• Title/Summary/Keyword: Above sea level

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A Strength Analysis of a Hull Girder in a Rough Sea

  • Kim, Sa-Soo;Shin, Ku-Kyun;Son, Sung-Wan
    • Selected Papers of The Society of Naval Architects of Korea
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    • v.2 no.1
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    • pp.79-105
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    • 1994
  • A ship in waves is suffered from the various wave loads that comes from its motion throughout its life. Because these loads are dynamic, the analysis of a ship structure must be considered as the dynamic problem precisely. In the rationally-based design, the dynamic structural analysis is carried out using dynamic wave loads provided from the results of the ship motion calculation as a rigid body. This method is based on the linear theory assumed low wave height and small amplitude of motion. But at the rough sea condition, high wave height, compared with ship's depth, induce the large ship motion, so the ship section configuration under waterline is rapidly changed at each time. This results in a non-linear problem. Considering above situation in this paper, a strength analysis method is introduced for the hull girder among waves considering non-linear hydrodynamic forces. This paper evaluates the overall or primary level of the ship structural dynamic loading and dynamic response provided from the non-linear wave forces, and bottom flare impact forces by momentum slamming theory. For numerical calculation a ship is idealized as a hollow thin-walled box beam using thin walled beam theory and the finite element method is used. This method applied to a 40,000 ton double hull tanker and attention is paid to the influence of the response of the ship's speed, wave length and wave height compared with the linear strip theory.

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The feature of geomorphology and a factor of retreat in Franz Josef Glacier (프랜츠 요셉 빙하의 지형적 특성과 빙하 후퇴의 원인)

  • 심인선
    • Journal of the Speleological Society of Korea
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    • no.63
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    • pp.61-79
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    • 2004
  • The Franz Josef Glacier is sited 250 m above sea level. The moisture westerly winds from Tasman Sea and the feature of the alp geomorphology have made the Franz Josef Slatier. That is why the Franz Josef Slatier is. The Franz Josef Slatier has receded during the past century in response to global warming since the end of the Little ice Age in the 1890s. Even between 2002 and 2003, the Franz Josef Glacier is confirmed retreat ins. This is confirmed by climate factors. The expressing of the Franz Josef Slatier retreating in 2003 which is advanced air temperature and amount of precipitation in 1998 than compared another years. There are lots of metamorphic rock as known biotite, schist, greywack and the Alpine Fault is passing near the Franz Josef Glacier. The grooved and scratching trend surface the rock are observed as the evidence of retreating glacier left.

Experimental Study on Wave Overtopping Rate of Wave Overtopping Control Structure for Wave Energy Conversion (파랑 에너지 변환을 위한 월파제어구조물의 월파량 산정 실험)

  • Shin, Seung-Ho;Hong, Key-Yong
    • Journal of Ocean Engineering and Technology
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    • v.19 no.6 s.67
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    • pp.8-15
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    • 2005
  • Wave energy has been considered to be one of the most promising energy resources for the future, as it is pollution-free and an abundant natural resource. However, since it has drawbacks of non-stationary energy density, it is necessary to change the wave energy into a simple concentrated energy. Progressive waves in a coastal area can be amplified, swashed, and overtopped by a wave overtopping control structure. By conserving the quantity of overflow in a reservoir, the kinetic energy of the waves can be converted to the potential energy with a hydraulic head above the mean sea level. The potential energy in the form of a hydraulic head can be utilized to produce electric power, similar to hydro-electric power generation. This study aims to find the most optimal shape of wave overtopping structure for maximum overtopping volume of sea water; for this purpose, we carried out the wave overtopping experiment in a wave tank, under both regular and irregular wave conditions.

A study on the ice and snow loading condition in Taebaek and Sabuk area in Gangwon province for the construction of KEPCO 765kV transmission lines (한전 765 kV 송전선로 건설을 위한 강원도 태백.사북지역 착빙설 하중조건 검토)

  • Park, K.H.;Kim, Y.W.;Won, B.J.
    • Proceedings of the KIEE Conference
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    • 1996.07c
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    • pp.1923-1924
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    • 1996
  • Some part of the route in KEPCO 765kV transmission line being constructed passes through a high mountain area which is 800m above the sea level (Taebaek, Sabuk area in Gangwon province). This area is the top part of Taebaek mountains corresponding to the backbone of korean peninsula and has lots of snow during the winter season because the winter seasonal wind gone up along the mountainside of Taebaek Mts. meets open air of the East sea. KEPCO has experienced 63 faults of T/L between 1968 and 1993 in this area, which is a very serious problem. Especially 154kV Hwang-Ji T/L fault in 1990, 2 was a unprecedented case which needs to be analyzed carefully to take proper measures. After reviewing ice and snow loading conditions and analyzing the fault of Hwang-Ji T/L, we're going to determine the revisement of ice and snow loading condition in this area to increase reliability of 765kV transmission line.

