• Journal of the Korea Computer Graphics Society
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• v.26 no.5
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• pp.1-13
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• 2020

In this paper, we propose a new method to stable simulation the directional ice shape by coupling of freezing solver and viscous water flow. The proposed ice modeling framework considers viscous fluid flow in the direction of ice growth, which is important in freezing simulation. The water simulation solution uses the method of applying a new viscous technique to the IISPH(Implicit incompressible SPH) simulation, and the ice direction and the glaze effect use the proposed anisotropic freezing solution. The condition in which water particles change state to ice particles is calculated as a function of humidity and new energy with water flow. Humidity approximates a virtual water film on the surface of the object, and fluid flow is incorporated into our anisotropic freezing solution to guide the growth direction of ice. As a result, the results of the glaze and directional freezing simulations are shown stably according to the flow direction of viscous water.

• Journal of the Korean Geotechnical Society
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• v.39 no.6
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• pp.13-19
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• 2023

Lunar ice is a resource available for future human exploration in deep space and long-term extraterrestrial habitat. However, the origin and nature of lunar ice remains unclear. In addition to remote sensing, international space agencies are competitively planning and conducting missions for lunar surface exploration to determine the existence and resource extent of lunar ice. If a sufficient amount of lunar ice is confirmed, its future in-situ resource utilization is expected to be greatly beneficial. However, due to ice extraction, settlement may occur, which should be taken into account from a geotechnical engineering perspective. Herein, experimental investigations of the potential settlement caused by lunar ice extraction were conducted and different textures of lunar ice were simulated. Consequently, it was confirmed that significant settlement occurs even at the initial water content of ~10% in lunar regolith simulant-ice-mixed soil.

• Transactions of the Korean Society of Mechanical Engineers
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• v.7 no.4
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• pp.483-488
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• 1983

비교적 저온의 순수물 속에 있는 수직얼음 원기둥 주위에서 일어나는 자연대류 현상을 수치계산 방법을 사용하여 이론적인 해를 추구하였으며 기존 실험결과와 비교하였다. 유동의 형태는 주위 유체의 온도에 따라서 상향유동, 하향유동, 이 양자가 동시에 존재하는 유동의 형태로 구분되었으 며 해를 구할 수 있는 영역내에서는 상향유동과 하향유동이 동시에 존재하는 구역에서 열전달율 이 최소가 됨을 알 수가 있었다.

• The Bulletin of The Korean Astronomical Society
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• v.38 no.1
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• pp.54.1-54.1
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• 2013

이 연구는 질량이 낮은 별탄생 지역에서 '에피소딕 질량수축 이론'을 관측과 수치모델로 테스트하였다. 스피쳐 우주망원경을 비롯한 여러 망원경으로 별 탄생 지역을 관측한 결과, 어린 별의 광도는 0.01 태양광도에 불과한 매우 낮은 값에서부터 높은 값까지 넓은 영역에 걸쳐 분포한다는 것이 알려졌다. 이 관측 결과는 70년대부터 있어 온 소위 표준 별탄생 모델의 예측과는 다른 결과이다. 관측과 표준 별탄생 모델의 차이를 풀기 위해서 에피소딕 질량수축 모델이 제안되었다. 테스트를 통하여 광도가 낮은 어린 별의 관측적 특성이 에피소딕 질량수축 모델로 한꺼번에 설명될 수 있음을 보였다. 우선, 카르마 전파 간섭계를 사용하여 전체 어린 별의 광도 분포에 해당하는 별 샘플을 선택하여 관측하였다. 표준 별탄생 모형은 중력수축이 진행됨에 따라 디스크 질량이 점진적으로 증가하지만 에피소딕 중력수축 모델은 디스크 질량과 별의 진화상태 사이에 특별한 연관관계가 없음을 예측한다. 여섯 개의 측정된 디스크 질량은 별의 진화상태와 상관없음을 보여주었다. 다음으로, 열아홉 개 어린 별의 이산화탄소 얼음을 적외선으로 분광 관측하고 분석하였다. 관측대상별 중 절반은 다른 분자와 섞이지 않은 순수한 이산화탄소 얼음이 존재한다는 증거를 보였고, 그 중 여섯 개는 순수 이산화탄소 얼음 존재의 강력한 증거인 두개의 픽이 나온 흡수선 형태를 보였다. 순수 이산화탄소 얼음 성분이 현재 광도가 낮은 별에서 존재한다는 것은 과거에 광도가 밝았던 시기, 즉 중력수축속도가 높았던 시기가 있었다는 것을 뒷받침한다. 화학진화모델에 에피소딕 중력수축 모델과, 일산화탄소 얼음이 이산화탄소 얼음으로 전환될 수 있다는 새로운 화학 네트워크를 포함한 모델로 광도가 낮은 어린 별에서의 순수 이산화탄소의 존재, 총 이산화탄소의 양, 그리고 관측된 일산화탄소 가스의 양을 모두 설명할 수 있었다.

• Journal of the Korea Convergence Society
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• v.11 no.10
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• pp.25-30
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• 2020

In this study, a test system which can test performance of curling pad was developed to support Korea curling team. The developed system consists of a water tank, a mechanical pad driving system that can perform sweeping movement using a curling pad on surface of ice made by the water tank, and temperature sensors monitoring ice and air temperatures. To control the temperature of ice and humidity/temperature of air around the ice, all system are installed in a chamber that can isolate the developed system from external environment. Eight kinds of curling pads were tested using the developed system. Test result showed that each curling pad revealed different rate of ice temperature increasing. The pad with the highest rate of ice temperature rising was found to be the same as the most preferred pad by the athletes. Therefore, it was confirmed that the method of measuring change of ice temperature by the sweeping performed in this study is an effective method to test the performance of the pad.

