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BAKER HUGHES - Drilling Fluids Reference Manual

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Baker Hughes <strong>Drilling</strong> <strong>Fluids</strong><br />

pressure support (over-balance) is lost.<br />

Pressure Invasion: Finally, loss of differential pressure support at the wellbore surface allows<br />

the over-burden pressure (weight of shale pressing down) to destabilize the invaded shale and it<br />

will slough off (third image) into the annulus. In this case, the pressure of the mud column is<br />

equal to the pressure within the shale, leaving no supporting pressure to prevent the overburden<br />

force from sloughing the shale.<br />

Capillary Effects<br />

Neither water-base fluids nor oil-base fluids form a solid filter cake in shale. Under normal fluid<br />

pressures, shales are permeable to water-base fluids but almost impermeable to oil. The stable<br />

behavior of shales while drilling with oil-base fluid or synthetic-base fluids is a result of capillary<br />

action. When oil enters a shale, it has to overcome a threshold pressure caused by the capillary<br />

effect between oil and the pore fluid. The capillary pressure is in the order of thousands of psi and<br />

is generally too large to be overcome by the fluid pressure differential. The threshold pressure,<br />

therefore, acts as an alternative semi-permeable membrane and provides effective fluid support to<br />

the wellbore.<br />

Oil/ Synthetic Based mud<br />

Water Based Mud<br />

Wellbore<br />

pressure<br />

Wellbore<br />

pressure<br />

Water<br />

Pore pressure<br />

Water<br />

Water<br />

Pore pressure<br />

Figure 3-17<br />

Capillary Action in Oil/Synthetic vs. Water Base <strong>Fluids</strong><br />

As a consequence, shale instability with oil and synthetic drilling fluids is normally caused by<br />

lack of fluid support, i.e., too low of a fluid density.<br />

Cloud Point Behavior<br />

Definition<br />

Cloud point is a phenomenon exhibited by many glycols. The solubility of these glycols in water<br />

decreases as temperature increases, with materials that are fully soluble at room temperature<br />

forming separate phases at higher temperatures. The temperature at which the glycol and water<br />

separate is known as cloud point, since the previously clear solution becomes “cloudy” upon<br />

separation as shown in Figure 3-17 Capillary Action in Oil/Synthetic vs. Water Base <strong>Fluids</strong><br />

Baker Hughes <strong>Drilling</strong> <strong>Fluids</strong><br />

<strong>Reference</strong> <strong>Manual</strong><br />

Revised 2006 3-73

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