Nondestructive Evaluation of Materials 2018
DOI: 10.31399/asm.hb.v17.a0006461
|View full text |Cite
|
Sign up to set email alerts
|

Rayleigh Wave Nondestructive Evaluation for Defect Detection and Materials Characterization

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2023
2023
2023
2023

Publication Types

Select...
1

Relationship

0
1

Authors

Journals

citations
Cited by 1 publication
(3 citation statements)
references
References 98 publications
0
3
0
Order By: Relevance
“…The numerical TOF of the reflected wave mode can be calculated using DT num = t 3t 1 , where t 3 is the time corresponding to the maximum amplitude A r of the reflected wave shown in Figure 2a. The theoretical TOF of the transmitted wave can be determined by calculating the distance of the incident Rayleigh mode x 1 to the discontinuity D1, then to the transmitted mode x 2 shown in Figure 4 using DT th = (x 1 + x 2 )/V r , where V r is the Rayleigh wave velocity [7,42] for a given material. The difference in the theoretical and numerical TOF: DT = DT num À DT th , will be proportional to the change in the phase, which can be calculated using:…”
Section: Effect On Phasementioning
confidence: 99%
See 2 more Smart Citations
“…The numerical TOF of the reflected wave mode can be calculated using DT num = t 3t 1 , where t 3 is the time corresponding to the maximum amplitude A r of the reflected wave shown in Figure 2a. The theoretical TOF of the transmitted wave can be determined by calculating the distance of the incident Rayleigh mode x 1 to the discontinuity D1, then to the transmitted mode x 2 shown in Figure 4 using DT th = (x 1 + x 2 )/V r , where V r is the Rayleigh wave velocity [7,42] for a given material. The difference in the theoretical and numerical TOF: DT = DT num À DT th , will be proportional to the change in the phase, which can be calculated using:…”
Section: Effect On Phasementioning
confidence: 99%
“…Surface or Rayleigh wave interaction with an elastic wedge is one of the interesting and unsolved classical problems in the geophysics and acoustics area [1][2][3][4][5][6]. Rayleigh surface waves can propagate only along the stress-free boundary of a half-space, with their energy confined to the sub-surface and decaying exponentially along the outof-plane direction [7][8][9][10][11][12]. Rayleigh wave interaction with discontinuities can produce mode conversions which will result in the transmission, reflection and scattering of the incident energy.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation