• Title/Summary/Keyword: 음파 전달손실

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Characteristics of Acoustic Environment in three regions along the Korean East Coast (한반도 연안 3개 해역에서의 수중음향환경 특성)

  • Park S.W.;Yun J. Y.;Kim K.
    • Proceedings of the Acoustical Society of Korea Conference
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    • autumn
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    • pp.417-420
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    • 2004
  • 동해는 크게 북한한류계수의 지배적인 영향을 받는 북부해역, 동한난류계수의 지배적인 영향을 받는 남부해역과 이들이 만나서 극전선이 형성되는 중부해역 등 세 해역으로 구분할 수 있고 이러한 환경에서의 해군 함정의 대잠탐지환경은 같은 동해라 하더라도 크게 다를 것으로 예상된다. 본 연구에서는 저주파 거리종속 모델인 RAM 을 이용하여 평균해황 하에서 각 해역에서의 전달손실 값을 비교하였다. 음원을 수심 100m, 수신기 수심을 10m와 100m로 설정하여 실험을 하였으며 아울러 평균해황이 아닌 일정시기에 관측한 순간해황 자료를 통한 모델결과도 같이 분석하였다. 실험결과, 연안에 위치한 음원으로부터 음파가 외해로 전달됨에 따라 냉난수대간의 수온전선 영향을 받게되며 수온전선을 통과하면서 남부해역에서의 음파는 중부 및 북부해역 보다 난류의 영향을 더 많이 받게된다. 따라서 북부보다는 중부해역이, 중부보다는 남부해역에서의 전달손실값이 더 커지게 된다. 특히 이러한 경향은 북한한류계수가 발달하여 난류와 수온전선이 형성되는 8월에 더 큰 것으로 나타났다.

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Temporal and Spatial Variability of Sound Propagation Characteristics in the Northern East China Sea (동중국해 북부해역에서 음파전달 특성의 시공간적 변동성)

  • Park, Kyeongju;Chu, Peter Cheng
    • Journal of the Korea Institute of Military Science and Technology
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    • v.18 no.2
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    • pp.201-211
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    • 2015
  • Acoustic propagation in shallow water with changing environments is a major concern of navy. Temporal and spatial variability of acoustic propagation in the northern East China Sea (ECS) is studied, using the 11 years hydrographic data and the Bellhop acoustic model. Acoustic propagation in the northern ECS is highly variable due to extensive interaction of various ocean currents and boundaries. Seasonal variations of transmission loss (TL) with various source depths are highly affected by sharp gradient of sound speed and bottoms interaction. Especially, various bottom sediment types lead to severely degrading a waterborne propagation with bottom loss. In particular, the highly increased TL near the ocean front depends on the source position, and the direction of sound propagation.

Coastal upwelling observed off the East coast of Korea and variability of passive sound detection environment (동해 연안에서 관측된 용승현상과 수동 음탐환경의 변화)

  • Sang-Shin, Byun;Chang-Bong, Cho
    • The Journal of the Acoustical Society of Korea
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    • v.41 no.6
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    • pp.601-609
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    • 2022
  • In August 2007, coastal upwelling occurred off the east coast of Korea, and vertical water temperature and salinity data were obtained from a real-time surface ocean buoy. Based on the time series observation data, a vertical sound velocity structure was calculated before, during, and after the occurrence of the coastal upwelling, and how the coastal upwelling affects the sound propagation and detection environment through acoustic modeling considering the horizontal scale and actual seabed topography. As a result of comparing and analyzing the low-frequency (500 Hz) sound transmission loss and the target detection range by depth using the parabolic equation model, it was analyzed that if coastal upwelling occurs, a detection gain of up to about 10 dB can be expected. In addition, through this study, it was confirmed that the characteristics of sound propagation can be greatly changed even in a short period of about 2 to 3 days before and after coastal upwelling.

