• Journal of Astronomy and Space Sciences
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• 제34권4호
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• pp.251-256
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• 2017

The electric coupling between the lithosphere and the ionosphere is examined. The electric field is considered as a timevarying irregular vertical Coulomb field presumably produced on the Earth's surface before an earthquake within its epicentral zone by some micro-processes in the lithosphere. It is shown that the Fourier component of this electric field with a frequency of 500 Hz and a horizontal scale-size of 100 km produces in the nighttime ionosphere of high and middle latitudes a transverse electric field with a magnitude of ~20 mV/m if the peak value of the amplitude of this Fourier component is just 30 V/m. The time-varying vertical Coulomb field with a frequency of 500 Hz penetrates from the ground into the ionosphere by a factor of ${\sim}7{\times}10^5$ more efficient than a time independent vertical electrostatic field of the same scale size. The transverse electric field with amplitude of 20 mV/m will cause perturbations in the nighttime F region electron density through heating the F region plasma resulting in a reduction of the downward plasma flux from the protonosphere and an excitation of acoustic gravity waves.

• 한국해양공학회지
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• 제22권2호
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• pp.7-12
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• 2008

A far field solution of the slowly varying force on an offshore structure by gravity ocean waves was shown as a function of the reflection and transmission of the body disturbed waves. The solution was obtained from the conservation of the momentum flux, which simply describes various wave forces, while making it unnecessary to compute complicated integration over a control surface. The solution was based on the assumption that the frequency difference of the bichromatic incident waves is small and its second order term is negligible. The final solution is expressed in term of the reflection and transmission waves, i.e. their amplitudes and phase angles. Consequently, it shows that not only the amplitudes but also the phase differences make critical contributions to the slowly varying force. In a limiting case, the slowly varying force solution gives the one of the mean drift force, which is only dependent on the reflection wave amplitude. An approximation is also suggested in a case where only the mean drift force information is available.

• 자원환경지질
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• 제54권6호
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• pp.743-752
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• 2021

추가령 단층대가 발달하는 서울-경기 지역에서 단층의 3차원적인 규모를 확인하기 위해서, 곡률 분석(Curvature analysis)과 오일러 디콘볼루션(Euler deconvolution) 등의 중력장 해석 방법을 이용하여 잔여 중력이상을 해석하였다. 또한 2000년 이후 발생한 진앙과 비교하여 단열 특성을 비교하였다. 부게이상에서 포천단층은 경기 북부에서 서울의 중심부를 지나서 서해안 지역까지 연결된 약 100 km 단층으로 진앙이 빈도가 높아 활성 단층의 가능성이 있고, 단층을 경계로 동서 방향으로 7 km 정도의 변위가 관찰된다. 왕숙천단층은 서울을 중심으로 북동부와 서남부로 분절되어 있으나 지하에서 연결을 암시하는 단층 분절로 추정되는 중력이상대가 관찰된다. 특히 2010년 시흥에서 발생한 규모 3.0의 지진은 남북 방향으로 발달하는 20 km 길이의 단층에 의한 것으로 판단된다. 동두천단층의 서쪽 지역(≒5,500 m)은 중력경계면이 동쪽 지역(≒4,000 m)보다 깊게 나타나며 이는 동두천단층을 중심으로 서쪽 지역과 동쪽 지역의 지구조적인 운동이 다르다는 것을 시사한다. 동두천단층에서 발달한 파쇄대의 최대 깊이는 약 6,500 m이며 연구 지역에서는 가장 깊다. 포천 단층은 약 6,000 m, 왕숙천 단층은 약 5,000 m, 경강 단층은 약 6,000 m 깊이까지 파쇄대가 연장되는 것으로 판단된다.

• 제어로봇시스템학회:학술대회논문집
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• 제어로봇시스템학회 2005년도 ICCAS
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• pp.1641-1644
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• 2005

Magnetic actuation utilizes the mechanic torque that is the result of interaction of the current in a coil with an external magnetic field. A main obstacle is, however, that torques can only be produced perpendicular to the magnetic field. In addition, there is uncertainty in the Earth magnetic field models due to the complicated dynamic nature of the field. Also, the magnetic hardware and the spacecraft can interact, causing both to behave in undesirable ways. This actuation principle has been a topic of research since earliest satellites were launched. Earlier magnetic control has been applied for nutation damping for gravity gradient stabilized satellites, and for velocity decrease for satellites without appendages. The three axes of a micro-satellite can be stabilized by using an electromagnetic actuator which is rigidly mounted on the structure of the satellite. The actuator consists of three mutually-orthogonal air-cored coils on the skin of the satellite. The coils are excited so that the orbital frame magnetic field and body frame magnetic field coincides i.e. to make the Euler angles to zero. This can be done using a Neural Network controller trained by PD controller data and driven by the difference between the orbital and body frame magnetic fields.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
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• 제25권1호
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• pp.15-22
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• 1997

The GPS/levelling geoid calculated from GPS survey that data at 123 bench marks represents an appropriate regional geoid of the southern Korean peninsula. The GPS/levelling geoid fits best to the geoid calculated from the EGM96 geopotential model of degree and order to 360 with RMS difference 0.176 m. The good agreement of the GPS/levelling geoid with the EGM96 geoid suggests that the bench mark network is well established in Korea and the EGM96 geopotential model well represents the gravity field in the southern Korean peninsula.

