• 대한조선학회논문집
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• 제56권2호
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• pp.117-127
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• 2019

Vessel's ice speed performances will be verified in ice sea trial but environmental conditions of ice fields are changeable according to the weather condition of ice trial area. Speed performance has to correct in the no wind, wave and current etc. after sea trial. Especially finding ice fields which is exact the same as owner's ice thickness and strength requirements is not easy. Therefore speed correction according to environment condition has to be done after sea trial measurements. Correction methods for ice thickness, ice strength, wave, wind and ship draft, trim, ice drift etc. are checked in ice sea trial based on literature review such as ISO standard, ITTC recommendation, journal papers and proceedings of conferences. Possibility of application for current and ice drift correction in ice field are discussed and measuring schemes and procedures of correction methods are described in this paper. All of correction schemes are calculated for 'Araon' which is ice breaking research vessel with Arctic and Antarctic ice field test results. Analyzed results shows that Araon is satisfied with her official ice speed performance of 3 knots with 10MW power at 1m ice thickness, 570kPa ice flexural strength.

• International Journal of Naval Architecture and Ocean Engineering
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• 제11권1호
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• pp.422-434
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• 2019

Several model-scale tests with a ship model have been performed in the ice tank of the Marine Technology Group in the Aalto University. The ship model of ice going tanker Uikku was mounted rigidly to the main carriage and towed through ice fields. The model tests were performed by changing ice thickness, drift angles and speeds in different ice fields. This paper reports the testing results and different phenomenon during model tests. The measured ice forces are presented and compared to level ice forces. The process of ice forces from broken ice on the ship is also analyzed for some typical tests. The research work could provide guidance on marine structures operating in waters covered by broken ice.

• 한국해양공학회지
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• 제25권2호
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• pp.55-61
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• 2011

A field trial in an ice-covered sea is one of the most important tasks in the design of icebreaking ships and offshore structures. To correctly estimate the ice load and ice resistance of a ship's hull, it is essential to understand the material properties of sea ice during ice field trials and to use the proper experimental procedure for gathering effective ice data. The first Korean-made icebreaking research vessel, "ARAON," had her second sea ice trial in the Arctic Ocean during the summer season of 2010. This paper describes the test procedures used to obtain proper sea ice data, which provides the basic information for the ship's performance in an ice-covered sea and is used to estimate the correct ice load and ice resistance of the IBRV ARAON. The data gathered from the sea ice in the Chukchi Sea and Beaufort Sea during the Arctic voyage of the ARAON includes the temperature, density, and salinity of the sea ice, which was believed to be from two-year old ice floes. This paper analyses the gathered sea ice data in comparison with data from the first voyage of the ARAON during her Antarctic Sea ice trial.

• 한국해양공학회지
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• 제16권1호
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• pp.27-35
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• 2002

The interaction of grounded ice ridges with underlying seabed is one of the major considerations in the design of Arctic pipeline system. Previously several ice scour models were developed by researchers to describe the ice scour-seabed interaction mechanism. In view of possible improvements, a comparative study of those ice scour models is performed and their limitation in modeling is discussed. Simple laboratory tests are carried out and then the shape pattern of deposited soil around the ice model is newly defined. Unlike the rectangular idealization of an ice block, in this modified ice scour model, trapezoidal cross sections are assumed to represent the typical shape of an ice ridge based on the field observation data. With the horizontal and vertical motion of ice model, the ice scour depth and soil reacting forces on seabed are calculated with varying the keel angle of an ice ridge.

• 한국해양공학회지
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• 제25권1호
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• pp.49-55
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• 2011

The EG/AD/S model ice, originally developed by Timco (1986), was selected as the primary model ice material for the newly built MOERI Ice Model Basin in Korea. However, the existence of a sugar component in the EG/AD/S mixture may cause a serious maintenance problem, as described in certain references. This study focuses on the tests of the mechanical properties of the EG/AD/S and the EG/AD model ice. In order to understand the influence of sugar in the original EG/AD/S model ice and to find a possible substitute for sugar, a series of tests with the EG/AD model ice were performed, and the results were compared to those of the EG/AD/S model ice. The relatively large size of the MOERI Ice Model Basin made it difficult to control the initial strength of model ice, so it took a much longer time to achieve the target strength. In order to obtain a lower strength and stiffness for the model ice, the amount of chemical additives may be varied to achieve the desired strength level. This paper is a preliminary study aimed at seeking a possible substitute for the original EG/AD/S model ice for utilization in a large-scale ice tank. To understand the influence of sugar in the original EG/AD/S model ice, the mechanical properties of the EG/AD/S and EG/AD model ice, such as flexural strength, compressive strength, and elastic modulus, were tested in the laboratory condition and compared to each other. The warm-up procedure seems to be an important factor to reduce ice strength in the tests, so it is discussed in detail.

