BAKER HUGHES - Drilling Fluids Reference Manual
PRESSURE PREDICTION AND CONTROL Pressure Gradient in Equivalent Fluid Weight (lb m /gal) 10.0 10.5 11.0 11.5 12.0 12.5 13.0 13.5 14.0 14.5 15.0 15.5 16.0 17.0 17.5 MIOCENE- OLIGOCENE South Louisiana 1.09 1.15 1.20 1.28 1.34 1.43 1.53 1.65 1.78 1.93 2.10 2.33 2.60 3.58 5.00 Ratio: Observed Conductivity / Normal Conductivity Or: Normal Resistivity / Observed Resistivity FRIO FORMATION S. Texas Gulf Coast 1.34 1.55 1.78 1.97 2.18 2.43 2.68 2.96 3.33 3.60 3.95 4.31 4.67 5.72 WIL COX FORMATION S. Texas Gulf Coast NORTH SEA .08 .13 1.22 1.28 1.39 1.50 1.64 1.80 2.00 2.21 2.44 2.71 3.03 4.0 1.50 1.76 1.95 2.30 2.60 2.90 3.25 3.60 3.85 4.2 SOUTH CHINA SEA 1.32 1.50 1.65 1.80 2.00 2.20 2.45 2.65 2.85 3.1 4.5 3.30 3.54 3.70 NOTE: Plot conductivity values for shale on 3-cycle semi-log paper. Table 12 - 1 Predicted Pressure Gradients vs. Conductivity or Resistivity Ratios Example Figure 12-4 shows an example of an IES log. From the plot in Figure 12-5, it can be easily seen that a marked trend of normal pressure zone is obtained until a depth of approximately 11,000 feet. At this point, the sharp change indicates that an abnormal pressure zone has been encountered. Figure 12-5 shows the conductivity plot versus depth for the log in Figure 12-4. Sample calculations from Figure 12-5: • For abnormal pressure zone at 13,000 feet, • Shale conductivity observed = 1670 • Shale conductivity normal = 630 Calculate the ratio of observed conductivity to normal conductivity: If the formation were of Miocene-Oligocene geologic age, Table 12-1 indicates a formation pressure equivalent to approximately 16.1 lb m /gal drilling fluid density. Sonic Logs Sonic log data is used in a manner similar to the conductivity method of pressure prediction. Sonic logs measure transit time of sound for fixed distance through formations (the same as the seismic information). Interval transit time (microseconds per foot) decreases as formation BAKER HUGHES DRILLING FLUIDS REFERENCE MANUAL REVISION 2006 12-7
PRESSURE PREDICTION AND CONTROL porosity decreases because a denser material transmits sound waves at a higher velocity than a less dense material. Porosity generally decreases at a near linear rate as a function of depth in normally near a straight line with gradual reduction in travel time as a function of depth. Increased shale porosity (which usually indicates a change in compaction and abnormal pressures) would produce an increase in shale travel time. Figure 12-6 is a plot of shale transit time versus depth. Note the normal compaction trend indicating normal formation pressures down to approximately 11,000 feet. Below this depth, shale travel time values begin to increase in relation to extrapolated normal compaction line, indicating abnormal formation pressures. Figure 12 - 6 Shale Transit Time vs. Depth BAKER HUGHES DRILLING FLUIDS REFERENCE MANUAL REVISION 2006 12-8
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PRESSURE PREDICTION AND CONTROL<br />
Pressure<br />
Gradient<br />
in Equivalent<br />
Fluid Weight<br />
(lb m /gal)<br />
10.0<br />
10.5<br />
11.0<br />
11.5<br />
12.0<br />
12.5<br />
13.0<br />
13.5<br />
14.0<br />
14.5<br />
15.0<br />
15.5<br />
16.0<br />
17.0<br />
17.5<br />
MIOCENE-<br />
OLIGOCENE<br />
South Louisiana<br />
1.09<br />
1.15<br />
1.20<br />
1.28<br />
1.34<br />
1.43<br />
1.53<br />
1.65<br />
1.78<br />
1.93<br />
2.10<br />
2.33<br />
2.60<br />
3.58<br />
5.00<br />
Ratio: Observed Conductivity / Normal Conductivity<br />
Or: Normal Resistivity / Observed Resistivity<br />
FRIO<br />
FORMATION<br />
S. Texas Gulf Coast<br />
1.34<br />
1.55<br />
1.78<br />
1.97<br />
2.18<br />
2.43<br />
2.68<br />
2.96<br />
3.33<br />
3.60<br />
3.95<br />
4.31<br />
4.67<br />
5.72<br />
WIL COX<br />
FORMATION<br />
S. Texas Gulf Coast NORTH SEA<br />
.08<br />
.13<br />
1.22<br />
1.28<br />
1.39<br />
1.50<br />
1.64<br />
1.80<br />
2.00<br />
2.21<br />
2.44<br />
2.71<br />
3.03<br />
4.0<br />
1.50<br />
1.76<br />
1.95<br />
2.30<br />
2.60<br />
2.90<br />
3.25<br />
3.60<br />
3.85<br />
4.2<br />
SOUTH<br />
CHINA SEA<br />
1.32<br />
1.50<br />
1.65<br />
1.80<br />
2.00<br />
2.20<br />
2.45<br />
2.65<br />
2.85<br />
3.1<br />
4.5 3.30<br />
3.54<br />
3.70<br />
NOTE: Plot conductivity values for shale on 3-cycle semi-log paper.<br />
Table 12 - 1 Predicted Pressure Gradients vs. Conductivity or Resistivity Ratios<br />
Example<br />
Figure 12-4 shows an example of an IES log. From the plot in Figure 12-5, it can be easily seen<br />
that a marked trend of normal pressure zone is obtained until a depth of approximately 11,000<br />
feet. At this point, the sharp change indicates that an abnormal pressure zone has been<br />
encountered. Figure 12-5 shows the conductivity plot versus depth for the log in Figure 12-4.<br />
Sample calculations from Figure 12-5:<br />
• For abnormal pressure zone at 13,000 feet,<br />
• Shale conductivity observed = 1670<br />
• Shale conductivity normal = 630<br />
Calculate the ratio of observed conductivity to normal conductivity:<br />
If the formation were of Miocene-Oligocene geologic age, Table 12-1 indicates a formation<br />
pressure equivalent to approximately 16.1 lb m /gal drilling fluid density.<br />
Sonic Logs<br />
Sonic log data is used in a manner similar to the conductivity method of pressure prediction.<br />
Sonic logs measure transit time of sound for fixed distance through formations (the same as the<br />
seismic information). Interval transit time (microseconds per foot) decreases as formation<br />
<strong>BAKER</strong> <strong>HUGHES</strong> DRILLING FLUIDS<br />
REFERENCE MANUAL<br />
REVISION 2006 12-7