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Sound beam scanning in sediment layer using phase conjugated pseudo sound source

机译:使用相位共轭伪声源扫描沉积层中的声束

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When an object that is buried underwater in a sediment layer is detected from the diagonal, detection is often hampered by reflection from the bottom surface. Stated in different terms, the sound-wave energy that reaches the object is small because of reflection and refraction that occurs at the bottom surface when a sound wave is applied to the object in the sediment for diagonal detection. To alleviate that problem, a pseudo sound source can be set up in the sediment layer. The sound wave radiated from the pseudo sound source is then received by a time-reversal array. The sound wave can be injected into the sediment layer by reversing the received signal with time, and radiating it again from the time-reversal array. The beam can hit the target through movement of this pseudo sound source along the bottom surface. The sound wave that hits the target is reflected and returns in water. The sound wave is subsequently reflected many times at the surface and bottom, and is diffused over time. The passive-phase conjugate processing is then given to the received diffusing signal to reduce this diffusion. The pulse is compressed by this processing, thereby obtaining the target position.
机译:当从对角线检测到水下埋在沉积物层中的物体时,检测通常会受到底面反射的阻碍。换句话说,由于将声波施加到沉积物中的对象以进行对角线检测时,由于在底部表面发生的反射和折射,到达对象的声波能量较小。为了减轻该问题,可以在沉积物层中建立伪声源。从伪声源辐射的声波然后被时间反转阵列接收。通过将接收到的信号随时间反转,然后从时间反转阵列中再次辐射出去,可以将声波注入沉积层。通过该伪声源沿底面的移动,光束可以击中目标。击中目标的声波在水中反射并返回。声波随后在表面和底部多次反射,并随时间扩散。然后,对接收到的扩散信号进行无源共轭处理,以减少这种扩散。通过该处理将脉冲压缩,从而获得目标位置。

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