• 제목/요약/키워드: Inversion method

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복사/난류간 상호작용이 고려된 화염의 온도 및 농도분포의 SRS 역계산 (SRS Inversion of Flame Temperature/concentration Profile with Radiation/Turbulence Interaction)

  • 고주용;김현걸;송태호
    • 대한기계학회논문집B
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    • 제30권9호
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    • pp.891-897
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    • 2006
  • The SRS method is applied to a turbulent flame with radiation/turbulence interaction to invert the temperature and concentration profile. The flame is conditioned as optically thin per each fluctuation length and the flame spectral intensity is measured for inversion. From inversion result, we find that SRS can successfully invert the coupled temperature/concentration fluctuation amplitudes. For two cases of experiments, inverted values are within approximately 1% over the full range of fluctuation amplitude. However, SRS cannot find the detailed local fluctuation parameters such as pattern and phase, etc. as far as they do not affect the resulting radiation intensity. Important available parameters are the mean temperature and the temperature fluctuation amplitude. The radiation/turbulence interaction effect is verified to play an important role in the radiation.

반복적(反復的) 역산법(逆算法)에 의(依)한 중력자료(重力資料)의 해석(解析)에 관(關)한 연구(硏究) (A Study on Interpretation of Gravity Data by using Iterative Inversion Methods)

  • 노철환;양승진;신창수
    • 자원환경지질
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    • 제22권3호
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    • pp.267-276
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    • 1989
  • This paper presents results of interpretaton of gravity data by iterative nonlinear inversion methods. The gravity data are obtained by a theoretical formula for two-dimensional 2-layer structure. Depths to the basement of the structure are determined from the gravity data by four interative inversion methods. The four inversion methods used here are the Gradient, Gauss-Newton, Newton-Raphson, and Full Newton methods. Inversions are performed by using different initial guesses of depth for the over-determined, even-determined, and under-determined cases. This study shows that the depth can be determined well by all of the methods and most efficiently by the Newton-Raphson method.

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일차 차분 전력 분석에 안전한 저면적 AES S-Box 역원기 설계 (DPA-Resistant Low-Area Design of AES S-Box Inversion)

  • 김희석;한동국;김태현;홍석희
    • 정보보호학회논문지
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    • 제19권4호
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    • pp.21-28
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    • 2009
  • 전력분석 공격이 소개되면서 다양한 대응법들이 제안되었고 그러한 대응법들 중 블록 암호의 경우, 암/복호화 연산, 키 스케줄 연산 도중 중간 값이 전력 측정에 의해 드러나지 않도록 하는 마스킹 기법이 잘 알려져 있다. 블록 암호의 마스킹 기법은 비선형 연산에 대한 비용이 가장 크며, 따라서 AES의 경우 가장 많은 비용이 드는 연산은 S-box의 역원 연산이다. 이로 인해 마스킹 역원 연산에 대한 비용을 단축시키기 위해 다양한 대응법들이 제안되었고, 그 중 Zakeri의 방법은 복합체 위에서 정규 기저를 사용한 가장 효율적인 방법으로 알려져 있다. 본 논문에서는 복합체 위에서의 마스킹 역원 연산 방식을 변형, 중복되는 곱셈을 발견함으로써 기존 Zakeri의 방법보다 총 게이트 수가 10.5% 절감될 수 있는 마스킹 역원 방법을 제안한다.

마이크로디스플레이의 액정 러빙 방향과 전압 인가 방식에 따른 Disclination Line의 생성 (Generation of Disclination Line Dependent on Liquid Crystal′s Rubbing Direction and Voltage Driving Method in Microdisplays)

  • 정태봉;송제훈;오세태;이승희
    • 한국전기전자재료학회논문지
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    • 제17권6호
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    • pp.622-632
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    • 2004
  • We have studied how liquid crystal's rubbing direction and voltage driving method affect generation of disclination line. At first, generation of disclination line in vertical alignment(VA) cell and VA-twisted nematic(TN) cell has been examined. When liquid crystal's rubbing direction of bottom substrate was 0$^{\circ}$, the degree of generated disclination line was the smallest value. Further, the generation of disclination line above the electrode is less in the frame inversion than in the line inversion. Secondly, we have examined a generation of disclination line in reflective fringe-field switching cell. When the distance between common electrodes is over 3 ${\mu}{\textrm}{m}$ with on-state of one pixel and off-state of neighboring pixels, the reflectance appears only on-state pixel without generating reflectance in adjacent pixels.

근사적 모델 역변환을 활용한 전기-유압 액추에이터의 적응 위치 제어기 설계 (Adaptive Position Controller Design of Electro-hydraulic Actuator Using Approximate Model Inversion)

  • 이경하;백승국;구자춘
    • 로봇학회논문지
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    • 제11권2호
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    • pp.92-99
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    • 2016
  • An electro-hydraulic actuator (EHA) is widely used in industrial motion systems and the increasing bandwidth of EHA position control is important issue. The model-inverse feedforward controller is known to extend the bandwidth of system. When the system has non-minimum phase (NMP) zeros, direct model inversion makes system unstable. To overcome this problem, an approximate model-inverse method is used. A representative approximate model inversion method is zero phase error tracking control (ZPETC). However, if zeros locate right half plane of z-plane, the approximate inverse model amplifies the high-frequency response. In this paper, to solve the problem of ZPETC, an adaptive model-inverse control is proposed. The adaptive algorithm updates feedforward term in real-time. The effectiveness of the proposed adaptive model-inverse position control strategy is verified by comparison with typical proportional-integral (PI) control and feedforward control by experiments. As a result, the proposed adaptive controller extends the bandwidth of EHA position control.

