• Bulletin of the Korean Space Science Society
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• 1993.10a
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• pp.24-24
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• 1993

1991년 한국에서 열렸던 밀리미터파 및 적외선천문학에 관한 동북아시아지역 Workshop에서의 합의에 근거하여, 장래의 동북아시아천문대와 동북아시아 지역에 있어서의 당면적인 국제협력관계를 만들어가기 위하여, 중국오지에서의 지상관측을 위한 1차 부지탐사를 1993년 9월에 대만, 일본, 중국, 한국의 4개국 합동으로 추진하였다. 천문학은 본래 지극히 국제적인 과학이며, 따라서 국제협력없이는 앞으로 나아가지 않는다. 그러나, 과거의 여러 사정에 의해 현재 정상적인 협력관계에 놓여있지 않는 대만, 일본, 중국, 한국이 동북아시아 제국 공통의 최신의 관측소를 가지고서는 상호간에 밀접하게 천문학연구를 진행해 나가기 위한 하나의 꿈이 곧 동북아시아천문대라고 할 수 있다. 동북아시아천문대는 이 지역에서의 천문학의 공통적인 활동장소를 만들어나가는 것을 지향하고 있다. 즉, 여러 나라의 연구자들끼리 자연적으로 밀접한 교류를 행해 나가는 가운데, 천문학을 발전시켜나가는 센터를 만들고자 하는 것이다. 그러므로 여기서 계획하고 있는 부지탐사는 이러한 꿈을 실현해 나가기 위한 첫걸음이라고 할 수 있다. 현재 가시광, 적외선, 밀리미터파, 서브밀리미터파를 막론하고, 지상관측에 있어서 요구되는 조건은 모두 같다고 하겠다. 날씨가 좋고, 건조하여 수증기양이 적으며, 공기의 흔들림이 적고, 인간의 활동에 지장이 없을 정도의 높이와 교통편이 좋을 것 등을 들 수 있다. 그러므로 이번 1차부지탐사에서는 연간일조시간이 3000시간 이상에 달하는 후보지에 대한 대기의 종합적인 측정을 행하며, 아울러 가능하다면 적절한 장소에 소형의 적외선 및 서브밀리미터파의 망원경을 두는 공동계획을 구체화한다.ofile occurs along north-south direction there are a few peaks in most line profiles, and these indicate that there not multiple velocity components along the line of sight. Distributions of excitation temperah at and column density which were estimated from the excitation calculations show the existence of a small(IxEpc),hot(Tex> SOK) core which contains two tempegatlue peaks at -15" east and north of MDS. The column density of HCaN is (1-3):n1014cm-2. Column density at distant position from MD5 is larger than that in the (:entral region. We have deduced that this hot-core has a mass of 10sR1 which i:s about an order of magnitude larger those obtained by previous studies.previous studies.업순서들의 상관관계를 고려하여 보다 개선된 해를 구하기 위한 연구가 요구된다. 또한, 준비작업비용을 발생시키는 작업장의 작업순서결정에 대해서도 연구를 행하여, 보완작업비용과 준비비용을 고려한 GMMAL 작업순서문제를 해결하기 위한 연구가 수행되어야

• Geophysics and Geophysical Exploration
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• v.9 no.1
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• pp.30-36
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• 2006

Japan's first pilot-scale $CO_2$ sequestration experiment has been conducted in Nagaoka, where 10400 t of $CO_2$ have been injected in an onshore aquifer at a depth of about 1100 m. Among various measurements conducted at the site for monitoring the injected $CO_2$, we conducted time-lapse crosswell seismic tomography between two observation wells to determine the distribution of $CO_2$ in the aquifer by the change of P-wave velocities. This paper reports the results of the crosswell seismic tomography conducted at the site. The crosswell seismic tomography measurements were carried out three times; once before the injection as a baseline survey, and twice during the injection as monitoring surveys. The velocity tomograms resulting from the monitoring surveys were compared to the baseline survey tomogram, and velocity difference tomograms were generated. The velocity difference tomograms showed that velocity had decreased in a part of the aquifer around the injection well, where the injected $CO_2$ was supposed to be distributed. We also found that the area in which velocity had decreased was expanding in the formation up-dip direction, as increasing amounts of $CO_2$ were injected. The maximum velocity reductions observed were 3.0% after 3200 t of $CO_2$ had been injected, and 3.5% after injection of 6200 t of $CO_2$. Although seismic tomography could map the area of velocity decrease due to $CO_2$ injection, we observed some contradictions with the results of time-lapse sonic logging, and with the geological condition of the cap rock. To investigate these contradictions, we conducted numerical experiments simulating the test site. As a result, we found that part of the velocity distribution displayed in the tomograms was affected by artefacts or ghosts caused by the source-receiver geometry for the crosswell tomography in this particular site. The maximum velocity decrease obtained by tomography (3.5%) was much smaller than that observed by sonic logging (more than 20%). The numerical experiment results showed that only 5.5% velocity reduction might be observed, although the model was given a 20% velocity reduction zone. Judging from this result, the actual velocity reduction can be more than 3.5%, the value we obtained from the field data reconstruction. Further studies are needed to obtain more accurate velocity values that are comparable to those obtained by sonic logging.

