• Title/Summary/Keyword: 파도

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지상파 DTV 전환 및 실험방송 동향

  • 안동수
    • The Proceeding of the Korean Institute of Electromagnetic Engineering and Science
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    • v.11 no.3
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    • pp.22-34
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    • 2000
  • KBS는 지난 해 국내 최초로 업체와 공동으로 개발한 디지털 송신기를 사용하여 실험방송 송출에 성공하였으며, 현재 본격적인 필드테스트를 수행하고 있는 실정이다. 본 논문에서는 지상파 디지털 TV의 실시를 위해 지상파 디지털 TV의 전환과 실험 방송의 진행 사항, KBS의 지상파 DTV 송신 시스템에 대해 기술적인 사양과 구성, 그리고 필드 테스트 현황에 대해 소개한다.

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배전계통에 있어서의 고조파와 고조파 장해의 실태

  • 대한전기협회
    • JOURNAL OF ELECTRICAL WORLD
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    • no.12 s.72
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    • pp.95-99
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    • 1982
  • 최근의 엘렉트로닉스기술의 급속한 발전과 에너지절약 기운의 고조에 따라 다이리스터등을 응용한 전력제어기술의 다양화$cdot$ 대용량화가 진전되어 배전계통에 있어서의 고조파문제의 필요성은 금후 더욱 증대할 것으로 예상되고 있다. 여기에서는 배전계통에 있어서의 고조파의 실태와 고조파에 의한 장해실태에 대하여 일본의 경우를 들어 그 개요와 최근의 상황을 기술하기로 한다.

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조류에 의한 천해 파랑 스펙트럼 변환의 수치실험 및 서해 연안에서 동시 현장 파랑 관측 자료의 분석

  • 이동영;김유인;송태관
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 1992.08a
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    • pp.90-90
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    • 1992
  • 원해에서 파랑이 천해로 진행할 때 수심의 변화와 마찬가지로 조류에 의해서도 파랑 스펙트럼이 변환된다. 조류에 의해 파랑 스펙트럼의 변환을 정확히 추정하는 수치 모델의 개발은 우리나라 서해안과 같이 조류가 큰 해안에서 해상상태의 추정에 중요한 과제이다.(중략)

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조파기에 의하여 발생된 선단파의 전개

  • 박인규;최항순
    • Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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    • 1991.07a
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    • pp.69-72
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    • 1991
  • 2차원 수조에서 조파기를 정현파형으로 가동시키면, 조파기에서 멀리 떨어진 점에서는 초기의 천이과정을 거쳐 파고와 주기가 일정한 정면파가 전파되어 나간다. 초기의 천이과정에서는 비교적 파장이 긴 파성분이 전파하며 감쇄하는데, 이 파성분은 정상파형과 다른 특성을 보인다.(중략)

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Harmonic Analysis Method for Power Quality Problems (전기품질 분석을 위한 고조파 해석 기법)

  • 사근하;이의용;설용태
    • Proceedings of the KAIS Fall Conference
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    • 2001.11a
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    • pp.147-149
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    • 2001
  • 본 논문에서는 산업용 전력시스템의 전기품질을 평가하기 위한 고조파 해석기법을 제시하였다. 먼저 수변전계통의 전압강하, 고조파, 고장전류 등을 PTW Tool을 이용해서 시뮬레이션 하였으며, 실제 계통에서의 운전중 고조파 현상을 실측치와 비교 분석함으로써 기존 시뮬레이션 기법의 정확성을 검증하였다.

Study on Analysis of Evanescent Waves Generating the Strong End Axial Vibration of a Finite Cylindrical Shell (유한 원통셸의 큰 끝단 종진동을 발생시키는 감쇠파에 대한 분석 연구)

  • Kil, Hyun-Gwon
    • The Journal of the Acoustical Society of Korea
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    • v.30 no.7
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    • pp.361-367
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    • 2011
  • Propagating waves (flexural, longitudinal and shear waves) travelling with constant amplitudes and evanescent waves decaying exponentially are generated on a cylindrical shell. Evanescent waves are generally generated in the vicinity of an vibration excitation point and near ends of the shell. But the evanescent waves can generates strong axial vibration at the ends of the cylindrical shell. The strong end axial vibration due to those evanescent waves has been observed in an author's previous paper dealing with measurements of the in-plane axial vibration of a finite cylindrical shell. In this paper the strong end axial vibration due to the evanescent waves has been theoretically analyzed. In order to analyze the vibration of the cylindrical shell, wave propagation approach has been implemented. Comparison between theoretical and experimental results for the axial vibration of the shell showed that the strong evanescent wave can be generated due to mode conversion (conversion from flexural wave to evanescent wave) at the ends of cylindrical shell. It also showed that the evanescent wave can generate the strong axial vibration near the ends of the cylindrical shell and that it can have effect even on 1/3 of the total length of the shell.