A Study on Determining the Transmission Loss of Water-Borne Noise Silencer in a Sea-Connected Piping System (해수연결 배관계 소음감소기의 투과손실 측정에 관한 연구)

  • Park, Kyung-Hoon
    • The Journal of the Acoustical Society of Korea
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    • v.26 no.6
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    • pp.286-292
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    • 2007
  • The dominant source of noise in a sea-connected piping system is usually due to a seawater cooling pump which circulates seawater to operate onboard equipments normally, and so its water-borne noise with some tonal frequencies should be reduced using proper silencers. In order to obtain the transmission loss of water-borne noise silencers experimentally the present paper suggests a transfer function technique that acoustic wave in the piping system is decomposed into its incident and transmitted components when the reflection at the termination of the system exists. Good agreement in the interested frequency range with theory and the proposed technique shows the validity of the technique.

Time Variation Characteristics of Internal Waves and Acoustic Pressures Observed in Shallow Water (천해에서 관측한 내부파와 음장의 시간변화 특성)

  • 나영남
    • Proceedings of the Acoustical Society of Korea Conference
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    • 1998.06d
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    • pp.18-24
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    • 1998
  • 최근의 연구를 통해 해양의 내부파가 음파전달에 영향을 주어 비정상적인 손실을 일으키는 것을 밝혀졌다. 한국 동해세서도 강한 수온약층을 중심으로 내부파가 존재할 것으로 여겨져 왔으며, 이를 규명하고자 '98년 6월 각종 장비를 동원한 해양 관측을 동해항 근해에서 실시하였다. 또한 내부파에 의한 음파의 전파 특성을 추정학자 음원과 수신기를 고정한 상태에서 음향 실험을 실시하였다. 실험 결과 전형적인 내부파는 주기가 약 5-12분이고 최대 진폭은 15m 정도임이 밝혀졌다. 특히 10여개의 내부파 묶음이 약 36cm/sec 의 속도로 이동하고 있음도 확인하였다. 15개의 음향센서로 이뤄진 수직선배열 수신기와 음원을 이용한 음향 실험결과 역시 4-12분 주기에서 부분적으로 스펙트럼이 높게 나타났으며, 특히 주파수 1kHz 인 경우에는 4, 6분 주기에서 15개의 센서에 대해 일관되게 높은 스펙트럼 준위가 나타났다. 내부파에 의한 이러한 음파의 특성은 음파의 모든간 결함으로 나타나는 일종의 간섭 현상으로 설명될 수 있다.

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Shallow water Low-Frequency Reverberation Model (천해 저주파 잔향음 예측모델)

  • Kim Namsoo;Oh Suntaek;Na Jungyul
    • Proceedings of the Acoustical Society of Korea Conference
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    • spring
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    • pp.429-432
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    • 2002
  • 천해에서의 저주파 단상태 잔향음 모델(L-HYREV)을 개발하였다. 음선이론에 기초한 전파모델은 해저 내로 투과되는 음파에 대한 효과를 적절하게 고려 할 수 없으므로, 해저 내 상호작용을 계산할 수 있는 전파모델이 필요하다. 따라서 본 논문에서는 RAM을 이용해서 전달손실을 계산 후, 다중경로 확장모델을 이용해서 산출한 전달손실을 보정하였다. 모델의 검증을 위하여 GSM(generic sonar model) 잔향음 모의 신호 및 실측잔향음 신호와 비교하였으며, 비교 결과 GSM 보다 L-HYREV 모델이 저주파 잔향음 예측에 적합함을 확인할 수 있다.

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Shallow Water Low-frequency Reverberation Model (천해 저주파 잔향음 예측모델)

  • 김남수;오선택;나정열
    • The Journal of the Acoustical Society of Korea
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    • v.21 no.8
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    • pp.679-685
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    • 2002
  • Low-frequency mono-static reverberation model for shallow-water environment is presented. It is necessary to develop the transmission loss model to calculate the sub-bottom interaction because the ray-based transmission loss model is difficult to compute the pressure accurately which penetrates the bottom medium. In this paper reverberation level is calculated using the RAM (Range dependent Acoustic Model) to augment the multi-path expansion model because it does not estimate transmission loss accurately in shallow water. The signals generated by the L-HYREV and the GSM are compared with the observed signals and it is showed that the L-HYREV model provides a closer fit to the observed signals than those obtained using the GSM.

