Introduction
what is a guided wave dispersion and its
corresponding dispersion curve? Guided waves are ultrasonic waves that
propagate differently than the more commonly used longitudinal and shear
waves. They are similar to rayleigh and lamb waves in that they propagate
at the surface or in thin materials. Their velocity is not only dependent
on the material (like longitudinal, shear and surface waves) but also
the thickness of the material and frequency. Dispersion curves are used
to describe and predict the relationship between frequency, phase velocity
and group velocity, mode and thickness. Fundamental to the understanding
of guided wave analysis in NDT is the generation or utilization of phase
velocity, group velocity and attenuation dispersion curves. How do we
use the curves and where do they come from?
Governing Equations
All engineering problems have associated with them a governing equation.
In the case of wave propagation, the governing equation is Navier's
equation. It is a second order linear partial differential equation
for which we'd like to obtain a solution subject to certain boundary
conditions. In trying to solve the second order partial differential
equation, a variety of different techniques could be used. If we propose
a particular solution, let's say for the longitudinal displacement component
and lateral displacement component a harmonic solution (oscillating
sinusoidal functions of time), we can substitute this into the governing
equations to see what happens.
Wave
propagation possibilities must come from points on the dispersion
curves and not points in between.
We find that we do indeed satisfy the governing
equation through this solution and the challenge really becomes one
of satisfying the boundary conditions. As an example, in a stress free
plate or tubular structure, we have to make sure that the stress components
on the outside surface are zero. The boundary conditions utilize stress,
strain and displacement and equations from the theory of elasticity.
Once we have the relationships between stress, strain and displacement
and a corresponding constitutive equation, in most cases considered
as a generalized form of Hooke's law, we can now make an attempt to
satisfy the boundary conditions. In our initially assumed harmonic solution
there will be unknown coefficients. The coefficients are obtained by
satisfying the boundary conditions.
Dispersion curves
With our assumed harmonic solution and an attempt to satisfy the boundary
conditions, we end up with a system of homogeneous equations. In order
to find a nontrivial solution, the system of homogeneous equations must
have the determinant of the coefficient matrix set equal to zero. In
extracting the roots, we end up with solutions for phase velocity versus
frequency or versus frequency times thickness because of the scale factor
of wavelength to thickness. These values are plotted on an engineering
dispersion curve, so named because the velocity changes with frequency
and the pulses tend to become stretched or dispersed as they propagate.
Phase Velocity Dispersion Curves
A typical phase velocity dispersion curve for lamb waves taken from
Rose (1999) is illustrated in Figure 1a. A lot of information is presented
in the dispersion curve: cp is phase velocity, f is frequency,
d is thickness of the plate, cR
is the rayleigh surface wave velocity, cT
is the shear wave velocity and cplate
is the plate velocity. As the fd number
increases, all the modes approach the rayleigh wave velocity. The waves
formed by throwing a stone into water can help explain the difference
between phase and group velocity. The velocity of a particular wave
in the packet of waves that are propagating is the phase velocity and
the group velocity is the packet velocity. Dispersion curves can be
generated for all types of structures including plates, rods, tubes,
multilayer structures, rails or any wave guide, whether isotropic or
anisotropic.