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Wind Resource Assessment on the Western Offshore of Korea Using MERRA Reanalysis Data (MERRA 재해석자료를 이용한 서해상 풍력자원평가)

  • Kim, Hyun-Goo;Jang, Moon-Seok;Ryu, Ki-Wahn
    • Journal of Wind Energy
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    • v.4 no.1
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    • pp.39-45
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    • 2013
  • Massive offshore wind projects of have recently been driven in full gear on the Western Offshore of Korea including the 2.5 GW West-Southern Offshore Wind Project of the Ministry of Trade, Industry and Energy, and the 5 GW Offshore Wind Project of the Jeollanamdo Provincial Government. On this timely occasion, this study performed a general wind resource assessment on the Western Offshore by using the MERRA reanalysis data of temporal-spatial resolution and accuracy greatly improved comparing to conventional reanalysis data. It is hard to consider that wind resources on the Western Sea are excellent, since analysis results indicated the average wind speed of 6.29 ± 0.39 m/s at 50 m above sea level, and average wind power density of 307 ± 53 W/m2. Therefore, it is considered that activities shall be performed for guarantee economic profits from factor other than wind resources when developing an offshore wind project on the Western Offshore.

Comparative Study of Antioxidant Activities at Different Cultivation Area and Harvest Date of the Gomchwi 'Sammany' Variety (곰취 '쌈마니' 품종의 재배지역 및 수확기별 항산화 활성 비교)

  • Suh, Jong Taek;Kim, Ki Deog;Sohn, Hwang Bae;Kim, Su Jeong;Hong, Su Young;Kim, Yul Ho
    • Korean Journal of Plant Resources
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    • v.33 no.4
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    • pp.245-254
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    • 2020
  • This study was conducted for the comparison of antioxidant activities in different cultivation areas, harvest date and processing statuses in the new variety 'Sammany' of Gomchwi (Fischer ligularia). The lowland was Gangneung, 20 m above sea level, and the highland was Daegwallyeong, 750 m above sea level. The total phenolic contents, flavonoids, DPPH free radical scavenging activities, and reducing power were analyzed by freezing and drying the raw and blanched of Gomchwi leaves from April 18th to July 15th, and extracting them through in the use of methanol. Total phenolic contents, flavonoids, DPPH free radical scavenging activities and reducing power were found to be more pronounced during May than they were in the period of early harvest on April 18th in the lowland, as well as to be more effective during June than in May in the highland. Total phenolic contents, flavonoids, DPPH free radical scavenging activities, and reducing power by region, harvest date, and processing status were more effective in May than the early harvest of April in flat areas, and antioxidant activity in the highlands was elevated as of June. When compared with raw and blench leaves, raw leaves exhibited higher antioxidant activities across the board. Highland cultivation also displayed higher antioxidant activities than did lowland cultivation. Combining the above results, the 'Sammany' variety of Gomchwi was found to be more active in terms of antioxidants, which were harvested in May in flat areas and June in the highlands. Also, consuming them raw showed higher antioxidant activity than when blanched.

Traits of Water Level Control by Sluice Gates and Halophyte Community Formation in Saemangeum (새만금 배수갑문 수위조절 특성과 염생식물 군락지 형성에 관한 연구)

  • Sin, Myoung-Ho;Kim, Chang-Hwan
    • Korean Journal of Environment and Ecology
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    • v.24 no.2
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    • pp.186-193
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    • 2010
  • In order to examine the traits of sluice gate water control, halophyte community formation and their inter-relations in Saemangeum, both water level condition and halophyte community formation were analyzed periodically and spatially on the topographic map with Surfer, Saemageum Spatial Analysis System, and related field reports. The traits of water level condition are that average water level in the growing period of halophytes was similar to annual average water level, annual low level and high level appeared in the growing period, and water level was usually maintained within a range of -1.0m~0.5m above mean sea level, but it has changed more frequently year by year. Routine water level control, natural disaster prevention, construction, and civil appeal took major percentages of the reasons for sluice gate's opening and shutting. Since 2007, not only the overall control frequency of sluice gate but also its control frequency for construction and natural disaster prevention have increased outstandingly. Halophyte community had formed at a rate of 1,209ha/year in the 4,315 ha land in 2008, 6.3 times larger than in 2005, and 2,382 ha above around 1.0m was estimated to be artificially vegetated, 89.1 % of the 2,673ha-size sown area. High water level was found to be a more possible determinant than average water level or low water level in halophyte community formation and it was thought to be secondary factors whether tillage was conducted or/and whether surface sealing formed.

