
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