• Journal of Food Hygiene and Safety
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• v.30 no.4
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• pp.309-314
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• 2015

The purpose of this study is to monitor the microbial contamination of ice collected from food stores or restaurants from all over the country. From the ice collected on a regional basis, it was observed that the average number of total aerobic bacteria (TAB) of samples from Seoul was the highest, showing 2.31 log CFU/g, while that of samples from Jeolla-do was the lowest, showing 1.83 log CFU/g. The food-borne pathogens (Staphylococcus aureus, Listeria monocytogenes) were not detected from the ice. Also the average number of TAB of packaged ice (commercial ice) was 0.45 log CFU/g lower than that of ice from ice-making machine. Among three types of stores (the bakery, the dessert store and the beverage store), ice from dessert store showed the highest number of TAB (2.37 log CFU/g). This study suggests that the hygienic management of the ice from the stores is necessary. Therefore, to ensure the hygienic management of ice, not only the ice-making machine should be sanitized on a regular basis but also a thorough individual hygiene is required from food manufacturing workers.

• Journal of the Korea Society of Computer and Information
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• v.29 no.3
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• pp.91-98
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• 2024

In this paper, we present a particle-grid blending framework based on a geometric approach to efficiently represent opaque ice spheres with air bubbles. The water temperature is diffused through the grid and the air bubbles represented inside the ice through the particles. To solve the problem of previous methods that generate noisy dissolved air fields, we use levelsets to lighten the algorithm, i.e., the number of active particles and the initial amount of dissolved oxygen can be used to efficiently control the termination conditions of heat diffusion. We also extend the previous dissolved air field method, which only computes near air bubbles, to transparent regions to represent realistic ice spheres, and introduce a levelset-based approach to accurately compute the orientation of particles. As a result, the method presented in this paper is about three times faster than the existing methods and shows visually improved visualization of opaque ice spheres, which can be used in the field of representing physical virtual ice forms.

• Journal of the Korean association of regional geographers
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• v.3 no.1
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• pp.165-182
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• 1997

The aim of this paper is to clarify geomorphic features on talus within ${\check{O}}rumkol$ and the origin of ${\check{O}}rumkol$. ${\check{O}}rumkol$ is located in Milyang of Kyungnam province, in South Korea. ${\check{O}}rumkol$ is good area to study talus. because it is characterized by following three geomorphic landscapes : free face surrounding ${\check{O}}rumkol$ ; ${\check{O}}rumkol$ with deep and wide valley floor ; lots of taluses typically developing within ${\check{O}}rumkol$. The main results can be summarized as follows: 1) The origin of ${\check{O}}rumkol$ may be suggested two assumptions : one is that its origin have been resulted from intrusion structure(intrusive rock might capture less resistant rock as tuff) ; the other is that its origin have been resulted from volcanic depression after intrusion or eruption. But these assumptions are not obvious. therefore more geological evidences will be supplemented after this 2) The characteristics of ${\check{O}}rumkol$ talus (1) Pattern ${\check{O}}rumkol$ taluses are tongue-shaped or cone-shaped in appearance. They are $50{\sim}200m$ in length and the range of the maximum width from 25 to 115m and one of their mean slope gradient from 32 to $36^{\circ}$ (2) Origin ${\check{O}}rumkol$ taluses have been formed under periglacial environment in the last glacial age and they are classified into rock fall talus type, considering in conjunction with the shape, hardness, sorting, weathering conditions of constituent debris. (3) The stage of landform development ${\check{O}}rumkol$ talus slope profiles are mainly concave slope. This concave slope type was eventually caused by talus creep at the lower end of the talus. That means new additions of debris from the free face have virtually ceased and there is no evidence of recent motion in the deposit. Now it is predominant that vegetation cover is gradually increasingly. Therefore ${\check{O}}rumkol$ taluses appear to be relict form stage. at present.

• The Science & Technology
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• v.35 no.8 s.399
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• pp.28-29
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• 2002

석빙고는 자연 환기구의 적절한 배치, 유선형의 외부형태, 배수구의 이용, 흙과 돌의 열전도율의 차이를 이용한 축열구조의 채택 등 기계장치와 비교하여 결코 떨어지지 않는 과학적 기술이 접목된 것이다.

• Journal of the Korean Society for Aeronautical & Space Sciences
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• v.46 no.8
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• pp.611-620
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• 2018

For the past decades, the analytic model for distributed surface roughness has been developed to improve the accuracy of the icing simulation code. However, it remains limitations to validate the developed model and determine the empirical parameters due to the absence of the quantitative experimental data which were focused on the surface state. To this end, the experimental study conducted to analyze the ice covered surface state from a micro-perspective. Above all, the tendency of the smooth zone width which occurs near the stagnation point has been quantitatively analyzed. It is observed that the smooth zone width is increased as growing the ambient temperature and freestream velocity. Next, the characteristics of the ice covered surface under rime and glaze ice have been analyzed. For rime ice conditions, ice elements are developed as the opaque circular corn in the opposite direction of freestream. The height and interval of each circular corn are increased as rising the ambient temperature. For glaze ice conditions, numerous lumps of translucent ice can be observed. This is because the beads formed by gravity concentrate and froze on the lower surface.