330
Advanced
Bowout
and
Well
Control
Several directional surveys were available at the
TXO
Marshall.
Unfortunately, there were serious discrepancies among them.
As
illustrated in Figure 7.7,
two
north-seeking
gyro
surveys (3-21 and 3-26)
and
a
magnetic single-shot were tied together at 11,800 feet and plotted.
The
two
gyro
surveys, which represent the state of the art
as
of
this
writing, were very discordant with one another even though they were run
with the SAME TOOL, by the
SAME
OPERATOR
and using the
SAME
WIRELINE. After only 650 feet MD of surveying from 11,800 feet
to
12,450 feet, the north-seeking
gyros
disagreed by 7 feet for an overall
reliability of only 11 feet per 1,000 feet. Further, the 3-21 gyro survey
disagreed with the single-shot
data
by 10 feet in the 650 feet for an overall
reliability of 15.7 feet per 1,000 feet. The deviation in this portion
of
the
hole varied between 10 and 14 degrees. These values for reliability and
repeatability are far worse
than
those normally quoted within the industry.
Survey
data
were
also
available from other portions of the
Marshall for comparison.
In
the upper part of the hole between 10,650
feet and 11,500 feet, there were four sets of survey
data:
a magnetic
single-shot, a magnetic multi-shot (1-17), and the
two
north-seeking
gyros
(3-2 1 and 3-26). These data were plotted together at 10,650 feet and their
deviations are illustrated
as
Figure 7.8. Analysis of Figure 7.8 indicates
similar systematic relationships between the
two
gyro
runs
and the
magnetic single-shot
data.
The magnetic multi-shot results
seem
to
support the 3-21
gyro
data.
The
maximum
discrepancy is between the
magnetic single-shot and the 3-26
gyro.
As
illustrated, these
two
surveys
disagree by approximately 9 feet over the 850-foot interval for an overall
reliability of 10.6 feet per 1,000 feet.
In
some instances, magnetic
data
compared better
than
the more
expensive north-seeking
gyro
data.
For example, the 1-1 7 magnetic multi-
shot and the magnetic single-shot
data
were compared
in
the interval
between 11,400 feet and 12,300 feet (see Figure 7.9).
A
5-foot
uncertainty is indicated over the 863-foot
interval
for
a
reliability of 5.8
feet per 1,000 feet.
Several other comparisons were made and are presented in
reference 9. Careful study of the survey data obtained
in
this instance
makes it difficult
to
ascribe a survey precision of better
than
10 feet of
lateral movement per 1,000 feet of survey. Further, since the survey
errors were primarily systematic, there
was
no reason
to
prefer the more