• 제목/요약/키워드: ice-5

검색결과 808건 처리시간 0.021초

Synchronized Expression of Two Bombyx mori Caspase Family Genes, ice-2 and ice-5 in Cells Induced by Ultraviolet Irradiation

  • Wang, Wenbing;Sun, Ying;Song, Lina;Wu, Yan;Wu, Huiling
    • International Journal of Industrial Entomology and Biomaterials
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    • 제17권1호
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    • pp.121-124
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    • 2008
  • The caspase family proteins play an important role in programmed cell death (apoptosis). To date, the expression profiles of the caspase family genes in Bombyx mori (Bm) are poorly known. In this study, we examined the expression profiles of two novel Bm caspase family genes (ice-2 and ice-5), the potential change of the mitochondrial membrane and the morphology in Bm cells after stimulation of ultraviolet (UV) irradiation. The results showed the potential change of the mitochondrial membrane occurred at 5 hours after UV irradiation treatment. Analysis of fluorescent quantitative RT-PCR demonstrated that both the ice-2 and ice-5 might be involved in UV induced apoptosis in Bm cells. Notably, after UV irradiating, expression pattern of ice-2 and ice-5 were remarkably different. The ice-2 gene was highly expressed at two time points, 0.5 and 5 hours after UV stimulating, while the expression level of ice-5 only peaked at 5 hours after UV stimulating. It indicated that apoptosis induced by UV irradiation was involved in the mitochondrial pathway and the two isoforms of Bm ice may act but play different role during the apoptosis of Bm cells.

빙수조 모형시험법 개선 연구 (A Study on Improvement of Ice Model Test Procedure)

  • 이춘주;조성락
    • 대한조선학회논문집
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    • 제45권5호
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    • pp.562-568
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    • 2008
  • In this study, the target FSICR class is 1A whose target thickness of the brash ice is 46 mm in model scale. Normally ice floes for brash ice do not exceed 2 m in full scale, so the model ice sheet was cut by about 10 cm by 10 cm using hand saws. Since the target thickness of brash ice is 46 mm, 46 mm ice sheet makes one layer brash ice. For 23 mm thickness ice sheet, two layers should be accumulated to reach 46mm brash ice thickness. For 15mm thickness ice sheet, three layers need to be accumulated as the same as those in 23 mm ice sheet. New methodology to produce a brash ice was proposed. The results showed that it would be important to use multi-layer rather than single layer possibly because of significant thrust deduction from the propeller-ice interaction in the present ice condition (FSICR 1A).

사각 빙해수조에서의 Pack Ice 모형시험 기법 개발 (Development of Model Test Methodology of Pack Ice in Square Type Ice Tank)

  • 조성락;유창수;정성엽
    • 대한조선학회논문집
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    • 제48권5호
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    • pp.390-395
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    • 2011
  • The main purpose of ice model basin is to assess and evaluate the performance of the Arctic ships and offshore structures because the full-scale tests in ice covered sea are usually very expensive and difficult. There are various ice conditions, such as level ice, brash ice, pack ice and ice ridge, in the real sea. To estimate their capacities in ice tank accurately, an appropriate model ice sheet and prepared ice conditions copied from actual sea ice conditions are needed. Pack ice is a floating ice that has been driven together into a single mass and a mixture of ice fragments of varying size and age that are squeezed together and cover the sea surface with little or no open water. So Ice-class vessels and Icebreaker are usually operated in pack ice conditions for the long time of her voyage. The most ice model tests include the pack ice test with the change of pack ice concentration. In this paper, the effect of pack ice size and channel breadth in pack ice model test is conducted and analyzed. Also we presented some techniques for the calculation of pack ice concentration in the model test. Finally, we developed a new model test methodology of pack ice condition in square type ice tank.

후빙기조륙운동 보정을 통한 한반도 주변 해역의 절대해수면 변화 분석 (Analysis of Absolute Sea-level Changes around the Korean Peninsula by Correcting for Glacial Isostatic Adjustment)

