Geoscience Reference
In-Depth Information
Substituting these expressions into (5.35) yields
1
Σ
P
Λ
n
nπ
1
Σ
P
Σ
P
→∞
δ
n
≈−
+
at
(5.36)
and
nπ
Σ
P
+
Σ
P
at
Λ
n
Σ
P
→
δ
n
≈−
0
.
(5.37)
Comparing (5.36) and (5.37) with (5.24) and (5.25) we get a relationship of
the half-width
δ
n
with decrement
γ
n
:
d
ω
An
d
x
−
1
x
=
x
n
γ
n
ω
An
Λ
n
=
γ
n
δ
n
≈−
.
(5.38)
We obtained (5.38) using the explicit expressions for
γ
n
and
δ
n
.Moreover,
these formulae can be applied in a rather wider field than could been assumed
when deriving them. Let us present other approach independent on the form
of the explicit solution.
Curved Field-Line
Let us consider field-lines that are not obligatory straight. Let their position
be determined by one coordinate of a curvilinear coordinate system. Gener-
ally, a complex resonant frequency
ω
n
(
x
) corresponds to each field-line. These
frequencies are found from the dispersion equation
∆
(
ω, x
)=0(seeChap-
ter 6). The latter, as in the case considered above, can be continued to the
complex plane
w
=
x
+
iu
. Then, assuming low dissipation, we first find the
resonance point
x
n
(
ω
) at a given frequency
ω
, and then determine the real
function
ω
A
(
x
). For a weak dissipation, we have
w
n
(
ω
)=
x
n
(
ω
)+
iδ
n
(
ω
)
,
where
ω
is real and
ω
n
(
x
)=
ω
An
(
x
)
−
iγ
n
(
x
)
.
Functions
δ
n
(
ω
)and
γ
n
(
x
) are small. Expanding
∆
by
δ
n
at a fixed
x,
we
have
∆
(
ω
A
,x
n
)
∂∆
(
ω
An
,x
n
)
/∂x
,
δ
n
=
i
and expanding by
γ
n
∆
(
ω
An
,x
n
)
∂∆
(
ω
An
,x
n
)
/∂ω
.
γ
n
=
−
i
Search WWH ::
Custom Search