• International Journal of Naval Architecture and Ocean Engineering
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• 제11권1호
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• pp.542-552
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• 2019

The strength assessment is the most important part at the design of ice-class propeller. Based on ice rules for ice-class propeller in IACS URI3 and FEM, the strength assessment method of ice-class propeller is established in this paper. To avoid the multifarious meshing process of propeller blade, an automatic meshing method has been developed by dividing the propeller geometry into a number of 8-node hexahedron elements along radial, chordwise and thickness directions, then the loaded areas in five cases can easily be calculated and identified. The static FEM is applied to calculate the stress and deformation of propeller blade. The fair agreements between the results of the present method and ANSYS/Workbench demonstrate its robust and the feasibility, and also the method is able to produce smooth gradient field. The blade stress and deformation distributions for five load cases are studied, and then the strength of the whole blade is checked.

• 대한기계학회논문집A
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• 제22권1호
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• pp.227-237
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• 1998

In case the systems have radioactivity, toxic liquid or expensive fluid, and have to be performed repair work at one point of the system pipe, the formation of an internal ice plug by the removal of heat from the pipe is often consideredas a useful method. In this procedure, an annular jacket is placed around the pipe, and the jacket is then filled with liquid Nitrogen(-196.deg. C). Thermal analysis by the finite element method based on the laboratory experiments has been constructed. The result of the finite element analysis on the experimental model shows to be reasonable, and thus the finite element analysis for different pipe size, material and thickness has been performed to see if the ice plugging procedure in various applications can be safely performed without possibility of damage to the pipe. It has been confirmed that in carbon steel pipes the maximum stress is found around the boundary of the freezing jacket, and the stress increases as pipe thickness increases, but the maximum stress shows no consistency along the increment of the pipe diameter. The maximum stresses appear lower than yield stress in carbon steel. It has been also shown that in stainless steel pipes the maximum stresses are also found around the boundary of the freezing jacket, but almost the same value in spite of different pipe size an thickness, and the maximum stresses show slightly higher than the yield stress of the stainless steel.

• 대한원격탐사학회지
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• 제35권6_1호
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• pp.933-944
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• 2019

이 연구에서는 영상레이더(synthetic aperture radar; SAR) 이중차분간섭기법(Double-Differential Interferometric SAR; DDInSAR)을 이용하여 남극 로스 빙붕(Ross Ice Shelf)의 동쪽(A지역)과 서쪽(B지역)에 위치한 육지 경계부 지역의 조위변형을 분석하고, 조위예측 모델의 정밀도와 빙붕의 영률(Young's modulus) 추정을 위해 2015-2016년에 획득된 총7장의 Sentinel-1A SAR 영상을 획득하였다. 먼저, 남극 로스해(Ross Sea)에 대한 대표적인 조위예측 모델인 Ross Sea Height-based Tidal Inverse (Ross_Inv) 모델과 DDInSAR영상에서 추출된 빙붕의 조위변형을 비교한 결과, 모델의 조위예측 오차는 동쪽에서는 3.86 cm로 분석되었으며 조위모델에서 역기압효과가 필수적으로 보정되어야 함을 확인하였다. 그러나 서쪽에서는 역기압효과 보정 후에도 큰 오차가 발생하여 조위모델이 부정확할 수 있음을 확인했다. 또한, 조위변형이 나타나는 힌지 영역(hinge zone)의 폭과 얼음두께의 상관성을 나타내는 1차원 탄성 보 모델에 의거하여 얼음의 영률을 계산하였다. 이를 위해 DDInSAR 영상에서 조위에 의한 변위가 나타나기 시작하는 곳을 지반선(grounding line)으로, 조위에 의한 최대변위가 나타나는 지점을 힌지선(hinge line)으로 새롭게 정의했고, 이두선 사이를 힌지 영역으로 정의했다. 반무한 평면체를 가정한 1차원 탄성 보 모델에 의하면 힌지 영역의 폭은 얼음두께의 0.75승에 정비례한다. DDInSAR에서 나타나는 힌지 영역 중 지반선과 힌지선이 직선에 가까운 지역에서 힌지 영역의 폭을 측정하였고, 이를 BEDMAP2 얼음 두께의 0.75승과의 선형 회귀 분석을 통해 로스 빙붕 동쪽과 서쪽 힌지 영역의 영률을 1.77±0.73 GPa로 추정할 수 있었다. 이러한 방법으로 향후 Sentinel-1 영상이 축적되면 더 정밀한 영률을 추정할 수 있을 것으로 기대된다.