Identification of Culturable Bioaerosols Collected over Dryland in Northwest China: Observation using a Tethered Balloon

  • Chen, Bin;Kobayashi, Fumihisa;Yamada, Maromu;Kim, Yang-Hoon;Iwasaka, Yasunobu;Shi, Guang-Yu
    • Asian Journal of Atmospheric Environment
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    • v.5 no.3
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    • pp.172-180
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    • 2011
  • The transfer of microorganisms is important process for ecosystems. Microorganisms in dryland can transport itself to wetland through atmospheric diffusion, but only few papers reported about the atmospheric bioaerosol present over dryland. We carried out the direct sampling using a tethered balloon over Dunhuang City, China's northwestern dryland. Bioaerosols were collected using a tethered balloon with a bioaerosol collector at 820 m above the ground (1,960 m above the sea level) around noon on August 17, 2007. The bioaerosols were cultured after the collection at Dunhuang Meteorological observatory. Two strains of molds were isolated using the Nutrient agar medium. About 400-bp 18S rRNA partial sequences were amplified by PCR and determined afterwards. The results of a homology search by 18S rRNA sequences of isolates in DNA databases (GenBank, DDBJ, and EMBL) and an observation of the form revealed that two bioaerosols in the convective mixed layer over Dunhuang City were Cladosporium sp. and Aspergillus sp.

Demography of Juniperus phoenicea L. and Juniperus procera Hochst. ex Endl. populations at Sarrawat Mountains, Southwest of Saudi Arabia

  • Yassin Mohamed Al-Sodany;Hatim Matooq Al-Yasi;Salma Kamal Shaltout
    • Journal of Ecology and Environment
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    • v.48 no.1
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    • pp.49-59
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    • 2024
  • Background: The present study aims to identify the pattern and size of Juniperus species (Juniperus phoenicea and J. procera) in the natural forests in terms of tree dimension, size structure and density, discussing the existing both species in Sarrawat Mountains for suggesting the preservation, conservation, and sustainable development. For achieving this, the height and mean crown diameter of each individual was measured based on 2-4 diameter measurements per ind. (506 ind. for J. phoenicea and 322 ind. for J. procera). Results: The size index of both species was classified into 7 classes: the first (< 100 cm) and the second (100-200 cm) classes were chosen to represent the juvenile stage. The total mean of the J. phoenicea population increased with the increase of altitude, while the whole population decreased after altitude of 2,000 m. The total mean of the J. procera population increased with the increase of altitude till altitude of 2,000-2,100 m. Conclusions: The present study indicated that both of species grow at low altitudes, they only grow at altitude above 1,700 m above sea level. The present study indicated that the study area has the two Juniperus spp. (J. phoenicea and J. procera) associated together all over the area. The results were discussed and compared with other related studies.

Wind Castle: The Natural Intelligence Control of Hallasan-Oreum-Batdam I (윈드캐슬: 한라산-오름-밭담의 자연지능 제어 I)

  • Lee, Moon-Ho;Kim, Jeong-Su
    • The Journal of the Institute of Internet, Broadcasting and Communication
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    • v.20 no.3
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    • pp.105-111
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    • 2020
  • We defined Jeju Wind Castle and analyzed the relationship between Hallasan-Oreum-Batdam, the main subject, for the first time. In Jeju, 1.5m high Batdam(Black Silk Road), 368 Oreums, Hallasan Mountain 1950m are all unique scenery. The verification of this paper demonstrates that Samdasoo's groundwater extraction sea level is equal to the height of Hallasan and that this problem is mathematically complete in neutral plane theory. Donnaeko(700meters above sea level)-Baeknokdamdongneung-Jindallebat-Seongpanak-Gyorae(453 meters)-Witsaeoreum(1700meters) is a rain belt that hits the low-air pressure air-conditioned North Pacific humidity rising from the southeast and the high-pressure cold air of Hallasan Peak. It rains a lot because - and + are neutral plane, which adds to zero. Hallasan is called Jinsan in Jeju history. The answer is Wind Castle. The number of Oreum in Jeju is 369 including Hallasan, and Batdam, which is about 1.5m high, does not collapse even with a typhoon blowing over 50m/s. Because the wind castle's core is 1.5 meters of Batdam and it is a triangular number.