• Proceedings of the Korea Water Resources Association Conference
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• 2023.05a
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• pp.424-424
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• 2023

댐, 저수지 등 수자원 시스템분석 시 가장 기초가 되는 유입량 자료는 실측 수위(저수량)와 방류량을 역산하여 산정된다. 이 중 댐 수위는 수표면 진동으로 인해 변동이 크며, 특히, 급격한 수위 변화가 발생하는 홍수기에는 수위-저수량 변환 시 큰 오차가 발생하여 유입량 진동이 더욱 커지게 된다. 하지만 홍수기 저수지 운영 효과 분석 등 관련 연구를 위해서는 시간 간격이 짧은 10분 또는 1시간 단위의 유입량 자료가 필요함에 따라 관련 연구 수행 시 이동평균법(Moving Average) 등을 통해 실측 유입량 자료를 보정하여 사용하는 것이 일반적이다. 데이터 평활화를 위해 이동평균법을 적용하면 데이터의 변동을 효과적으로 줄일 수는 있지만 실측자료와 비교하였을 때 첨두 유입량이 큰 폭으로 감소하거나, 첨두 유입량 발생시간이 지체되는 문제가 발생한다. 본 연구에서는 저수지 유입량과 같이 변동이 큰 수문자료의 평활화를 위해 가우시안 가중 이동평균법(Gaussian-weighted moving average technique), 사비츠키-골레이 필터링기법(Savitzky-Golay filtering technique) 등 필터링 기법을 댐 유입량 보정에 적용하고, 이에 따른 효과를 분석하고자 하였다. 이를 위해 2020년 8월에 발생한 홍수사상을 대상으로 충주댐, 합천댐 등 다목적댐 유입량 자료를 수집하고, 보정을 수행하였다. 필터링 기법의 적용 효과 분석을 위해서는 실측자료와 이동평균법을 적용하여 보정한 결과와 비교하였고, 추가적으로 비교적 변동이 작은 일 단위 유입량 자료와의 양적 비교를 진행하였다. 그 결과 이동평균법을 적용하였을 때보다 필터링 기법을 적용하였을 때 실측자료와의 양적 차이가 작고, 첨두 유입량 및 첨두 유입 발생시간에서도 차이를 큰 폭으로 감소시킬 수 있는 것으로 확인되었다.

• Journal of The Institute of Information and Telecommunication Facilities Engineering
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• v.2 no.1
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• pp.37-44
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• 2003

In this paper, a technique to estimate EMI source distribution on a digital circuit board ir introduced. A sensitivity analysis method is applied to reconstruct the source distribution from measured electric field data. Results from a single-layer measurement and a double-layer measurement are compared. It will be shown, from the simulation, that the use of sensitivity analysis for the EMI source reconstruction problem can be a very promising technique.

• 한국정보통신설비학회:학술대회논문집
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• 2002.08a
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• pp.6-9
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• 2002

In this paper a technique to estimate EMI source distribution on a digital circuit board is introduced. A sensitivity analysis method is applied to reconstruct the source distribution from measured electric field data. Results from a single-layer measurement and a double-layer measurement are compared. It will be shown, from the simulation, that the use of sensitivity analysis for the EMI source reconstruction problem can be a very promising technique.

• Economic and Environmental Geology
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• v.28 no.4
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• pp.425-431
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• 1995

Genetic algorithms are so named because they are analogous to biological processes. The model parameters are coded in binary form. The algorithm then starts with a randomly chosen population of models called chromosomes. The second step is to evaluate the fitness values of these models, measured by a correlation between data and synthetic for a particular model. Then, the three genetic processes of selection, crossover, and mutation are performed upon the model in sequence. Genetic algorithms share the favorable characteristics of random Monte Carlo over local optimization methods in that they do not require linearizing assumptions nor the calculation of partial derivatives, are independent of the misfit criterion, and avoid numerical instabilities associated with matrix inversion. An additional advantage over converntional methods such as iterative least squares is that the sampling is global, rather than local, thereby reducing the tendency to become entrapped in local minima and avoiding the dependency on an assumed starting model.