• 한국전산유체공학회지
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• 제18권3호
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• pp.51-59
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• 2013

A significant change in aerodynamic characteristics of wind turbine blade can occur by ice formed on the surface of the blade operated in cold climate. The ice accretion can result in performance loss, overloading due to delayed stall, and excessive vibration associated with mass imbalance. In this study, the impact of ice accretion on the aerodynamic characteristics of NREL 5MW wind turbine blade sections is examined by a CFD-based method. It is shown that the thickness of ice accretion increases from the root to the tip and the effects of icing conditions such as relative wind velocity play a significant role in the shape of ice accretion. In addition, the computational results are used to assess the degradation in the lift and drag coefficients of the blade sections.

• International Journal of Air-Conditioning and Refrigeration
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• 제7권
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• pp.1-10
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• 1999

In this study, a numerical analysis is made on the ice-formation for laminar water flow inside a stenotic tube. The study takes into account the interaction between the laminar flow and the stenotic port in the circular tube. The purpose of the present numerical investigation is to assess the effect of a stenotic shape on the instantaneous shape of the flow passage during freezing upstream/downstream of the stenotic channel. In the solution strategy, the present study is substantially distinguished from the existing works in that the complete set of governing equations in both the solid and liquid regions are resolved. In a channel flow between parallel plates, the agreement between the of predictions and the available experimental data is very good. Numerical analyses are performed for parametric variations of the position and heights of stenotic shape and flow rate. The results show that the stenotic shape has the great effect on the thickness of the solidification layer inside the tube. As the height of a stenosis grows and the length of a stenosis decreases, the ice layer thickness near the stenotic port is thinner, due to backward flow caused by the sudden expansion of a water tunnel. It is found that the flow passage has a slight uniform taper up to the stenotic channel, at which a sudden expansion is observed. It is also shown that the ice layer becomes more fat in accordance with its Reynolds number.

• 한국지반공학회논문집
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• 제34권11호
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• pp.43-55
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• 2018

인공동결공법은 일시적으로 지반의 강성을 높이고 투수계수를 낮추는 지반개량공법으로 지반에 적용가능하다. 하지만, 지하수 흐름과 지반의 불균질성은 동결구근 형성을 불확실하게 하여 공법에 대한 신뢰성을 저해한다. 동결지반 대한 열-수리 유한요소 해석 프로그램을 이용하여, 인공동결공법에서 지하수 흐름속도와 지반의 층상 비균질이 얼음벽 형성을 미치는 영향을 분석하였다. 지하수의 흐름은 원형의 동결구근을 원형에서 타원형을 변형시키며 얼음벽의 완성 소요시간을 증가시킨다. 기존의 이론식은 인접 동결구근의 열적 상호작용을 무시하여, 얼음벽의 완결시간과 한계유속을 과대 평가하였다. 수치해석 결과를 바탕으로 수정식을 제시하였으며 무차원 얼음벽 완결시간에 대한 제안식을 검증하였다. 층상의 비균질 지반에서 투수계수가 큰 지층의 두께와 상대적인 투수계수비는 얼음벽 완결시간과 한계 유속에 중요한 인자인 것으로 나타났다.

• 한국환경과학회지
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• 제26권7호
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• pp.827-836
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• 2017

Freezing rain is a phenomenon when precipitation falls as a liquid rain drop, but freezes when it comes into contact with surfaces or objects. In this study, we investigated the predictability of freezing rain and its characteristics, which are strongly related with the occurrence of black ice using synoptic scale meteorological observation data. Two different cases occurred at 2012 were analyzed and in the presented cases, freezing rain often occurs in the low-level low pressure with the warm front. The warm front due to the lower cyclone make suitable environment in which snow falling from the upper layer can change into supercooled water. The $0^{\circ}C$ temperature line to generate supercooling water is located at an altitude of 850 hPa in the vertical temperature distribution. And the ground temperature remained below zero, as is commonly known as a condition for black ice formation. It is confirmed that the formation rate of freezing rain is higher when the thickness after 1000-850 hPa is 1290-1310 m and the thickness of 850-700 hPa layer is larger than 1540 m in both cases. It can also be used to predict and estimate the generation of freezing rain by detecting and analyzing bright bands in radar observation.

