• 제목/요약/키워드: Dispersive Wave

검색결과 132건 처리시간 0.028초

Dispersive Broadening of Two-photon Wave Packets Generated via Type-I and Type-II Spontaneous Parametric Down-conversion

  • Hong, Kang-Hee;Baek, So-Young;Kwon, Osung;Kim, Yoon-Ho
    • Journal of the Korean Physical Society
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    • 제73권11호
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    • pp.1650-1656
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    • 2018
  • Photons generated via spontaneous parametric down-conversion (SPDC) have broad spectrums and suffer from dispersive broadening of the temporal wave packets when they are transmitted through dispersive media. In this paper we theoretically and experimentally study the detailed amount of the temporal broadening of the two-photon wave packets generated via both type-I and type-II SPDC with ${\beta}-BaB_2O_4$ of various lengths, by transmitting them through optical fibers. We interpret the results with respect to the spectral properties of the two-photon wave packets. We believe that our results will contribute to implementing protocols involving long-range distributions of photon pairs.

고립파와 파도패킷의 상호작용 (On the Interaction of a Solitary Wave and a Wave-Packet)

  • 김종언;장택수
    • 대한조선학회논문집
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    • 제60권5호
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    • pp.341-350
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    • 2023
  • In this paper, numerical experiments are performed to examine the collision between a solitary wave and a wave-packet (dispersive wave) in shallow water. We attempt to introduce the improved Boussinesq equation governing the experiments, which is solved by using a semi-analytical approach, called Pseudo-parameter Iteration method(PIM). Using various numerical experiments, we have observed that the wave-packet (propagating dispersive wave) experiences a phase shift after collision with a solitary wave. This phenomenon may be considered as a nonlinear wave-wave interaction in shallow water.

레이다파의 분산성 가이드 현상을 이용한 지하 물성 계산 (Determination of dielectric property of subsurface by dispersive guided GPR wave)

  • 이명종;;김정호
    • 한국지구물리탐사학회:학술대회논문집
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    • 한국지구물리탐사학회 2006년도 공동학술대회 논문집
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    • pp.25-30
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    • 2006
  • 지표수의 토양층 침투에서와 같이 천부 토양층이 하부에 비하여 수분 함유량이 높은 조건하에서 레이다파는 감쇄되지 않고 습윤 토양층을 통하여 가이드 되는 현상을 보이는 경우가 발생한다. 이는 레이다파의 분산성 가이드 현상으로 천부 층의 두께가 레이다파의 파장보다 비슷하거나 작은 경우에 발생한다. 이 연구에서는 FDTD에 의한 수치 모델링을 수행하고 F-K 분석을 통하여 속도분산곡선을 획득함으로써 레이다파의 분산성 가이드 현상을 확인하였다.이와 같은 가이드 현상은 모드 전파이론으로 설명되며,이 연구에서는 이를 이용하여 2층 층서구조의 두 층의 유전율과 층의 두께를 정확히 계산할 수 있는 알고리듬을 개발하였다. 이론 모델링 자료에 대한 실험 결과 두층의 유전율과 두께를 정확하게 계산할 수 있었으며, 특히 고차 모드를 포함함으로써 그 정확도를 향상 시킬 수 있었다. 향후 비슷한 조건을 가지는 현장에 적용하여 정량적인 전기적 물성을 획득할 수 있을 것으로 기대된다.

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해저구조물에 대한 비선형분산파의 변형 (Deformation of Non-linear Dispersive Wave over the Submerged Structure)

  • 박동진;이중우
    • 한국항만학회지
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    • 제12권1호
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    • pp.75-86
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    • 1998
  • To design a coastal structure in the nearshore region, engineers must have means to estimate wave climate. Waves, approaching the surf zone from offshore, experience changes caused by combined effects of bathymetric variations, interference of man-made structure, and nonlinear interactions among wave trains. This paper has attempted to find out the effects of two of the more subtle phenomena involving nonlinear shallow water waves, amplitude dispersion and secondary wave generation. Boussinesq-type equations can be used to model the nonlinear transformation of surface waves in shallow water due to effect of shoaling, refraction, diffraction, and reflection. In this paper, generalized Boussinesq equations under the complex bottom condition is derived using the depth averaged velocity with the series expansion of the velocity potential as a product of powers of the depth of flow. A time stepping finite difference method is used to solve the derived equation. Numerical results are compared to hydraulic model results. The result with the non-linear dispersive wave equation can describe an interesting transformation a sinusoidal wave to one with a cnoidal aspect of a rapid degradation into modulated high frequency waves and transient secondary waves in an intermediate region. The amplitude dispersion of the primary wave crest results in a convex wave front after passing through the shoal and the secondary waves generated by the shoal diffracted in a radial manner into surrounding waters.

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Design and Fabrication of Reflective Array Type Wideband SAW Dispersive Delay Line

  • Choi Jun-Ho;Yang Jong-Won;Nah Sun-Phil;Jang Won
    • Journal of electromagnetic engineering and science
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    • 제6권2호
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    • pp.110-116
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    • 2006
  • A reflective array type surface acoustic wave(SAW) dispersive delay line(DDL) with high time-bandwidth at the V/UHF-band is designed and fabricated for compressive receiver applications. This type of the SAW DDL has the properties of the relative bandwidth of 20 %, the time delay of 49.89 usec, the insertion loss of 38.5 dB and the side lobe rejection of 39 dB. In comparison with a commercial SAW DDL, the insertion loss, amplitude ripple and side lobe rejection are improved by $1.5dB{\pm}0.6dB$ and 4 dB respectively. Using the fabricated SAW DDL, the prototype of the compressive receiver is developed. It is composed of RF converter, fast tunable LO, chirp LO, A/D converter, signal processing unit and control unit. This prototype system shows a fine frequency resolution of below 30 kHz with high scan rate.

