상대 주시 토모그래피)

  • Cho, Seongheum;Chang, Sung-Joon
    • Geophysics and Geophysical Exploration
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    • v.20 no.1
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    • pp.18-24
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    • 2017
  • We performed seismic imaging based on relative S-wave travel times to examine S-wave velocity of upper mantle structure beneath East Asia. We used teleseismic events recorded at 129 broadband stations of the Korea Institute of Geoscience and Mineral Resources (KIGAM), Korea Meteorological Administration (KMA), and National Research Institute for Earth Science and Disaster Prevention (NIED). Relative travel time residuals were obtained by a multi-channel cross-correlation method designed to automatically determine accurate relative phase arrival times. The resulting images show high-velocity anomalies along plate boundaries around the Japanese islands region. These anomalies may indicate subducting Pacific and Philippine Sea plates. On the other hand, a low-velocity anomaly is revealed beneath east of the Korean peninsula down to around 300 km depth, which is thought to be related to the formation of the Ulleung basin and the Ulleung island. Low-velocity anomalies revealed beneath the Jeju island may imply that the formation and volcanism of the Jeju island have been caused by magmatic sources from the deep mantle.

A study on the characteristics of difference arrow using three-dimensional MT(Magneto-Telluric) modeling (3차원 전도체의 공간적 위치 및 크기에 따른 차이 지시자의 특성 연구)

  • Yang, Jun-Mo;Oh, Seok-Hoon;Lee, Duk-Kee;Kwon, Byung-Doo;Youn, Yong-Hoon
    • Journal of the Korean Geophysical Society
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    • v.5 no.4
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    • pp.305-319
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    • 2002
  • The three-dimensional MT(Magneto-Telluric) modeling is performed to examine the validity of difference arrow of GDS(Geomagnetic Depth Sounding) survey, In this paper, we investigate the validity of the difference arrow on three configurations of conductors; which is located 1) at surface, 2) at the deep part and 3) vertically extended f개m surface to the deep part, respectively, For conductors located at surface, the validity of difference arrows is certified in our numerical model when long periods over 40 minutes are used or the distance between sea and conductor is over 150 km. However, for conductors located at the deep part, the validity of difference arrow is dependent on the size of conductors. Further, if the size of conductor is adequately larger than that of our model, we recognize the possibility that the mutual coupling of them influences up to longer periods, Moreover, in case of conductors which is vertically extended from surface to the deer part, the mutual coupling of them is reinforced for all periods, especially for longer periods, so that the validity of difference arrow is considerably in doubt. Therefore, to remove the known conductor effect such as the sea effect from the observed induction arrow, the mutual coupling between them must be examined. The difference arrow that certifies the validity in this way can only provide the Subsurface information based on physical supports.

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