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Geoacoustic model of the transverse acoustic variability experiment area in the northern East China Sea

机译:东海北部横向声学变化实验区的地球声学模型

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Transverse Acoustic Variability Experiment (TAVEX) is a joint ROK-US acoustic experiment for testing transverse acoustic variability in the northern limit of the East China Sea. TAVEX was performed in a water depth of 70-90 m around 32°30 to 40N, 125°20 to 30E, about 150 km southwest of Cheju Island, in August 2008. Purpose of this paper is to provide geoacoustic models of the TAVEX area, integrated and detailed as available. Two geoacoustic models of three layers were reconstructed, located at 32°40N/125°30E and 32°30N/125°30E of the northern East China Sea, respectively. The models were based on the data of the high-resolution subbottom and air-gun seismic profiles with cores. Geoacoustic data of the cores were extrapolated down to a depth of 100 m of the geoacoustic models. For actual underwater experiments, the P-wave speed of the models was compensated to in situ depth below the sea floor using the Hamilton method.
机译:横向声学变异性实验(TAVEX)是ROK-US联合进行的声学实验,用于测试东海北部边界的横向声学变异性。 TAVEX于2008年8月在距济州岛西南约150 km的32°30至40N,125°20至30E的水深70-90 m内进行。本文的目的是提供TAVEX地区的地声模型,集成且详细可用。重建了三个三层的两个地声模型,分别位于东海北部的32°40N / 125°30E和32°30N / 125°30E。这些模型基于高分辨率的底部和带芯的气枪地震剖面的数据。将岩心的地声数据外推至地声模型的100 m深度。对于实际的水下实验,使用汉密尔顿方法将模型的P波速度补偿到海床以下的原位深度。

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