Analysis of Surface Sound Channel by Low Salinity Water and Its Mid-frequency Acoustic Characteristics in the East China Sea and the Gulf of Guinea (동중국해와 기니만에서 저염분수로 인한 표층음파채널과 중주파수 음향 특성 분석)

  • Kim, Hansoo;Kim, Juho;Paeng, Dong-Guk
    • The Journal of the Acoustical Society of Korea
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    • v.34 no.1
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    • pp.1-11
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    • 2015
  • Salinity affects sound speed in the low salinity environment, in the seas where freshwater from large rivers and flows into the marginal sea area near the Yangtze River and the Niger River. In this paper, SSC (Surface Sound Channel) formed by low salinity water was investigated in the East China Sea and the Gulf of Guinea of rainy season. The data from KODC (Korea Oceanographic Data Center) in the East China Sea and from ARGO (Array for Real-time Geostrophic Oceanography) in the Gulf of Guinea of the tropical area were used for analysis. SSC haline channel was formed 14 times among 32 SSC occurrences when the 90 data from 9 points were analyzed during a decade (2000 ~ 2009) in the East China Sea. In the Gulf of Guinea, haline channel was formed 18 times among 20 SSC occurrences during 3 years (2006 ~ 2009). When the sound speed gradient was analyzed from temperature-salinity gradient diagram, the gradients of both salinity and temperature affect SSC formation in the East China Sea. In contrast, the salinity gradient mostly affects SSC formation due to the least change of temperature in the well-developed mixed layer in the Gulf of Guinea. Their acoustic characteristics show that channel depth is 6.5 m, critical angle is $1.5^{\circ}$ and difference of transmission loss between surface and thermocline is 11.5 dB in the East China Sea, while channel depth is 18 ~ 24 m, critical angle is $4.0{\sim}5.4^{\circ}$ and difference of transmission loss is 21.5 ~ 27.9 dB in the Gulf of Guinea. These results are expected to be used as a basic understanding of the acoustic transmission changes due to low salinity water at the estuaries and the ocean with heavy precipitation.

Effects of Warm Eddy on Long-range Sound Propagation in the East Sea (동해에서 난수성 소용돌이의 원거리 음파전달에 미치는 영향)

  • Kim, Won-Ki;Cho, Chang-bong;Park, Joung-Soo;Hahan, Jooyoung;Na, Youngnam
    • The Journal of the Acoustical Society of Korea
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    • v.34 no.6
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    • pp.455-462
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    • 2015
  • It is well known that warm eddy is frequently developed through the year in the East Sea. The warm eddy may affect sound propagation due to changes of sound velocity structures in the sea water. To verify the effects of the warm eddy for long-range sound propagation, transmission loss and performance surface, which were used mean direct signal excess range generated by sound propagation modeling using re-analyzed climatology data on March 23th in 2007 were analysed. From these analyses, we found that characteristics of sound propagation in the sea water are changed by the warm eddy, and boundaries of the warm eddy act as a barrier for long-range sound propagation. Furthermore, these disadvantages of the eddy related to sound propagation were increased when the sea bottom depth is shallow.

Development of Range-Dependent Ray Model for Sonar Simulator (소나 시뮬레이터용 거리 종속 음선 모델 개발)

  • Jung, Young-Cheol;Lee, Keunhwa;Seong, Woojae;Kim, Hyoung-Rok
    • The Journal of the Acoustical Society of Korea
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    • v.33 no.3
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    • pp.163-173
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    • 2014
  • Sound propagation algorithm for a sonar simulator is required to run in real-time and should be able to model the range and depth dependence of the Korean ocean environments. Ray model satisfies these requirements and we developed an algorithm for range-dependent ocean environments. In this algorithm, we considered depth-dependence of sound speed through rays based on a rectangular cell method and layer method. Range-dependence of sound speed was implemented based on a split-step method in the range direction. Eigen-ray is calculated through an interpolation of ray bundles and Gaussian interpolation function was used. The received time signal of sonar was simulated by Fourier transform of eigen-ray solution in the frequency domain. Finally, for the verification of proposed algorithm, we compared the results of transmission loss with other validated models such as BELLHOP, SNUPE, KRAKEN and OASES, for the Pekeris waveguide, wedge, and deep ocean environments. As a result, we obtained satisfactory agreements among them.