• 물과 미래
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• 제21권4호
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• pp.399-406
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• 1988

만곡수로에서의 흐름, ice jam의 형성 및 분포특성을 규명하기 위하여 기본이론을 분석하고, 실험수로로는 연속 만곡수로와 단일 만곡수로를 사용하였다. 연속 만곡수로는 13개의 중심각 $90^{\circ}$만곡부가 연결된 수로이며 하폭에 대한 수심의 비가 2이며 단일 만곡수로는 중심각 $180^{\circ}$이며 하폭에 대한 수심의 비가 4로 비교적 수심이 얕은 수로이다. 실험에 사용된 얼음재료는 폴리에칠렌과 폴리프로필렌 구슬(bead)와 조각(block)이다. 연속 만곡수로에서는 저면유속이 표면유속보다 크며 ice jam의 형성으로 이러한 현상은 더욱 크게 나타났다. Jam의 두께는 일반적으로 내측이 외측보다 두꺼웠으며 최대 유속선은 ice jam의 발생으로 인하여 더욱 내측으로 편이되었다. 횡방향 jam의 두께는 하폭에 대한 얼음 조각의 길이 비가 증가함에 따라 규칙적으로 분포 되었다. 단일 만곡수로에서의 jam hed는 얼음의 운송량이 일정한 경우 외측이 내측 보다 빨리 진행되었으며 그 속도는 비교적 일정하였다. Froude 수가 증가되므로 jam 두께는 횡단면에 걸쳐 불균일하게 되며, 내측과 jam 끝부분이 두껍게 된다. Two-Layer model은 수심이 얕은 만곡부에서 적용가능하며, 2차 흐름의 분포는 상하 2개의 cell이 존재함을 알 수 있었다.

• 대한기계학회논문집B
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• 제28권12호
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• pp.1484-1493
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• 2004

In this study, it induced to a conclusion below by experiment consideration to regarding an effective supercooling ends method of the flow cooling water in a tube of continuous ice making method and the static cooling water in a tube of continuous ice making method which used magneticfluid in a dynamic type ice storage system. Continuous ice making in a tube of the flow cooling water was shortened about 12 minutes until supercooling ends that case which gave vertical eccentricity rotation magnetic field 120rpm than did not provide magnetic field by experimental result that was tested to supercooling ends effect from shape control of magneticfluid. Continuous ice making method in a tube of the static cooling water compared with and reviewed the case that was not provided with the magnetic field and exposed cooling surface instantaneously by magnetic field. It confirmed that supercooling degree $\Delta$ $T_{c}$, $\Delta$ $T_{s}$, and $\Delta$ $T_{w}$ became lower because of heat transfering increasing by the occurrence of natural convection between after cooling starting progress time 1∼3 minutes if it did not give a magnetic field, and peformed the supercooling ends when natural convection occurred confirmed that refrigerating capacity was better. That relation $\Delta$ $T_{c}$, and $t_{e}$/($\Delta$ $T_{c}$-$\Delta$ $T_{s}$) after convection occurred, was not depended on $T_{b}$ and initial temperature if the depth of water and thickness of magneticfluid were regular and it was possible to verify conjecture of tp from $\Delta$ $T_{s}$ and $\Delta$ $T_{c}$.lar and it was possible to verify conjecture of tp from $\Delta$ $T_{s}$ and $\Delta$ $T_{c}$.c}$.>.

• Journal of Information Processing Systems
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• 제15권6호
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• pp.1350-1364
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• 2019

The ice damage occurs frequently in cold and dry region of western China in winter ice period and spring thaw period. In the drift ice condition, it is easy to form different extrusion force or impact force to damage tunnel lining, causing project failure. The failure project could not arrive the original planning and construction goal, giving rise to the water allocation pressure which influences diversion irrigation and farming production in spring. This study conducts the theoretical study on contact-impact algorithm of drift ices crashing diversion tunnel based on the symmetric penalty function in finite element theory. ANSYS/LS-DYNA is adopted as the platform to establish tunnel model and drift ice model. LS-DYNA SOLVER is used as the solver and LS-PREPOST is used to do post-processing, analyzing the damage degrees of drift ices on tunnel. Constructing physical model in the experiment to verify and reveal the impact damage mechanism of drift ices on diversion tunnel. The software simulation results and the experiment results show that tunnel lining surface will form varying degree deformation and failure when drift ices crash tunnel lining on different velocity, different plan size and different thickness of drift ice. The researches also show that there are damages of drift ice impact force on tunnel lining in the thawing period in cold and dry region. By long time water scouring, the tunnel lining surfaces are broken and falling off which breaks the strength and stability of the structure.