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Let's now assume the string is perfectly flexible (zero stiffness) so
that the direction of the force vector
is given by the unit
vector
tangent to the string. (To accommodate
stiffness, it would be necessary to include a force component at right
angles to the string which depends on the curvature and stiffness of
the string.) The magnitude of
at any position is the rest
tension
plus the incremental tension needed to stretch it the
fractional amount
If
is the constant cross-sectional area of the string, and
is the
Young's modulus (stress/strain--the ``spring constant''
for solids--see §B.5.1), then
so that
![$\displaystyle \mathbf{K}= \left[K+ SY\left(\frac{ds}{dx} - 1\right)\right]\frac{d{\bf s}}{ds}$](img3020.png) |
(B.35) |
where no geometrical limitations have yet been placed on the
magnitude of
and
, other than to prevent the
string from being stretched beyond its elastic limit.
The four equations (B.31) through (B.35) can be combined
into a single vector wave equation that expresses the
propagation of waves on the string having three displacement
components. This differential equation is nonlinear, so that
superposition no longer holds. Furthermore, the three
displacement components of the wave are coupled together at all
points along the string, so that the wave equation is no longer
separable into three independent 1D wave equations.
To obtain a linear, separable wave equation, it is necessary to assume
that the strains
,
, and
be
small compared with unity. This is the same assumption
(
) necessary to derive the
usual wave equation for transverse vibrations only in the
-
plane.
When (B.35) is expanded into a Taylor series in the strains
(see (B.33)), and when only the first-order terms are retained, we obtain
 |
(B.36) |
This is the linearized wave equation for the string, based only
on the assumptions of elasticity of the string, and strain magnitudes
much less than unity. Using this linearized equation for the force
, it is found that (B.31) separates into the three wave
equations
where
is the longitudinal wave velocity, and
is the transverse wave velocity.
In summary, the two transverse wave components and the longitudinal
component may be considered independent (i.e., ``superposition''
holds with respect to vibrations in these three dimensions of
vibration) provided powers higher than 1 of the strains (relative
displacement) can be neglected, i.e.,

and
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