• Journal of the Speleological Society of Korea
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• no.70
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• pp.1-8
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• 2006

처마 끝에 열리는 고드름은 흔히 겨울철에 내린 눈이 지붕위에 쌓여 있다가 따사로운 햇살이 비치면 녹은 눈이 중력에 의해 흘러내리면서 영하의 찬 기류에 얼면서 성장하여 길게 매달린다. 그러나 땅바닥이나 물그릇 속에서 위로 자라 올라오는 역고드름은 특별히 그곳에서만 지상의 역 중력이 작용할 이유가 없기 때문에 간단히 해석되기가 쉽지 않다. 겨울밤에 정안수를 놋그릇에 떠놓고 공불기도를 올리다가 물이 어면서 나타나는 기이한 역 고드름은 물이 얼면서 생긴 표면의 숨구멍을 통하여 물보다 저밀도인 얼음의 체적이 불어서 밀려나오면서 생길 수 있으나, 이 현상만으로는 역고드름이 그렇게 크게 자랄 수가 얼다. 따라서 이 경우는 주변에서 불어오는 찬 기류가 지형지물에 부딪히면서 회오리쳐 소슬바람을 일으킬 때 일시적인 부압이 작용하여 그릇속의 물이 숨구멍을 통해 나오면서 얼어 성장되는 현상이 부가적으로 상승작용을 일으켜 길게 자라 올라온 것이다.

• Journal of the Korean Society of Propulsion Engineers
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• v.20 no.1
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• pp.76-81
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• 2016

At negative-g condition, a float-type valve can open the passage of fuel in order to it flows continuously through a pressurized fuel tank system. Since specialized test conditions and high-cost supports are required, it is truly difficult to test the valve in a real high-speed test. Therefore, this paper contains performance analysis of a float-type fuel supply valve through flight tests conducting roll and negative-g maneuvers.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.13 no.2
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• pp.177-185
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• 1995

Gravity anomalies were recovered on a $5'\times{5'}$grid using the sea surface height data obtained from the combination of Geosat, ERS-1, Topex/Poseidon altimeter data around Korean Peninsula bounded by latitude between $30^\circ{N}\;and\;50^\circ{N}$ and longitude $120^\circ{E}\;to\;140^\circ{E.}$ In order to recover the gravity anomalies from SSH(Sea Surface Height), inverse FFT technique was applied. The estimated gravity anomalies were compared with gravity anomalies measured by shipboard around Korean Peninsula. In comparison with the differences of gravity anomaly between measured data and altimeter data, the mean and the standard deviation were found to be -0.51 mGal and 13.48 mGal, respectively. In case of comparison between the measured data and the OSU91A geopotential model, the mean and the standard deviation were found to be 11.93 mGal and 19.19 mGal, respectively. The comparison of gravity anomalies obtained from the OSU91A geopotential model and the altimeter data was carried out. The results were mean of 5.30 meal and standard deviation of 19.62 mGal. From the results, we could be concluded that the gravity anomalies computed from the altimeter data is used to the geoid computation instead of the measured data.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 1991.07a
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• pp.98-98
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• 1991

항만 및 연안역 이용이 다변화되고 방파제를 설치할 지점의 수심이 깊어짐에 따라 기존의 착저 중력식 방파제는 한계점을 노출하고 있으며, 각 이용목적에 보다 부합되는 형태의 신소파제 개발이 요구되고 있다. 기존의 착저 중력식 방파제는 외해로부터의 파랑을 차단하는 데에는 탁월한 성능을 가지나 항내의 해수순환을 차단하여 수질악화 등의 환경문제를 유발시키는 문제점이 있으며, 대수심에 설치해야 할 경우에는 공사비가 많이 들며 시공이 어려워진다.(중략)

• Economic and Environmental Geology
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• v.40 no.4
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• pp.445-459
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• 2007

Superconducting Gravimeter(SG) was installed and has been successfully operated at MunGyung, Kyungsang province in Korea in March 2005. It was registered as the 21st observatory of the Global Geodynamics Project. Since SG can precisely measure the gravity variations below the 1mHz frequency band, it has the outstanding capability to sense and resolve many different periodic gravity components from each other. From the raw data collected between 18 March 2005 and 21 February 2006 diurnal and semi-diurnal tidal band's residual gravity components were analyzed. During this process, the instrumental noises, air pressure, and ground water corrections were carried out. Values of $-3.18nm/s^2/hPa\;and\;17nm/s^2/m$ were used respectively in the air pressure and groundwater corrections. Hartmann-Wenzel and Whar-Dehant Earth tide models were adopted to compute the residual gravity for Q1, O1, P1, K1, M2, N2, S2, K2 tidal bands. For the ocean loading correction, SCW80, FES952, and FES02 models were used and compared. As a result, FES02 ocean loading model has shown the best match for the data processing at MunGyung SG MunGyung SG gravity was compared with GRACE satellite gravity. The correlation coefficient between the two gravity after groundwater correction was 0.628, which is higher than before ground water correction. To evaluate sensitivity at MunGyung SG gravity statition, the gravity data measured during 2005 Indodesian earthquake was compared with STS-2 broad band seismometer data. The result clearly revealed that the SG could recorded the same period of earthquake with seismometer event and a few after-shock events those were detected by seismometer.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 2002.08a
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• pp.162-176
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• 2002

