Geology Reference
In-Depth Information
w
2
u/wt
2
- c
2
w
2
u/wx
2
= 0 (3.B.1)
c
2
= B/U (3.B.2)
p = - B wu/wx (3.B.3)
u(x,t) = X(x) e
i
Zt
(3.B.4)
d
2
X(x)/dx
2
+ Z
2
/c
2
X = 0 (3.B.5)
X
1
(x) =
A
sin Zx/c +
B
cos Zx/c (3.B.6)
X
2
(x) =
C
sin Zx/c +
D
cos Zx/c (3.B.7)
X
3
(x) =
E
exp (-iZx/c) (3.B.8)
Equations 3.B.6 and 3.B.7 allow standing waves to form in Sections 1 and
2, while Equation 3.B.8 for Section 3 states that u
3
=
E
e
i
Z(t - x/c)
which implies
that the wave is traveling to the right without reflection. This wave will
attenuate, but only at a distance far from the dimensions shown in Figure 3.B.1.
At x = L
c
, continuity of volume velocity (A
c
u
2
= A
p
u
3
) and of acoustic pressure
(wu
2
/wx = wu
3
/wx) require that
C
sin ZL
c
/c +
D
cos ZL
c
/c = (A
p
/A
c
)
E
exp (-iZL
c
/c)
(3.B.9)
C
cos ZL
c
/c -
D
sin ZL
c
/c = - i
E
exp (-iZL
c
/c)
(3.B.10)
At x = L
m
, continuity of displacement yields
A
sin ZL
m
/c +
B
cos ZL
m
/c =
C
sin ZL
m
/c +
D
cos ZL
m
/c
(3.B.11)
The pulser develops a pressure discontinuity at x = L
m
of the form
p
2
- p
1
= 'p = P
s
exp (iZt)
(3.B.12)
Since p = - B wu/wx, we have
A
cos ZL
m
/c -
B
sin ZL
m
/c -
C
cos ZL
m
/c +
D
sin ZL
m
/c = cP
s
/(ZB)
(3.B.13)
At the drillbit x = 0, the assumption of an open reflector, i.e.,
Case (e)
,
requires wu
1
/wx = 0 or
A
= 0, while the assumption of a solid reflector, that is,
Case (f)
, requires u
1
= 0 or
B
= 0, In either event, we have five equations for the
five complex unknowns
A
,
B
,
C
,
D
and
E
which can be solved exactly in closed
analytical form. Some algebra shows that
E
solid
= {(cP
s
)/(ZB)} sin ZL
m
/c exp (+iZL
c
/c) / {(A
p
/A
c
) cos ZL
c
/c + i sin ZL
c
/c}
(3.B.14)
E
open
= - {(cP
s
)/(ZB)} cos ZL
m
/c exp (+iZL
c
/c)/ {(A
p
/A
c
) sin ZL
c
/c - i cos ZL
c
/c}
(3.B.15)
Since p
3
(x,t) = - B wu
3
/wx = i(BZ/c)
E
e
i
Z(t - x/c)
, then
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