• Geophysics and Geophysical Exploration
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• v.15 no.2
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• pp.85-91
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• 2012

Multiple Lapse Time Window (MLTW) analysis for obtaining intrinsic attenuation value require numerous data without directional bias to compensate focal mechanism. The first window of MLTW, therefore, shows large deviation in fitting smoothed theoretical curve. The information on the focal mechanism may reduce burdens of number and distribution. This study combined algorithm of computing focal mechanism to DSMC method by Yoshimoto (2000). However, the MLTW method based on the numerous data was not applicable to this study, because of the limited data to the almost same fault plane solution. This study showed that the available data was too insufficient to construct smoothed theoretical curve, although the deviation of the first window was improved. Instead of conventional solution by more data, the study seems to be needed for new constraints to obtain smoothed curve.

• Geophysics and Geophysical Exploration
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• v.12 no.1
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• pp.99-104
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• 2009

We propose a waveform inversion method for SH-wave data obtained in a shallow seismic refraction survey, to determine a 2D inhomogeneous S-wave profile of shallow soils. In this method, a 2.5D equation is used to simulate SH-wave propagation in 2D media. The equation is solved with the staggered grid finite-difference approximation to the 4th-order in space and 2nd-order in time, to compute a synthetic wave. The misfit, defined using differences between calculated and observed waveforms, is minimised with a hybrid heuristic search method. We parameterise a 2D subsurface structural model with blocks with different depth boundaries, and S-wave velocities in each block. Numerical experiments were conducted using synthetic SH-wave data with white noise for a model having a blind layer and irregular interfaces. We could reconstruct a structure including a blind layer with reasonable computation time from surface seismic refraction data.

• Proceedings of the Korean Information Science Society Conference
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• 2004.10a
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• pp.91-93
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• 2004

차세대 정보통신 기술의 가장 중요한 패러다임으로 '유비쿼터스 컴퓨팅' 이 새롭게 주목받고 있다 유비쿼터스 환경에서의 서비스 지원 시스템을 개발하기 위한 중요한 문제 중의 하나는 이동 객체(사용자)의 시간과 이벤트의 관계를 파악하고 위치 이동 데이터로부터 시공간 이동 패턴을 탐사하는 것이다. 본 논문에서는 유비쿼터스 환경 내에서 사용자에게 시간과 관련된 서비스를 적절히 제공하기 위해서 다음과 같은 연구를 한다. 첫째, 서비스 관점에서의 시간적 추론(Temporal Reasoning)이다. 각 사용자들은 각자의 취향을 가지고 있으며 이는 시간과 밀접한 관계를 가지고 있다. 시간과 관련된 사용자의 취향이 기록된 각 사용자 프로파일을 기반으로 서비스 지원 시스템은 적절한 서비스를 제공할 수 있다. 둘째, 사용자의 취향을 기록하기 위한 시간적 추론(Temporal Reasoning)이 다. 기록된 내 용들은 사용자 프로파일 (User Profile)을 생성하는데 도움을 준다.

• Geophysics and Geophysical Exploration
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• v.16 no.4
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• pp.293-299
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• 2013

The recent Multiple Lapse Time Window (MLTW) analysis of Korean Peninsula event showed that the focal depth was far greater influence factor than the velocity structure of the model, applying the analysis of the direct simulation Monte Carlo (DSMC) method. Thus, using the events with focal depth of about 10 km, this study considered 330 paths connecting 41 events and 71 stations, and re-examined uniform and depth-dependent velocity models previously studied. As a result, the residual of misfit function greatly decrease from analytic model to DSMC model, reflecting variation of the focal depth from 0 to 10 km. On the other hand, the difference of residuals for each velocity model were relatively small.