웨이블릿 변환을 이용한 유도초음파의 모드 확인 (Guided Wave Mode Identification Using Wavelet Transform)

  • Ik-Keun Park
    • 한국공작기계학회논문집
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    • 제12권5호
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    • pp.94-100
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    • 2003
  • One of unique characteristics of guided waves is a dispersive behavior that guided wave velocity changes with an excitation frequency and mode. In practical applications of guided wave techniques, it is very important to identify propagating modes in a time-domain waveform for determination of detect location and size. Mode identification can be done by measurement of group velocity in a time-domain waveform. Thus, it is preferred to generate a single or less dispersive mode But, in many cases, it is difficult to distinguish a mode clearly in a time-domain waveform because of superposition of multi modes and mode conversion phenomena. Time-frequency analysis is used as efficient methods to identify modes by presenting wave energy distribution in a time-frequency. In this study, experimental guided wave mode identification is carried out in a steel plate using time-frequency analysis methods such as wavelet transform. The results are compared with theoretically calculated group velocity dispersion own. The results are in good agreement with analytical predictions and show the effectiveness of using the wavelet transform method to identify and measure the amplitudes of individual guided wave modes.

표면파 시험을 위한 향상된 위상각 스펙트럼 결정방법의 개발 (Development of advanced phase spectrum for surface wave method)

  • 박형춘;조성은
    • 한국지반공학회:학술대회논문집
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    • 한국지반공학회 2008년도 춘계 학술발표회 초청강연 및 논문집
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    • pp.599-604
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    • 2008
  • The dispersive phase velocity of a wave propagating through a system is an important parameter and carries valuable information in non-destructive tests related to multilayered systems such as a soil site. The dispersive phase velocity of a wave can be determined using the phase spectrum, which is easily evaluated through the cross power spectrum. However, the phase spectrum as determined using the cross power spectrum is sensitive to background noise which always exists in the field. This causes difficulties in the determination of the dispersive phase velocities. In this paper, a new method to evaluate the phase spectrum using the harmonic wavelet transform is proposed. The proposed method can successfully remove background noise effects. To evaluate the validity of the proposed method, numerical simulations of multi-layered systems were performed. Phase spectrums by the proposed method were found to be in good agreement with the actual phase spectrums under conditions characterized by heavy background noise. This shows the potential of the proposed method.

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TRAVELING WAVE SOLUTIONS TO THE HYPERELASTIC ROD EQUATION

  • MOON, BYUNGSOO
    • Journal of applied mathematics & informatics
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    • 제33권3_4호
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    • pp.261-273
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    • 2015
  • We consider the hyperelastic rod equation describing nonlinear dispersive waves in compressible hyperelastic rods. We investigate the existence of certain traveling wave solutions to this equation. We also determine whether two other equations(the b-family equation and the modified Camassa-Holm equation) have our solution type.

Accurate FDTD Dispersive Modeling for Concrete Materials

  • Chung, Haejun;Cho, Jeahoon;Ha, Sang-Gyu;Ju, Saehoon;Jung, Kyung-Young
    • ETRI Journal
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    • 제35권5호
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    • pp.915-918
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    • 2013
  • This work presents an accurate finite-difference time-domain (FDTD) dispersive modeling of concrete materials with different water/cement ratios in 50 MHz to 1 GHz. A quadratic complex rational function (QCRF) is employed for dispersive modeling of the relative permittivity of concrete materials. To improve the curve fitting of the QCRF model, the Newton iterative method is applied to determine a weighting factor. Numerical examples validate the accuracy of the proposed dispersive FDTD modeling.

GUIDED WAVE MODE IDENTIFICATION USING WAVELET TRANSFORM

  • Park, Ik-Keun;Kim, Hyun-Mook;Kim, Young-Kwon;J. L. Rose
    • 한국공작기계학회:학술대회논문집
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    • 한국공작기계학회 2003년도 춘계학술대회 논문집
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    • pp.79-85
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    • 2003
  • One of unique characteristics of guided waves is a dispersive behavior that guided wave velocity changes with an excitation frequency and mode. In practical applications of guided wave techniques, it is very important to identify propagating modes in a time-domain waveform for determination of defect location and size. Mode identification can be done by measurement of group velocity in a time-domain waveform. Thus, it is preferred to generate a single or less dispersive mode But in many cases, it is difficult to distinguish a mode clearly in a time-domain waveform because of superposition of multi modes and mode conversion phenomena. Time-frequency analysis is used as efficient methods to identify modes by presenting wave energy distribution in a time-frequency. In this study, experimental guided wave mode identification is carried out in a steel plate using time-frequency analysis methods such as wavelet transform. The results are compared with theoretically calculated group velocity dispersion curves. The results are in good agreement with analytical predictions and show the effectiveness of using the wavelet transform method to identify and measure the amplitudes of individual guided wave modes.

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