Geology Reference
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u
(x,t) =
u
m
(x,t) +
u'
(x,t) (5.35)
p(x,t) = p
m
(x,t) + p'(x,t) (5.36)
We now assume, in an absolute value sense, that the (primed) disturbances
represent small deviations from mean conditions, that is,
m
(x,t) >> '(x,t) (5.37)
u
m
( x , t) >>
u'
(x,t) (5.38)
p
m
(x,t) >> p'(x,t) (5.39)
Substitution of Equations 5.37 to 5.39 in Equations 5.31 and 5.33, and
subsequent algebraic expansion, lead to a system of equations amenable to
simple limit processes.
Limit No. 1.
If the primed disturbances vanish identically, and
m
is
constant, the mean pressure p
m
and velocity
u
m
satisfy Equation 5.32, that is,
Bernoulli's equation.
Limit No. 2.
If the mean density
m
is constant, and the mean speed
u
m
vanishes, our acoustic disturbances satisfy
m
u'
t
= - p'
x
(5.40)
and
'
t
+
m
u
'
x
= 0 (5.41)
to leading order. To obtain Equations 5.40 and 5.41, formally small quadratic
quantities in the disturbances have been dropped. Let us now introduce the
“compressibility” defined by
' =
m
p'
(5.42)
We differentiate Equation 5.40 with respect to x, and Equation 5.41 with respect
to t, to find that
m
u'
tx
= - p'
xx
and '
tt
+
m
u'
xt
= 0. Then, using Equation 5.42,
we have the pressure equation
2
p'/ t
2
- (B/
m
)
2
p'/ x
2
= 0 (5.43)
where the “bulk modulus” B and the “fluid compressibility” are related by
B = 1/ (5.44)
As in the Lagrangian description, the speed of sound c satisfies c
2
= B /
m
.
Thus, Equation 5.43 takes the form
2
p'/ t
2
- c
2 2
p'/ x
2
= 0. We could have
eliminated pressure as the working variable and obtained the wave equation for
velocity
2
u'
/ t
2
- (B/
m
)
2
u'
/ x
2
= 0
(5.45)
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