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It is estimated the thickness of the material layer, which can be characterized by
determining the velocity of the Rayleigh wave of a certain frequency. This analysis is
based on the depth distribution of the Rayleigh wave energy. A criterion is proposed
according to which wave velocity is determined by a layer of material with a
thickness of 0,6 Λ (Λ is the wavelength).
To ensure the required resolution of measuring of changes in the surface acoustic
Rayleigh wave parameters in thickness, it is justified the use of long-term probing
radio pulses, which are narrowband. The width of the allowable spectrum of Rayleigh
wave acoustic pulse and its connection with depth separation are analyzed. It is
shown that for high separation it is necessary to use probing acoustic pulses with
duration one and half orders of magnitude for the period of high-frequency signal
filling.
A method for measuring the velocity of surface acoustic Rayleigh waves based
on the use of long-term probing radio pulses has been developed. Rigidly connected
piezoelectric transducers are used to measure the speed of Rayleigh surface acoustic
waves, and the measurement is performed by determining the time offset of the
probing signal relative to the reference sinusoidal signal.
To determine the distribution of surface layer parameters by thickness based on
probing surface acoustic Rayleigh waves with different frequencies, the inverse
problem is solved, which includes determining the effective penetration depth of the
surface acoustic Rayleigh wave and the algorithm for determining surface layer
thickness parameters which is based on velocity changes of acoustic surface
Rayleigh wave with different frequency.
This method has been tested on two types of control objects - sills and objects
with abrasive blasting, which confirmed the manufacturability and efficiency of its
use.
A method for studying the parogon material has been developed and local
sections of the parogon in which the Rayleigh wave velocity decreases have been
identified, and the dependence of this decrease on the wave frequency is also