• Ocean and Polar Research
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• 제33권1호
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• pp.1-11
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• 2011

This study describes measurements of fast ice recorded on May 23, 2009, in Kongsfjorden (translated as 'Kongs Fjord'), an inlet on the west coast of Spitsbergen in the Svalbard Archipelago. Seasonal fast ice is an important feature for Svalbard fjords, both in relation to their physical environment and also the local ecosystem, since it grows seaward from the coast and remains in place throughout the winter. Ice thickness, snow, ice properties, and wind speed were measured, while SAR (Synthetic Aperture Radar) data was observed simultaneously observed two times from ALOS-PALSAR (L-band). Measured ice thickness was about 25-35 cm while the thickness of ice floe broken from fast ice was measured as 10-15 cm. Average salinity was 1.9-2.0 ppt during the melting period. Polarimetric data was used to extract H/A/alpha-angle parameters of fast ice, ice floe, snow and glacier, which was classified into 18 classes based on these parameters. It was established that the area of fast ice represents surface scattering which indicates low and medium entropy surface scatters such as Bragg and random surfaces, while fast ice covered with snow belongs to a zone of low entropy surface scattering similar to snow-covered land surfaces. The results of this study will contribute to various interpretations of interrelationships between H/A/alpha parameters and the wave scattering Phenomenon of sea ice.

• 대한원격탐사학회지
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• 제23권6호
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• pp.507-520
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• 2007

인공위성 수동 마이크로파(passive microwave, PM) 센서는 1970년대부터 극지 해빙의 면적비(sea ice concentration, SIC)와 표면 온도(ice temperature), 적설 두께(snow depth) 등을 관찰하고 있다. 특히 SIC는 기후 및 환경 변화 관찰을 위한 1차 요소로 고려되는 등 다양한 연구 분야에서 중요한 역할을 하기 때문에 PM SIC의 지속적인 검증과 보정이 필요하다. 본 연구에서는 2005년 7-8월 북극해의 가장 자리를 촬영한 KOMPSAT-1 EOC 영상으로부터 SIC를 계산하였고, 이를 NASA Team(NT) 알고리즘으로 계산된 SSM/I SIC와 비교하였다. EOC와 SSM/I NT SIC는 서로 다른 해상도와 관측 시각을 가지며 북극의 여름철 해빙 분포지역의 가장자리에서 해빙의 시공간적인 변화가 크기 때문에, 해빙의 유형을 고려하지 않았을 경우 0.574의 낮은 상관성을 보였다. 해빙의 유형에 따른 SSM/I NT SIC를 검증하기 위하여 EOC 영상으로부터 정착빙, 부빙, 유빙으로 해빙 형태를 분류하였고, 각 유형 별로 EOC와 SSM/I NT SIC를 비교하였다. 정착빙의 면적비는 EOC와 SSM/I NT SIC 사이에서 평균 오차가 0.38%로 매우 유사한 값을 나타냈다. 이는 정착빙의 시공간적인 변화가 작기 때문이며, 표면에 쌓인 눈은 건조한 상태일 것으로 추정되었다. 부빙의 경우 NT 알고리즘에서 면적비가 과소평가되는 빙맥(ice ridge)과 new ice가 많이 관찰되었으며, 이로 인해 SSM/I NT SIC는 EOC보다 평균 19.63%작은 값을 나타냈다. 유빙 지역에서 SSM/I NT SIC는 EOC보다 평균 20.17% 큰 값을 가진다. 유빙은 부빙의 가장자리와 가까운 지역에 위치하기 때문에 SSM/I의 넓은 IFOV 내에 비교적 높은 SIC를 가지는 부빙이 포함되어 오차를 일으킬 수 있다. 또한 유빙표면에 쌓인 수분 함량이 높은 눈의 영향으로 SSM/I NT SIC가 과대 측정되었을 것으로 사료된다.