  • 김경희;박관동;임채호;한동훈
    • 한국지구과학회지
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    • 제32권7호
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    • pp.719-731
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    • 2011
  • 국립해양조사원 39개소 조위관측소의 후빙기조륙운동(Glacial Isostatic Adjustment, GIA)에 의한 지각변동 속도를 ICE-3G와 ICE-5G 모델로 예측하였다. 또한 위도 $32^{\circ}-38.5^{\circ}N$, 경도 $124^{\circ}-132^{\circ}E$ 범위의 한반도 지역을 $0.5^{\circ}{\times}0.5^{\circ}$ 격자로 분할하고 각 격자점에서의 GIA 지각변동 속도를 계산하였다. 그 결과 ICE-3G 모델의 경우 한반도 GIA 수직 지각변동은 평균 0.33 mm/yr이고, ICE-5G 모델의 경우 평균 1.21 mm/yr의 속도로 지각변위가 발생하는 것으로 나타났다. 최신 Ice model인 ICE-5G 모델을 사용할 경우 한반도에서도 약 1 mm/yr 이상의 비교적 높은 GIA 수직 지각변동이 발생하므로 절대해수면 변동을 산정하기 위해서 GIA에 의한 수직변위를 보정해야 함을 확인하였다. 따라서 국립해양조사원에서 제공하는 13개 조위관측소의 상대해수면 변동률에서 ICE-5G 모델에 의한 GIA 지각변동 속도를 보정하여 절대해수면 변동률을 결정하였다. 절대해수면 상승속도를 분석한 결과 GIA 지각변동 속도를 보정한 절대해수면 변동률은 한반도 해역에서 평균 5.04 mm/yr의 상승속도를 나타냈으며, 제주 해역은 평균 8.84 mm/yr로 다른 해역보다 높은 이상 상승률을 나타냈다.

해빙과의 접촉 면적을 고려한 국부 빙압력 추정 연구 (Study on Estimation of Local Ice Pressures Considering Contact Area with Sea Ice)

  • 김태욱;이탁기
    • 한국해양공학회지
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    • 제28권5호
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    • pp.423-428
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    • 2014
  • Ice loads may be conveniently categorized as local ice loads and global ice loads. Local ice loads are often defined as ice pressures acting on local areas of shell plates and stiffeners. Therefore, local ice loads are defined in all ice class rules. However, directly measuring the local ice pressure using the actual ice class vessel is a very difficult task because appropriate instruments for direct measurement must be installed on the outer hull, and they are easily damaged by direct ice contacts/impacts. This paper focuses on the estimation of the local ice pressure using the data obtained from icebreaking tests in the Arctic sea in 2010 using the Korean icebreaking research vessel (IBRV) ARAON. When she contacted the sea ice, the local deformation of the side shell was measured by the strain gauges attached to the inside of the shell. Simultaneously, the contact area between the side shell and sea ice is investigated by analyzing the distribution of the measured strain data. Finally, the ice pressures for different contact areas are estimated by performing a structural analysis.

쇄빙연구선 "Araon"호를 활용한 빙해역 속력 시운전에 관한 연구 (A Study on the Speed Sea Trial on the Ice Field for Ice Breaking Research Vessel "Araon")

  • 김현수;이춘주;정성엽;최경식
    • 대한조선학회논문집
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    • 제48권5호
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    • pp.421-425
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    • 2011
  • To know the speed performance of "ARAON" in Arctic ice field, the measurement of ice properties which is ice thickness & strength, snow depth and free board were performed on July 2010. The measuring method of nautical signals such as heading angle, power of engine, wind & current information etc. was described in this paper. The speed sea trials in ice were performed on the four different positions with different ice properties and engine powers because the uniform level ice is not detected in the Chukchi Sea. The test field was partially constrained ice floe with hummocks and it was superposed with small broken ice pieces each other. All of the measured ice properties were compared and evaluated according to the results of sea trial. The relations between speed, ice thickness, strength and power were summarized. Consequently according to the sea trial results, the speed of ARAON is 2.78knots at the 2.49m ice thickness with 6.55MW engine power.

북극해에서 계측된 국부 빙하중에 대한 선속 및 빙두께 영향 (Effects of Ship Speed and Ice Thickness on Local Ice Loads Measured in Arctic Sea)

  • 이탁기;이종현;임채환;최경식
    • 한국해양공학회지
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    • 제27권5호
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    • pp.82-87
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    • 2013
  • The icebreaking research vessel ARAON conducted her second ice trial in the Arctic Ocean during the summer season of 2010. During this voyage, the local ice loads acting on the bow of the port side were measured using 14 strain gauges. The measurement was carried out during icebreaking while measuring the thickness of the ice every 10 m. The obtained strain data were converted to the equivalent stress values, and the effects of the ship speed and ice thickness on the ice load were investigated. As a result, it was found that a faster speed produced a larger stress, according to the variation in the peak values below an ice thickness condition of 1.5 m. Meanwhile, the effect of the ice thickness on the ice load was not clear.