태음-태양-지구 체계의 상호인력에 의해 발생하는 해양조석은 해수면의 주기적인 승강운동으로서 고체 지구상에서는 지구의 응력 및 중력장의 교란을 야기하는 변동하중을 의미한다. 해양조석에 대한 연구는 심해 및 천해역에서 정확한 조석예보를 위해서 뿐만 아니라 신뢰성 있는 해면변위(sea surface topography)를 추정하기 위해 중요하다. (중략)

• The Journal of Engineering Geology
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• v.8 no.3
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• pp.285-296
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• 1998

As a part of the study for understanding the deep geological structure of the Ogcheon Zone, both gravity and geomagnetic surveys are performed. A 70km survey line of which direction is nearly perpendicular to major faults in the southern tip of the Zone. The observed data are corrected and transformed into Bouguer and total magnetic intensity anomalies, respectively. Recent studies for petrology and geochemistry in the southwestern Ogcheon Zone in the vicinity of the survey line are reviewed for better interpretation. Both gravity and geomagnetic anomalies abruptly change around Janghung area, the southern boundary of the, Ogcheon Zone. This rapid increase of Bouguer anomaly around Janghung area can be explained by a deep seated normal fault with fairy large displacement between Precambrian gneisses and the denser intermediate plutonic rocks. It is believed that the fault acted an important role for the formation and evolution of the Ogcheon Zone. A pseudomagnetic intensity anomaly is calculated from the Bouguer anomaly assuming that the both anomalies are associated with the common source. From the origin of the survey line to the 50km point, the calculated anomaly coincides with observed magnetic anomaly. Whereas both anomalies show negative correlation in the outside 50km. From the residual Bouguer anomalies, the subterranean geological structure is provided through the iterative forward method. The initial model is obtained from informations about the surface geology as well as the results of the inverse method.

• Proceedings of the Korean Institute of Intelligent Systems Conference
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• 2007.04a
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• pp.349-352
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• 2007

본 논문은 계층적 공정 경쟁 유전자 알고리즘(Hierarchical Fair Competition-based Genetic Algorithms : HFCGAs)을 이용한 회전형 역 진자 시스템의 최적 2-자유도 제어기 설계를 제안한다. 비선형이며 불안정한 운동을 하는 회전형 역 진자 시스템은 회전지렛대(rotating arm) 위의 폴(pole)이 적당한 제어력이 없는 상황에서 중력에 의해 어느 한 쪽 방향으로 넘어지려고 할 때, 외부에서 회전지렛대에 힘을 가하여 회전지렛대의 특정위치와 폴의 각도를 유지시키는 시스템으로, 본 논문에서는 두 개의 피드백 제어루프를 갖는 2-자유도 제어기를 구성한다. 각각의 제어기는 PD 제어기로 구성하고, 조기수렴 문제를 내재하고 있는 기존의 유전자 알고리즘의 해결방안중 하나인 HFCGAs를 이용하여 최적의 제어기 파라미터들을 구한다. 마지막으로 실제 공정에 적용하여 설계된 제어기의 성능을 평가한다.

• Economic and Environmental Geology
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• v.2 no.2
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• pp.1-35
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• 1969

The structure and geologic history of the Triassic basin in southern Connecticut have been interpreted by using gravimetric data. A gravity survey of 800 gravity stations was made by the U.S. Geological Survey in the southern Connecticut area. The resulting data were reduced by the Bouguer method and then plotted and contoured along with the generalized geology. Residual gravity maps were prepared by different methods to obtain the most plausible agreement with the known geology of the area. Seven gravity profiles across the basin are presented to show the distribution of the Triassic deposits that could produce the measured anomalies. It is concluded that the basin was formed by successive step faulting in the late Triassic period and that the sediments accumulated progressively in this basin. The deepest portion of the basin is located in the middle of the present Triassic belt and reaches a depth of about 2 miles below the surface. The data also appear to indicate the possible source areas for the basalt which at present forms the lava flows, sills, and dikes exposed in the Cheshire and Gaillard regions. The information concerning the tectonic history of the Connecticut Triassic Valley aids considerably in establishing the geologic history of the Appalachians in late Triassic time.

• 건축구조
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• v.12 no.4
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• pp.52-53
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• 2005

a. 구조체가 받는 힘 중 횡력을 모두 메가컬럼이 부담하고, 내부외 보와 기둥은 중력방향의 하중만을 부담한다. b. 메가컬럼 안으로 코어 기능을 모두 넣어 자유로운 평면구성이 가능하다는 것이 최대의 장점이다. c. 모듈의 반복적인 조합을 통해 나온 유닛의 재조합으로 메가컬럼을 형성하고, 거대한 이 기둥을 외부로 노출시켜 구조미를 추구한다. d. 2009년 9호선 연장을 앞두고 서울의 최고 중심지가 될 강남역을 사이트로 정해 초고층 건물을 건축하여 도시경관을 더 돋보이게 한다.