• Journal of the Society of Naval Architects of Korea
• /
• v.44 no.4
• /
• pp.389-397
• /
• 2007

This research describes a framework to compare and analyze the icebreaker(Terry Fox) resistance in pack ice condition between with a refrigerated ice and a synthetic ice. Model tests with a refrigerated ice have been conducted at Institute for Ocean Technology (IOT/NRC) and the tests with a synthetic ice were conducted at Pusan National University towing tank. For the validation of further tests of measurement and accuracy, the open water tests were first carried out with same model ship to compare the test results of both Institutes. Two different size of the wax-type synthetic ice were used and tests were conducted in pack ice of three different concentration ice conditions. The test results show that the difference of resistance between with synthetic and with refrigerated ice becomes larger according to the increase of ship speed. Although the quantity of resistance difference is not so small in high speed range, the present study is predicted to be used as a useful correlation between synthetic and refrigerated ice.

• Journal of Ocean Engineering and Technology
• /
• v.11 no.3
• /
• pp.144-152
• /
• 1997

본 논문에서는 1년생 빙맥에 의하여 해양구조물에 작용하는 하중을 추정할 수 있는 모델을 제시하였다. 1년생 빙맥을 수면하부(keel), 수면상부(sail), 경화층(consolidated layer)의 3부분으로 나누어 각 부분에 의한 하중을 추정할 수 있는 방법을 논의하였다. 수면하부는 얼음조각(ice rubble)이 층으로 쌓여져 형성된 것이므로 수면하부에 의한 하중추정을 할 때 얼음조각을 선형 Mohr-Coulomb재료로 생각하여 토질역학(soil mechanics)의 이론을 사용하였다. 수면상부에 의한 하중도 토질역학 이론을 이용하여 추정하였으며 경화층에 의한 하중은 Korzhavin식을 이용하여 추정하였다. 제시한 모델을 이용하여 빙맥하중 추정에 미치는 인자들의 영향을 검토하였다.

• Journal of Life Science
• /
• v.27 no.5
• /
• pp.584-590
• /
• 2017

Antifreeze proteins (AFPs) bind to ice crystals and inhibit their growth. AFPs are essential for the survival of organisms living in subzero environments. Type I AFP (AFP37) isolated from winter flounder is an ${\alpha}$-helical peptide of 37 residues long. In this study, we attempted to develop short AFP fragments with higher activity and solubility. We designed and synthesized N-terminal 15 and 21 residue-long AFPs, designated AFP15 and 21. Also dimerized AFP15 and 21, designated dAFP15N and dAFP21N, respectively, were generated through disulfide bonds between peptides containing CGG residues added to the N-terminus of AFP15 and AFP21 (designated AFP15N and 21N). Their helical contents and antifreeze activities were assessed using circular dichroism (CD) spectroscopy and a nanoliter osmometer, respectively. The helical content of AFP15 AFP21, AFP15N, AFP21N, dAFP15N and dAFP21N was 47, 48, 23.8, 28, 49.1, and 52%, respectively compared to that of wild type AFP37; the antifreeze activity was 8.4, 9.3, 0.05, 5.6, 12.1, 11.2% respectively, compared to that of wild type AFP37. Contrary to our anticipation, the dimerized peptides showed almost the same antifreeze activity as their monomeric counterparts. These results indicate that the dimerized peptides behave as monomeric peptides due to the high rotational freedom of disulfide bonds connecting two monomeric peptides. The star-shaped ice crystals generated by the peptides also demonstrated weak interaction between ice and peptides.

• Water for future
• /
• v.21 no.4
• /
• pp.399-406
• /
• 1988

Presented in this paper is a brief summary of the basic theory and observation from a laboratory investigation aimed at determining flow characteristics and ice jam topography in a sinuous channel, and in a single-bend channel. The sinuous channel comprised thirteen $90^{\circ}$ bends and was of comparatively small s\aspect ratio. The single-bend channel was a $180^{\circ}$ bend, which was an order of magnitude large in width as well as aspect ratios than the sinuous channel. The simulated ices were polyethylene and polypropylene beads and block. The streamwise velocities near the bottom were larger than that of surface in sinuous channel and forming ice jam in sinuous channel, this phenoumena were found strongly. Jams were generally thicker along the inner bank of bends. The path of maximum-streamwise velocity was displaced towards approachs side of the inner bank of bends. Radial variation of jam thickness was to be regular by increasing size of ice fragments. The rate of jam head progression around outer bank of the single bend was faster than that of inner bank and its velocity was roughly steady. With increasing Froude number, jm thickness became less uniformly distributed; being generally thicker along the inner bank and near the jam's toe. Two-layer model might be adaptable for the computing the streamwise velocity in shallow river bends. Two cells of secondary flow cound be expected in ice covered-river bends.