Image Enhancement of the Weathered Zone and Bedrock Surface with a Radial Transform in Engineering Seismic Data (엔지니어링 탄성파자료에서 방사변환을 통한 풍화대 및 기반암 표면의 영상강화)

  • Kim, Ji-Soo;Jeon, Su-In;Lee, Sun-Joong
    • The Journal of Engineering Geology
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    • v.22 no.4
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    • pp.459-466
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    • 2012
  • A difficulty encountered in engineering seismic mapping is that reflection events from shallow discontinuities are commonly overlapped with coherent noise such as air wave, direct waves, head waves, and high-amplitude surface waves. Here, the radial trace transform, a simple geometric re-mapping of a trace gather (x-t domain) to another trace gather (v-t domain), is applied to investigate the rejection effect of coherent linear noises. Two different types of data sets were selected as a representative database: good-quality data for intermediate sounding (hundreds of meters) in a sedimentary basin and very noisy data for shallow (${\leq}50m$) mapping of the weathered zone and bedrock surface. Results obtained with cascaded application of the radial transform and low-cut filtering proved to be as good as, or better than, those produced using f-k filtering, and were especially effective for air wave and direct wave. This simple transform enables better understanding of the characteristics of various types of noise in the RT domain, and can be generally applied to overcoming diffractions and back-scatterings caused by joints, fractures, and faults commonly that are encountered in geotechnical problems.

Surface Wave Method: Focused on Active Method (표면파 탐사: 능동 탐사법을 중심으로)

  • Kim, Bitnarae;Cho, Ahyun;Cho, Sung Oh;Nam, Myung Jin;Pyun, Sukjoon;Hayashi, Koich
    • Geophysics and Geophysical Exploration
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    • v.22 no.4
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    • pp.210-224
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    • 2019
  • Surface wave (SW) surveys, which have been applied to numerous application fields ranging from micro-scale ultrasonic analysis to geological scale analysis, are widely used to monitor near-surface stability. The survey method is basically made through analysis on dispersion of SW propagating along the earth surface, in order to delineate shear velocity structure of subsurface. SW survey data are inverted with assuming one-dimensional (1D) layered-earth in order to recover shear wave velocities of each layer, after being analyzed to make the dispersion curve that shows phase velocity of SW with respect to frequency. This study reviews surface wave surveys with explaining the basic theory including the characteristics of dispersion and the procedure of general data processing. Even though surface wave surveys can be categorized into active and passive methods, this paper focuses only on active surface wave methods which includes continuous SW (CSW), spectral analysis of SW (SASW) and multichannel analysis of SW (MASW). Passive method will be reviewed in the subsequent paper.

Characteristics of Elastic Waves in Sand-Silt Mixtures due to Freezing (동결에 따른 모래-실트 혼합토의 탄성파 특성)

  • Park, Junghee;Hong, Seungseo;Kim, Youngseok;Lee, Jongsub
    • Journal of the Korean GEO-environmental Society
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    • v.13 no.4
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    • pp.27-36
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    • 2012
  • The water in surface of the earth is frozen under freezing point. The freezing phenomenon, which causes the volume change of soils, affects on the behavior of soils and causes the significant damage on the geotechnical structures. The purpose of this study is to investigate the characteristics of elastic waves in sand-silt mixtures using small size freezing cells, which reflect the frozen ground condition due to temperature change. Experiments are carried out in a nylon cell designed to freeze soils from top to bottom. Bender elements and piezo disk elements are used as the shear and compressional wave transducers. Three pairs of bender elements and piezo disk elements are placed on three locations along the depth. The specimen, which is prepared by mixing sand and silt, is frozen in the refrigerator. The temperature of soils changes from $20^{\circ}C$ to $-10^{\circ}C$. The velocities, resonant frequencies and amplitudes of the shear and compressional waves are continuously measured. Experimental results show that the shear and compressional wave velocities and resonant frequencies increase dramatically near the freezing points. The amplitudes of shear and compressional waves show the different tendency. The dominant factors that affect on the shear wave velocity change from the effective stress to the ice bonding due to freezing. This study provides basic information about the characteristics of elastic waves due to the soil freezing.

Broadband Seismic Exploration Technologies via Ghost Removal (도깨비파 제거를 통한 광대역 탄성파 탐사 기술)

  • Choi, Woochang;Pyun, Sukjoon
    • Geophysics and Geophysical Exploration
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    • v.21 no.3
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    • pp.183-197
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    • 2018
  • In the delineation of geological structures using seismic exploration, it is very important to improve resolution of seismic data as well as accurate velocity model building and subsurface imaging. The resolution of seismic data can be enhanced by employing high-frequency energy sources or by applying deconvolution techniques in data processing. In marine seismic exploration, however, the main reason for degradation of resolution is the loss of specific frequency components due to ghosts. If we remove the ghosts, we can obtain broadband seismic data by avoiding frequency loss, and thus providing high-resolution subsurface images. Although ghosts can be properly filtered out in the data processing step, more effective broadband seismic technologies have been developing through the evolution of seismic instruments and the innovation of survey design. Overseas exploration companies developed brand-new configurations of receivers such as over/under streamer and variable-depth streamer, or ghost removal techniques using dual-sensor streamer to serve high-resolution imaging technologies. Unfortunately, neither broadband seismic instrument nor processing technique has been studied in Korea. In this paper, we introduce fundamental theories and current status of broadband seismic technologies to assist domestic researchers to study those technologies.