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浅海平均混响强度的简正波理论

NORMAL-MODE THEORY OF THE AVERAGE REVERBERATION INTENSITY IN SHALLOW-WATER

  • 摘要: 本文用简正波方法导出了浅海远程混响强度的一般表式,该式对较广泛的一类声速剖面、海底反射与散射系数皆适用。由于考虑了复本征值对简正波入射场的影响,所得结果比以往的混响场简正波理论有较大的改进。所得出的平均混响强度的表式物理意义清楚,形式简单,便于进行数值计算与解析讨论。作为例子,文中分析了负跃层浅海中平均混响强度的衰减规律。计算表明,当声源与接收器皆位于跃变层之上时,远程混响强度与r-5成正比。

     

    Abstract: In this paper, the general expressions of long-range average revedberation intensity in shallow water have been developed on the basis of the normal-mode thoery. Because the effects of the complex eigenvalues on the mode incident field have been considered, the results are more accurate than those in the former normal-mode theories of reverberation. In addition, for the sake of simplifying the calculations and making the results convenient to compare with the experiments, the reverberation intensity was smooth-averaged in space. The obtained expressions have obvious physical meaning and concise form so that they can be used for numerical calculation and analytical discussion. These expressions are suitable for wider types of velocity-profile, bottom-reflection and scattering coefficients.
    When the source and receiver are at the same position, the reverberation intensity is expressed as IR=\fracc_0\pi E_0r \int_a^c^x/2 \frac\sin (2a)\sigma (a)\exp - 2\beta (a)rdaS'(a)|V(a)|D(z) + sin ^2a(z)1/2D(h) + sin ^2a1/2^2
    As an example, the average reverberation intensity in shallow-water with the thermocline is evaluated. The result shows that when both the source and receiver are located above the thermocline, the long-range revedberation intensity is proportional to r-5. This result is in agreement with the experimental data.

     

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