• 한국재료학회지
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• 제12권4호
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• pp.264-268
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• 2002

Magnetic fluid is a very stable colloid that is attracted by magnetic force as wholly. The magnetic fluids is composed with 10 nm magnetic materials such as magnetite, iron etc., which is dispersed homogeneously in solvent by coating surfactant on their surface. Also this colloid is not separated into magnetic particles and solvent even under magnetic field, centrifugal force, gravity. Due to these properties, the magnetic fluids is used in high vacuum seal, exclusion seal, damper, etc. I would like to introduce the specific properties and applications of the magnetic fluids.

• 대한기계학회논문집A
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• 제20권3호
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• pp.933-944
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• 1996

In this paper, two new techniques, the pattern filling and the refined flow field regeneration, based on the finite element method and Eulerian mesh advancement approach have been developed to analyze incompressible viscous flow with free surfaces. The gorerning equation for flow analysis is Navier-Stokes equation including inertia and gravity effects. The penalty and Newton-Raphson methods are used effectively for finite element formulation. The flow front surface and the volume inflow rate are calculated using the pattern filling technique to select an adequate pattern among five filling patterns at each quadrilateral control volume. By the refined flow field regeneration technique, the new flow field which renders better prediction in flow surface shape is generated and the velocity field at the flow front part is calculated more exactly. Using the new thchniques to be developed, the dam-breaking problem has been analyzed to predict flow phenomenon of fluid and the predicted front positions versus time have been compared with the reported experimental result.

• 대한기계학회:학술대회논문집
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• 대한기계학회 2001년도 춘계학술대회논문집E
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• pp.727-732
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• 2001

The purpose of this study is to compare the time mean velocity distribution, the time mean kinetic energy, and the time mean turbulence intensity between vertical and horizontal flow fields in a coaxial circular pipe by PIV measurement. Experiments are performed at a Reynolds number 2,000, measuring regions divided as the section regions A, B, C, D in flow fields. The angle of the high-frequency ultrasonic is selected in the direction of $45^{\circ}$ to the flow axes and it is reflected several times. In results, it is clarified that the effect of gravity is given in the vertical flow field compared with the horizontal flow field and the ultrasonic affects the turbulence enhancement. And kinetic energy and turbulence intensity with ultrasonic are shown slightly bigger than those in flow field without it.

• 한국초전도ㆍ저온공학회논문지
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• 제24권3호
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• pp.19-23
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• 2022

We have been developing a magnetic separation device that can be used in low magnetic fields for paramagnetic materials. Magnetic separation of paramagnetic particles with a small particle size is desired for volume reduction of contaminated soil in Fukushima or separation of iron scale from water supply system in power plants. However, the implementation of the system has been difficult due to the needed magnetic fields is high for paramagnetic materials. This is because there was a problem in installing such a magnet in the site. Therefore, we have developed a magnetic separation system that combines a selection tube and magnetic separation that can separate small sized paramagnetic particles in a low magnetic field. The selection tube is a technique for classifying the suspended particles by utilizing the phenomenon that the suspended particles come to rest when the gravity acting on the particles and the drag force are balanced when the suspension is flowed upward. In the balanced condition, they can be captured with even small magnetic forces. In this study, we calculated the particle size of paramagnetic particles trapped in a selection tube in a high gradient magnetic field. As a result, the combination of the selection tube and HGMS (High Gradient Magnetic Separation-system) can separate small sized paramagnetic particles under low magnetic field with high efficiency, and this paper shows its potential application.

• 지구물리
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• 제1권1호
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• pp.31-40
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• 1998

양산단층이 통과하는 안강 부근에서 기반암 분포, 지표 근처 단층과 파쇄대 위치 및 규모 등을 밝히기 위하여 중력과 총지자기를 측정하였다. 예상되는 단층의 주향과 거의 직각이 되는 2개 측선을 따라 총 67개 지점에서 15 m 간격으로 중력을 정밀하게 측정하였으며, 총지자기는 동일 측선을 따라 3 m 간격으로 총 296 점에서 측정하였다. 스펙트럼 분석법으로 구한 자기 기반암의 평균 깊이는 형산강을 중심으로 서부와 동부 측선에서 각각 8.5, 10.0 m로 계산되며, 중력 측정값은 형산강 동부가 서부보다 평균 1.71 mGal 이상 크게 나타나서 서부가 동부보다 파쇄 정도가 더욱 심한 것으로 해석된다. 중력 순산모델 연구는 동부 측선의 동쪽 끝에서 210 m 떨어진 지점에 놓인 단층을 경계로 서쪽으로 밀도 2.44 g/cm3, 깊이 70 m의 파쇄대가 발달되어 있으며, 395 m 지점을 중심으로 기반암 상부면이 폭 190 m, 평균 3.5 m 깊이의 소규모 비대칭 지구가 존재할 가능성을 제시한다. 또한 이 지구 위치의 지표 고도는 주위보다 약 44 cm 꺼져 있어서, 이 지구가 그리 오래되지 않은 시기의 단층운동에 의해 형성되었을 가능성이 높은 것으로 해석된다.