• 설비공학논문집
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• 제14권1호
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• pp.31-37
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• 2002

This paper is concerned with the development of a new method for making and separating ice and saving floated ice by installing an evaporation plate at in-water within a storage tank. In a conventional harvest-type ice storage system, a tank saves ice by separating a formed ice from an installed evaporation plate, which is located above an ice storage tank as an ice storage system. A new harvest-type method shows very good heat transfer efficiency than a convectional method. It is because the evaporation panel is directly contacted with water in a storage tank. Also, at a conventional system a circulating pump, a circulating water distributor and a piping are installed, but these components are not necessary in a new method. In this study two kinds of ice storage systems are experimentally investigated to study the thermal characteristics of ice storage tanks. The results showed discharge of cold capacity of new type indicated the high values about 30~40% based on five time of drive, the temperature difference of inlet/outlet occurred the big range about $1.3^{\circ}C$. So, the new type which makes ice in water showed superiorly.

• 대한원격탐사학회지
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• 제34권6_2호
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• pp.1165-1178
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• 2018

남극 빙붕의 붕괴 및 흐름속도의 변화는 빙상에 대한 지지력을 약화시킬 수 있어 해수면 상승에 잠재적인 원인이 될 수 있다. 이 연구에서는 2016년 4월 대규모 붕괴가 발생한 동남극 난센 빙붕에 대해 Landsat-7 Enhanced Thematic Mapper Plus(ETM+) 및 Landsat-8 Operational Land Imager(OLI) 영상을 이용하여 2000년부터 2017년까지의 연간 흐름속도 변화를 분석하였다. 흐름속도 산출을 위해 Landsat의 청색, 녹색, 적색, 근적외선, 전정색 및 첫 번째 주성분 영상 등 총 6개 영상에 orientation correlation 기법을 적용하고, 각각의 변위 산출 결과를 융합하는 다중분광 영상정합 기법을 사용하였다. Landsat 다중분광 영상정합은 난센 빙붕에서 전정색 단일 밴드 영상정합을 사용하는 경우보다 최소 14% 더 넓은 영역에 대해 신뢰할 수 있는 흐름속도를 산출하였고, Global Positioning System(GPS)로 관측된 흐름속도와 비교한 결과 ${\pm}2.1m\;a^{-1}$의 매우 작은 오차를 가지는 것으로 분석되었다. 난센 빙붕에서 2000-2017년 사이에 가장 급격한 흐름속도 증가를 나타낸 곳은 Drygalski 빙하설과 인접한 영역이었으며, 빙붕의 중앙 유선을 따라 측정된 흐름속도는 빙붕 전면(ice front)에 rift가 발달하기 전인 2010년까지 거의 변화가 없었다(${\sim}228m\;a^{-1}$). Rift가 발달하기 시작한 2011-2012년에 rift 상류에서 흐름속도의 가속화가 관측되었으나(${\sim}255m\;a^{-1}$), 이는 2010년에 비해 약 11% 빨라진 것에 불과하였다. 난센 빙붕의 rift가 완전히 발달한 2014년부터 rift 상류의 흐름속도는 다소 감소한 상태(${\sim}225m\;a^{-1}$)로 안정화 되었다. 이는 rift의 발달 및 빙붕 전면의 붕괴가 난센 빙붕의 흐름속도에 거의 영향을 주지 않았음을 의미한다.

• 농업과학연구
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• 제25권2호
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• pp.176-180
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• 1998

충남지역 농특산물인 밤 및 호도의 과육을 분말화하여 아이스크림 믹스의 원료로 1~5% 첨가하고 아이스크림을 제조한 후, over run, 제품의 조성분 및 관능검사를 실시한 결과는 다음과 같다. 1. Over run의 측정에 있어서는 밤 분말 첨가의 경우 35.75~38.81%로서 41.18%인 control구에 비하여 낮게 나타나고 호도 첨가구에 있어서는 36.31~40.38%로서 control구에 비하여 낮았다. 2. 제품의 화학적 조성은 밤 분말을 첨가한 아이스크림의 경우 무지고형분과 단백질이 31.05~31.73%, 4.48~4.78%로서 control구에 비하여 높았고 호도 첨가구에 있어서는 지방량이 12.21~21.38%, 단백질량이 4.63~5.27%로서 control구에 비하여 높은 함량을 나타내었다. 3. 관능검사 결과 밤 첨가 아이스크림은 향취와 맛에 있어서 control구에 비하여 우수하였고 호도 첨가구는 향취에 있어서 통계적인 유의성이 인정되는 (0.05%) 우수성을 나타내었다.