Temporal Variation of Air Temperature in Ice-Valley at Milyang in Association with Ice Formation

  • Lee, Soon-Hwan;Hwang, Soo-Jin
    • 한국지구과학회지
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    • 제28권5호
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    • pp.598-602
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    • 2007
  • A long-term in situ observation was carried out in the Ice-valley at Milyang in order to explain the factors and processes associated with the summertime ice formation. The variation of temperature inside Ice-valley in relation with ice formation in summer time was found to depend on precipitation rate in spring and cold air sinking in autumn and winter. The rate of temperature rising tends to correspond to sensible heat release depending on the precipitation amount at the freezing location. The reason of the cold air accumulation in a talus in the Ice-valley is the cold air sinking over the surface of talus due to the occurrence of outside clod air mass and the accumulated cold air from autumn to spring flow outside at the bottom of talus. The out-flowing cold air can result in the ice formation in the hot summer.

실해역 해빙 크기에 따른 Araon호의 쇄빙성능 비교연구 (Comparative Study of Ice Breaking Performance according to Scale of Sea Ice on Ice Field)

  • 이춘주;김현수;최경식
    • 한국해양공학회지
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    • 제28권1호
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    • pp.28-33
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    • 2014
  • The Korean icebreaking research vessel "Araon" performed four sea trials in the Arctic and Antarctic Seas. The ice properties, such as the ice thickness, floe size, ice strength, and power of the vessel were quite different in these trials. To compare the speeds of ship with the same ice strength and power, the AARC (Arker Arctic Research Center) method is used with a vessel power of 10 MW and an ice strength of 630 Pa in this paper. Based on the analysis results, the speed of the ship was 1.62 knots (0.83 m/s) with a 1.02-m ice thickness and 2.5-km floe size, 5.3 knots (2.73 m/s) with a 1.2-m ice thickness and 1.0-km floe size, and 13.8 knots (7.10 m/s) with a 1.1-m ice thickness and 200-m floe size. The analysis results showed that the ship speed and floe size have an inversely proportional relationship. Two reasonable reasons are given in this paper for the final result. One is an ice breaking phenomenon, and the other is the effect of the ice floe mass. For the breaking phenomenon, the ice breaking force is very small because the ice floe is not breaking but tearing when a ship is passing through a small ice floe. Regarding the effect of the ice floe mass, it is impossible for a ship to push and tear an ice floe if the mass of the ice floe is too large compared to the mass of the ship. The velocity of the ship decreases when the ice floe has a large mass and a large size because the ship has to break the ice floe to move forward.

아이스크림 제품류에 함유되어 있는 지방함량 및 지방산조성 (Contents and Fatty Acid Compositions in Fats Extracted from Ice Creams and Ice Cream-Related Products)

  • 신민경;오현희;황금택
    • 한국식품영양과학회지
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    • 제35권6호
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    • pp.721-728
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    • 2006
  • 본 연구에서는 시중에 유통되는 일반 '아이스크림' 22개 제품과 프리미엄 '아이스크림' 10개 제품, '아이스밀크' 22개 제품, '샤베트' 4개 제품, '비유지방 아이스크림' 11개 제품과 '빙과류'인 '비유제품 아이스크림' 5개 제품을 수집하여, 이들 아이스크림 제품류에서 추출한 지방의 조지방 함량과 지방산조성을 분석하였다. 일반 '아이스크림', 프리미엄 '아이스크림', '아이스밀크'에는 지방이 각각 $5{\sim}11%,\;13{\sim}17%,\;2{\sim}10%$ 함유되어 있었다. '샤베트', '비유지방 아이스크림', '비유제품 아이스크림'에는 지방이 각각 $2{\sim}7%,\;4{\sim}11%,\;1{\sim}2%$함유되어 있었다. 일반 '아이스크림' 22개 제품 중 14개 제품, 프리미엄 '아이스크림' 10개 모든 제품, '아이스밀크' 22개 제품 중 11개 제품에서 분리한 지방에는 포화지방산이 $63{\sim}75%$, 트랜스지방산이 $2{\sim}5%$ 함유되어 있었는데, 이는 우유나 버터에 있는 지방과 유사한 조성이었다. 그러나 일반 '아이스크림' 8개 제품과 '아이스밀크' 11개 제품에서 추출한 지방에는 lauric acid가 각각 $11{\sim}28%$$11{\sim}34%$ 함유되어 있었는데, 이는 우유나 버터의 지방을 조성하고 있는 lauric acid 함량보다 3배 이상 높은 값으로서 유지방만을 지방원료로 사용하였다고 보기는 어렵다. 이들 19개 제품 중에서 5개 제품에서만 유지방 이외에 '야자유'나 '정제가공유지'를 사용하였다고 표시하였다. '샤베트', '비유지방 아이스크림', '비유제품 아이스크림'에서 분리한 지방에는 포화지방산이 각각 $81{\sim}92%,\;76{\sim}99%,\;84{\sim}99%$ 함유되어 있었으며, lauric acid가 각각 $33{\sim}34%,\;17{\sim}45%,\;27{\sim}46%$로써 가장 많은 부분을 차지하고 있었다.