• Geophysics and Geophysical Exploration
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• v.7 no.3
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• pp.164-173
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• 2004

To delineate geothermal water movement at the Pohang geothermal development site, Self-Potential (SP) survey and monitoring were carried out during pumping tests. Before drilling, background SP data have been gathered to figure out overall potential distribution of the site. The pumping test was performed in two separate periods: 24 hours in December 2003 and 72 hours in March 2004. SP monitoring started several days before the pumping tests with a 128-channel automatic recording system. The background SP survey showed a clear positive anomaly at the northern part of the boreholes, which may be interpreted as an up-flow Bone of the deep geothermal water due to electrokinetic potential generated by hydrothermal circulation. The first and second SP monitoring during the pumping tests performed to figure out the fluid flow in the geothermal reservoir but it was not easy to see clear variations of SP due to pumping and pumping stop. Since the area is covered by some 360 m-thick tertiary sediments with very low electrical resistivity (less than 10 ohm-m), the electrokinetic potential due to deep groundwater flow resulted in being seriously attenuated on the surface. However, when we compared the variation of SP with that of groundwater level and temperature of pumping water, we could identify some areas responsible to the pumping. Dominant SP changes are observed in the south-west part of the boreholes during both the preliminary and long-term pumping periods, where 3-D magnetotelluric survey showed low-resistivity anomaly at the depth of $600m\~1,000m$. Overall analysis suggests that there exist hydraulic connection through the southwestern part to the pumping well.

• Proceedings of the KSRS Conference
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• 2001.03a
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• pp.35-37
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• 2001

공간데이터의 특성은 양이 방대하고 복잡하여 구축하는데 많은 시간과 비용이 요구되어진다. 이러한 GIS데이터들은 각자의 요구사항을 준수하여 여러 포맷으로 구축되어지기 때문에 현실적으로 동일한 공간 데이터들이 중복해서 구축되는 문제점들이 존재해왔다. 이러한 문제점을 해결하기 위해서 OGC(OpenGIS Consortium)에서는 구축되어 있는 공간 데이터들을 유통할 수 있는 방법에 대해 제안하였고, 이를 정의한 Catalog 명세서가 1999년에 발표되었다. 데이터 유통을 통하여 공간 데이터 중복투자 방지 및 활용을 촉진하기 위해 서비스를 제공하는 카탈로그 서버를 구축하여 사용자들이 원하는 데이터들을 검색, 접근할 수 있도록 하는 것이 본 논문의 목적이다.

• The Journal of Engineering Geology
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• v.3 no.2
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• pp.101-114
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• 1993

GIS technique was applied to identify the regional hydrologic units for groundwater exploitation and recharge analysis in a study area. The technique was very effective to identify the potential areas for groundwater exploitation, and for groundwater management & land use planning. GIS database of environmental resources was complied from a variety of sources and scales as the foundation for analysis, including digitizing and scanning of hardcopy maps. A DEM(Digital Elevation Model) was used to dassify slopes, and identify problematic drainage system. Quantitative analysis of environmental resources helps us to develop the scoring system of GIS model, which evaluates each resource in relation to the others and reflects the relative importance of each resource. ARC4NFO was used to construct digital database, and the cartographic simulation techniques were applied in order to create new maps.

• Geophysics and Geophysical Exploration
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• v.9 no.1
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• pp.19-29
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• 2006

The first Japanese pilot-scale $CO_2$ sequestration project has been undertaken in an onshore saline aquifer, near Nagaoka in Niigata prefecture, and time-lapse well logs were carried out in observation wells to detect the arrival of injected $CO_2$ and to evaluate $CO_2$ saturation in the reservoir. $CO_2$ was injected into a thin permeable zone at the depth of 1110m at a rate of 20-40 tonnes per day. The total amount of injected $CO_2$ was 10400 tonnes, during the injection period from July 2003 to January 2005. The pilot-scale demonstration allowed an improved understanding of the $CO_2$ movement in a porous sandstone reservoir, by conducting time-lapse geophysical well logs at three observation wells. Comparison between neutron well logging before and after the insertion of fibreglass casing in observation well OB-2 showed good agreement within the target formation, and the higher concentration of shale volume in the reservoir results in a bigger difference between the two well logging results. $CO_2$ breakthrough was identified by induction, sonic, and neutron logs. By sonic logging, we confirmed P-wave velocity reduction that agreed fairly well with a laboratory measurement on drilled core samples from the Nagaoka site. We successfully matched the history changes of sonic P-wave velocity and estimated $CO_2$ saturation a(ter breakthrough in two observation wells out of three. The sonic-velocity history matching result suggested that the sweep efficiency was about 40%. Small effects of $CO_2$ saturation on resistivity resulted in small changes in induction logs when the reservoir was partially saturated. We also found that $CO_2$ saturation in the $CO_2$-bearing zone responded to suspension of $CO_2$ injection.