Figure 1 - Dispersion curves for a traction
free aluminum plate (the classic lamb wave problem): (a) phase velocity
dispersion curves; (b) group velocity dispersion curves.
In extracting the roots from the determinant, either
analytically or through a numerical solution technique, we end up with
possible wave propagation possibilities or wave resonances that might
occur in the structure. Wave propagation possibilities must come from
points on the dispersion curves and not points in between. The curves
are for an infinite plane wave excitation which is modified somewhat
for a finite sized transducer. We have to try to select a good phase
velocity and frequency to carry out a test. The phase velocity can be
evaluated by using, as an example, an angle beam entry into a structure.
As we know, for oblique incidence into a structure, the governing equation
is Snell's law. Snell's law can be used in this case to calculate the
corresponding phase velocity and incident angle into the structure in
producing the desired guided wave mode and frequency.
A comb type transducer could also be used to generate
guided waves by using linear shaped crystals or elements that are spaced
evenly apart (Rose et al., 1998). The modes or the curves are labeled
for convenience as S0, S1, S2 and so on. S0, S1, S2 and S3 are the symmetric
modes. A0, A1 and A2 are the antisymmetric modes. The reason for this
naming is associated with the vibrational character of the structure.
The symmetric modes have associated with them a compressional rarefaction
expansion of the plate or tube in which the waves propagate. The antisymmetric
nature is associated with flexural mode propagation as the wave travels
through the structure. More details can be found in Rose (1999).
Group Velocity Dispersion Curves
Shown in Figure 1b, to accompany the phase velocity dispersion curve,
is a group velocity dispersion curve. The phase velocity dispersion
curve contains values associated with the extraction of roots from the
determinant discussed earlier. However, when we take a group of waves
traveling in a structure at approximately the same frequency, that particular
wave packet travels with the group velocity. The group velocity can
be much different than the phase velocity and changes drastically as
we move along each mode as frequency is swept. It is this group velocity
that we measure in a laboratory in order to carry out location analysis
for a particular discontinuity. The group velocity is derived from the
phase velocity curve, being related to the phase velocity values and
slopes on the phase velocity dispersion curve. More information on this
subject can be found in Rose (1999). When complex roots are extracted
from the determinant referred to earlier, attenuation dispersion curves
are often generated (Rose, 1999).
Guided Wave Testing
Any of the points on the dispersion curves could be used to carry out
an ultrasonic guided wave test. Some points, however, are much better
than others for improved reception, sensitivity and penetration power.
One of the key variables associated with how good a particular point
might be is related to the wave structure, that is the wave displacement
characteristics across the thickness of the structure. We could think
of the displacement characteristics as in plane or out of plane, sometimes
referred to as the u and w displacements, with u
directed along the plate in the wave propagation direction and w
normal to the plate. The wave structure changes for every point on each
particular mode on a dispersion curve as the frequency is swept.
In looking at lamb wave propagation, a sample result
is illustrated in Figure 2, where the in plane and out of plane displacement
component is plotted across the thickness of the structure versus frequency
(or actually the frequency times thickness product ranging from 0.5
up to 3). For lower frequencies, it is easy to see that there is a dominant
in plane displacement characteristic across the thickness, particularly
noted on the outside surfaces. As the frequency increases, however,
the variations become considerable to a point where for a frequency
times thickness product of 2, the in plane displacement component is
almost 0 on the outside surface of the structure. At this point, there
is a dominant out of plane displacement characteristic and the waves
would tend to propagate or leak into water, if present, and quickly
attenuate the waves in the plate. The combination of in plane and out
of plane displacement components leads to variations in energy and stress.
The sensitivity to certain kinds of discontinuities depends on the wave
structure, for example, whether the discontinuity is on the outside
surface, in the center portion and so on.

Figure 2 - A wave structure for various points
on the S0 mode of an aluminum plate, showing the in plane (u,
solid line) and out of plane (w, dashed line) displacement profiles
across the thickness of the plate: (a) fd = 0.5; (b) fd
= 1; (c) fd = 1.5; (d) fd = 2; (e) fd = 2.5;
(f) fd = 3.
We have to select wave structures that have sufficient
amounts of energy and displacement with respect to in or out of plane
impingement onto a particular discontinuity. A great deal of work is
being carried out to find out which of the variables are key with respect
to improved sensitivity to certain kinds of discontinuities and also
to overall improved penetration power in a structure. Penetration power
is particularly important when we consider a multilayer structure or
something that is water or fluid loaded.
A sample shear horizontal phase velocity dispersion
curve is illustrated in Figure 3. We notice that the curves are simplified
somewhat when compared to the lamb wave type dispersion curves; there
are fewer modes involved and hence some simplicity with respect to the
wave propagation in the structure because of less mode conversion potential.
Also, it turns out that for the shear horizontal case, the wave structure
is uniform over the entire mode for all frequencies.

Figure 3 - Shear horizontal mode phase velocity
dispersion curves for an aluminum layer, cT = 3.1
mm/µs (0.1 in./µs): solid curves denote symmetric modes
and dashed curves denote antisymmetric modes.
Acknowledgments
Thanks are given to Jack Spanner, Jr., of the Electric Power Research
Institute, Charlotte, North Carolina, for discussions on this article.
References
Rose, J.L., Ultrasonic Waves in Solid Media, Cambridge, Cambridge
University Press, 1999.
Rose J.L., S.P. Pelts and M.J. Quarry, "A Comb Transducer
Model for Guided Wave NDE," Ultrasonics, Vol. 36, 1998, pp.
163-169.
* Ultrasonic
Laboratory, Department of Engineering Science and Mechanics, Pennsylvania
State University, 212 Earth and Engineering Science Building, University
Park, PA 16802; (814) 863-8026; fax (814) 863-8164; e-mail <jlresm@engr.psu.edu>.
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by the American Society for Nondestructive Testing, Inc. All rights
reserved.