• Tunnel and Underground Space
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• v.15 no.5 s.58
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• pp.352-358
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• 2005

For non-destructive testing of concrete structures, time and frequency domain method were applied to detect cavity in underground model and pier model. To interpret the measured data, time domain method made use of tomography which was completed with first arrivaltime and inversion method. In this steady, frequency domain method using Fourier transform was tried. Maximum frequency in the frequency domain was analyzed to calculate location of cavity.

• The Journal of Korean Institute of Electromagnetic Engineering and Science
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• v.11 no.6
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• pp.939-945
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• 2000

A cylindrical object buried in the lossy half space is reconstructed from the measured scattered fields above the lossy half space. The position, the size and the medium parameters i.e. relative dielectric constants and conductivity of the buried object as well as the medium parameters of the background lossy half space are obtained from the scattered fields by using the iterative inversion method and the optimization hybrid algorithm combining the genetic algorithm and the Levenberg-Marquardt algorithm. Illposedness of the inversion due to the measurement errors in the scattered fields are regularized by filtering out the evanescent modes in the spatial frequency spectrum domain.

• Geophysics and Geophysical Exploration
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• v.5 no.1
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• pp.46-55
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• 2002

We investigated the distorting factors of velocity structure reconstructed by traveltime inversion. The set of models that fit the data in a numerical sense usually contains unrealistic models. Reconstructed velocity structure was enhanced because unreasonable models were eliminated by defining constraint of variable grid using a priori information. To correct time delay of source explosion, which distorts traveltime tomograms, terms for correction of time delay was formulated into equation of travel time tomography.

• Proceedings of the KIEE Conference
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• 1999.07a
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• pp.79-82
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• 1999

So far, The methods for identifying the parameters of some region or material have been developed. This paper describes a new method for electric resistivity reconstruction using multi-resolution property of wavelet. The outputs of the potential electrodes are computed using two dimensional FEM in the wave number space by Fourier transforming the governing equation. The resistance distribution in the region of interests, which makes the computed potential distribution coincide with the measured potential, is found by minimizing the objective function using an optimization method. Multi-resolution analysis introduced in this paper will be proved to be the proper method in the viewpoint of effectivity and time-consuming by the numerical results.

• Journal of the Earthquake Engineering Society of Korea
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• v.27 no.2
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• pp.111-118
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• 2023

The 2017 Pohang earthquake afflicted more significant economic losses than the 2016 Gyeongju earthquake, even if these earthquakes had a similar moment magnitude. This phenomenon could be due to local site conditions that amplify ground motions. Local site effects could be estimated from methods using the horizontal-to-vertical spectral ratio, standard spectral ratio, and the generalized inversion technique. Since the generalized inversion method could estimate the site effect effectively, this study modeled the site effects in the Korean peninsula using the generalized inversion technique and the Fourier amplitude spectrum of ground motions. To validate the method, the site effects estimated for seismic stations were tested using recorded ground motions, and a ground motion prediction equation was developed without considering site effects.

• Journal of the Korean Geophysical Society
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• v.5 no.2
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• pp.99-109
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• 2002

Among the geophysical exploration methods, electromagnetic method(EM) has the broadest range of instrumental systems and remarkable range of applications. There are a lot of available techniques and instruments which have different depth of investigation and resolution depending on the operating frequency and source-receiver configuration. Furthermore, it is very easy to apply on the engineering and environmental problems since modern EM equipments are remarkably portable, considering their sophistication. Even though electromagnetic theory is very complex and not easy to understand, rapid avances in recent computer technology have made it possible to conduct accurate forward modeling and inversion of various EM exploration data. Here, we are going to provide brief theoretical principles, survey techniques and case histories of some selected EM methods that can be applied to geotechnical and environmental problems in Korea.