Abstract

A model was established for the fluid - solid interface of semi-infinite medium, and the characteristic equation was established using the potential function. Applying line source at the fluid-solid interface, transform solution of displacement could be obtained, and time-domain solution could be evaluated through the inverse Fourier transform. Two kinds of ultrasound suspension model, UA and HT, were used to study and discuss the effect of sediment content to fluid-solid interface time-domain waveform. The results of two models have a good consistency. The sediment content have a great impact on the Scholte wave. With the increase of the sediment content, for Scholte wave, the velocity increases and the attenuation decreases.

Highlights

  • Urick-Ament model (UA model) and coupling phase model (HT model) to study and discuss the effect of sediment content to fluid-solid interface time-domain waveform

  • MATEC Web of Conferences expressed as I1 \1 .The potential function of fluid medium can be expressed as I2

  • R is the radius of suspended sediment particles, k is real wave number of the pure liquid. ks is the plural wave number, whose real part represents real wave number, imaginary part denotes attenuation

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Summary

Establishment of potential function z

The potential function of solid can be. MATEC Web of Conferences expressed as I1 \1 .The potential function of fluid medium can be expressed as I2. The displacement potential obeys the Helmholtz equation[2]. ° ̄V zx V zx 0 we can get the characteristic equation: am m12 m13 o a A1 o a 0 o. By the formula (8), coefficients A1 B2 C1 can be obtained, the transform solution of displacement of solid can be obtained

Urick and Ament model
Hanker-Temple model
Numerical results
Conclusions
Full Text
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