Electrical resistivity survey and interpretation considering excavation effects for the detection of loose ground in urban area

  • Seo Young Song;Bitnarae Kim;Ahyun Cho;Juyeon Jeong;Dongkweon Lee;Myung Jin Nam
    • Geomechanics and Engineering
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    • 제35권2호
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    • pp.109-119
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    • 2023
  • Ground subsidence in urban areas due to excessive development and degraded underground facilities is a serious problem. Geophysical surveys have been conducted to estimate the distribution and scale of cavities and subsidence. In this study, electrical resistivity tomography (ERT) was performed near an area of road subsidence in an urban area. The subsidence arose due to groundwater leakage that carried soil into a neighboring excavation site. The ERT survey line was located between the main subsidence area and an excavation site. Because ERT data are affected by rapid topographic changes and surrounding structures, the influence of the excavation site on the data was analyzed through field-scale numerical modeling. The effect of an excavation should be considered when interpreting ERT data because it can lead to wrong anomalous results. A method for performing 2D inversion after correcting resistivity data for the effect of the excavation site was proposed. This method was initially tested using a field-scale numerical model that included the excavation site and subsurface anomaly, which was a loosened zone, and was then applied to field data. In addition, ERT data were interpreted using an existing in-house 3D algorithm, which considered the effect of excavation sites. The inversion results demonstrated that conductive anomalies in the loosened zone were greater compared to the inversion that did not consider the effects of excavation.

Development of TFT-LCD panel with reduced driver ICs

  • Kim, Sung-Man;Lee, Jong-Hyuk;Lee, Hong-Woo;Lee, Jong-Hwan;Choi, Kwang-Soo
    • 한국정보디스플레이학회:학술대회논문집
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    • 한국정보디스플레이학회 2008년도 International Meeting on Information Display
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    • pp.352-354
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    • 2008
  • A 15.4" WXGA TFT-LCD, featuring integrated a-Si:H gate driver circuits and reduced data driver ICs, has been developed. To reduce number of data lines into 1/2 of conventional structure, the pixel array has been re-mapped with re-organized data signal. Unintended artificial effects such as flicker were removed by adopting the novel pixel array having a 'zigzag' map. To minimize the power consumption, a column inversion method was incorporated in the zigzag pixel array (Fig.1) without modifying the polarity map of conventional dot inversion method.

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Phase inversion of seismic data

  • Kim, Won-Sik;Shin, Chang-Soo;Park, Kun-Pil
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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    • pp.459-463
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    • 2003
  • Waveform inversion requires extracting a reliable low frequency content of seismic data for estimating of the low wave number velocity model. The low frequency content of the seismic data is usually discarded or neglected because of the band-limited response of the source and the receivers. In this study, however small the spectral of the low frequency seismic data is, we assume that it is possible to extract a reliable phase information of the low frequency from the seismic data and use it in waveform inversion. To this end, we exploit the frequency domain finite element modeling and source-receiver reciprocity to calculate the $Frech\`{e}t$ derivative of the phase of the seismic data with respect to the earth model parameter such as velocity, and then apply a damped least squares method to invert the phase of the seismic data. Through numerical example, we will attempt to demonstrate the feasibility of our method in estimating the correct velocity model for prestack depth migration.

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AN INVERSION METHOD FOR DERIVING PHYSICAL PROPERTIES OF A SUBSURFACE MAGNETIC FIELD FROM SURFACE MAGNETIC FIELD EVOLUTION I. APPLICATION TO SIMULATED DATA

  • Magara, Tetsuya
    • 천문학회지
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    • 제50권6호
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    • pp.179-184
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    • 2017
  • We present a new method for solving an inverse problem of flux emergence which transports subsurface magnetic flux from an inaccessible interior to the surface where magnetic structures may be observed to form, such as solar active regions. To make a quantitative evaluation of magnetic structures having various characteristics, we derive physical properties of subsurface magnetic field that characterize those structures formed through flux emergence. The derivation is performed by inversion from an evolutionary relation between two observables obtained at the surface, emerged magnetic flux and injected magnetic helicity, the former of which provides scale information while the latter represents the configuration of magnetic field.

수신함수를 이용한 관측소 하부의 지진파 속도구조 (Crustal structure beneath broadband seismic station using receiver function)

  • 박윤경;전정수;김성균
    • 한국지진공학회:학술대회논문집
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    • 한국지진공학회 2003년도 춘계 학술발표회논문집
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    • pp.45-49
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    • 2003
  • The velocity structure beneath the CHNB broadband station is determined by receiver function analysis using by from teleseismic P waveforms. The detailed broadband receiver functions are obtained by stacking method for source-equalized vertical, radial and tangential components of teleseismic P waveforms. A time domain inversion uses the stacked radial receiver function to determine vertical P wave velocity structure beneath the station. The crustal velocity structures beneath the stations are estimated using the receiver function inversion method in the case at the crustal model parameterized by many thin, flat-tying, homogeneous layers. The result of crust at model inversion shows the crustal velocity structure beneath the CHNB station varies smoothly with increasing depth, and there are six discontinuity around 2.5km, 6.25km, 12.5km, 22.5km and 27.5km depth, with Moho discontinuity at about 32.5km depth.

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