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나영남,손수욱,한주영,이근화,Na, Youngnam,Son, Su-Uk,Hahn, Jooyoung,Lee, Keunhwa The Acoustical Society of Korea 2022 韓國音響學會誌 Vol.41 No.2
In order to examine the possibility of horizontal simulations of acoustic waves on the environments of big water depth variations, this study introduces a 3-dimensional model based on the pababolic equation. The model gives approximated solutions by separating the cross- and non cross-terms in the equation. Assuming artificial bathymetry (25 km × 4 km) with a source frequency 75 Hz, the simulations give clear horizontal refractions on the transmission loss distributions. The degree of refractions shows non-linear increase along the propagating range and proportional increase with water depth along the cross range. Another simulations with the real bathymetry (25 km × 8 km) also give clear horizontal refractions. The horizontal distributions present little difference with the depth resolution variations of the same data source because the model gives interpolations over the depth data before simulations. Meanwhile, the horizontal distributions show big difference with those of different data sources.
김병욱,안상겸,이근화,성우제,한주영,Kim, ByoungUk,An, SangKyum,Lee, Kuenhwa,Seong, WooJae,Hahn, JooYoung 한국군사과학기술학회 2013 한국군사과학기술학회지 Vol.16 No.4
Passive sonar in submarine can detect the target in long range and can attack using it. There are many noises which can be received at passive sonar of submarine. When noise received in the sonar it make diverse interference pattern depend on the ocean ambient and movement scenario. Interference pattern can be explained by theory of waveguide invariant. In this paper, analyze the interference pattern according to the relative motions of surface ship and submarine. And analyze the occurrence reason of 2 kinds of interference patterns those are usually display on the submarine console. The results show that if relative speed of submarine and target increase then gradient of interference pattern will increase. And closest point approach of submarine and target decrease then gradient of interference pattern will increase. Bathtube pattern usually appear when target pass though close to submarine and Pinetree pattern appear target pass though above of submarine.
거제 인근해역에서 측정된 중주파수 음향 해저면 반사 신호를 이용한 표층 해저면 두께 추정
권혁종,최지웅,손수욱,조성호,한주영,박정수,박경주,Kwon, Hyuckjong,Choi, Jee Woong,Son, Su-Uk,Cho, Sungho,Hahn, Jooyoung,park, Joung-Soo,Park, Kyeongju 한국음향학회 2016 韓國音響學會誌 Vol.35 No.6
천해 환경에서 수평입사각에 따른 음향반사 신호 측정 실험을 2015년 10월 거제 인근 해역에서 실시하였다. 본 논문에서는 수평입사각 $9{\sim}14^{\circ}$ 범위에서 측정된 중주파수 4 ~ 8 kHz의 표층 해저면 반사 신호와 하부 퇴적층 반사신호의 도달시간 차이를 이용하여 표층 퇴적층의 두께를 역으로 추정하였다. 실험 해역의 지질 정보는 한국지질자원 연구원에서 제공한 실험 해역의 평균입도범위인 $8{\sim}10{\phi}$를 사용하였다. 두 다중경로의 도달시간 차이를 이용하여 추정한 표층 퇴적층의 두께는 4 ~ 7 m이며, 한국해양과학기술원이 제공한 실험 해역 인근의 천부지층탐사기를 이용한 하부 퇴적층 분석 결과와 비교하였다. Measurements of bottom loss as a function of grazing angle (in range of $9{\sim}14^{\circ}$) at a frequency range of 4 ~ 8 kHz were conducted on an experimental site off Geoje island in October 2015. Geoacoustic inversion of the surficial sediment thickness is performed using the arrival time difference between the surficial layer and the sub-bottom layer reflected signal. To invert the thickness of surficial sediment, we used the grain size of $8{\sim}10{\phi}$ obtained by KIGAM (Korea Institute of Geoscience and Mineral Resources). The thickness of the surficial sediment was estimated to be 4 ~ 7 m. Finally, this inversion result was compared with the geoacoustic observation conducted by the KIOST (Korea Institute of Ocean Science & Technology) using sub-bottom profiler.