Up: J.E. Sonier's M.Sc. Thesis
Previous: Bibliography
The computer time allocated to calculating
of Eq. (3.9), is significant enough that it is
practical to avoid the large sum over reciprocal lattice vectors
for each iteration in the -minimization
procedure. Consequently, a Taylor series expansion around an initial
value of the magnetic penetration depth
was employed in the actual
fitting program:
so that,
is determined by expanding about the initial
point
.
In this way,
is calculated
by summing over the reciprocal lattice vectors
[in Eq. (3.9)], only once for an initial set of parameters
and ,
where
is the initial value of the
average field. It is not necessary to expand about .
This
is because changes in the average field merely shift the field distribution
along the field (or frequency) axis. In the fitting process, field shifts
in excess of a conservative value of
T were not permitted
before the program was stopped, the initial parameters changed, and the
data refitted.
Table A.1:
Accuracy of the Taylor series expansion used in the fitting program.
|
|
|
|
|
|
Error in |
Error in |
|
|
at the |
at the |
|
|
vortex core. |
saddle point. |
|
|
|
|
|
|
|
|
50 |
50 |
0.00 |
0.00 |
50 |
49 |
0.16 |
0.14 |
50 |
48 |
0.31 |
0.27 |
50 |
47 |
0.47 |
0.40 |
50 |
46 |
0.62 |
0.53 |
50 |
45 |
0.78 |
0.67 |
50 |
44 |
0.93 |
0.80 |
50 |
43 |
1.08 |
0.93 |
50 |
30 |
3.01 |
2.65 |
50 |
20 |
4.43 |
3.96 |
50 |
10 |
5.78 |
5.25 |
50 |
0 |
7.07 |
6.54 |
|
|
|
|
|
Table A.1
shows the accuracy of the Taylor series assuming an average magnetic
field 0.5T and
.
The error in using Eq. (A.1),
expressed as a percentage of
the exact calculation of
using
Eq. (3.9), is shown for
calculated at the
vortex core and at a saddle point. The results show that even
large changes in
give a good approximation for
.
In a typical fit,
is calculated in excess of 150,000times, so that using a Taylor series greatly diminishes the time required to
fit.
Up: J.E. Sonier's M.Sc. Thesis
Previous: Bibliography
Jess H. Brewer
2001-09-28