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BAKER HUGHES - Drilling Fluids Reference Manual

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Water Based <strong>Drilling</strong> <strong>Fluids</strong><br />

Inhibition Studies with Tertiary Clays<br />

Figure 3-16<br />

Inhibition Studies with Tertiary Clays<br />

Pore Pressure Transmission<br />

Baker Hughes <strong>Drilling</strong> <strong>Fluids</strong> has explored pore pressure transmission<br />

(PPT) testing for several years. PPT testing measures the formation pore<br />

pressure increase from filtrate invasion in very low permeability formations<br />

such as shales. In highly permeable formations the pressure rise from<br />

filtrate flow is rapidly dissipated in the formation volume and pore pressure<br />

is not affected. However, in very low permeability formations, the pressure<br />

increase from filtrate invasion declines very slowly and the pore pressure<br />

continues to increase with additional filtrate flow. This pore pressure<br />

increase reduces the effective over balance pressure. Over-balance pressure<br />

decline is exaggerated by wall fractures from drilling. These fractures<br />

increase near-wellbore permeability resulting in rapid pressure increase<br />

inside the wall. Reduced overbalance tends to destabilize the wellbore and<br />

promote sloughing. The introduction of cloud point glycols (AQUA-<br />

DRILL), aluminum complexes (ALPLEX) and sealing polymers<br />

(PERFORMAX) by Baker Hughes <strong>Drilling</strong> <strong>Fluids</strong> has greatly improved<br />

the osmotic effectiveness of water-based drilling fluids.<br />

Properly Pressured: Ideally, the hydrostatic pressure exerted by the mud<br />

column is higher than the formation (pore) pressure. Here, there is a<br />

pressure differential at the shale surface which serves as a support<br />

mechanism (first image) to offset over-burden pressure.<br />

Over Pressured: Here, drilling fluid pressure invasion (second image)<br />

occurs into the shale matrix. Due to the low permeability of the shale, the<br />

added pressure dissipates very slowly. In emulsion fluids, the capillary<br />

entry pressure effects strongly impede the invasion of pressure from base<br />

fluids (oils, esters or synthetics) because of the wetting characteristics of<br />

water vs. base fluids. However, in water-based muds, the capillary entry<br />

pressure can be very low and therefore water pressure invasion can easily<br />

occur in the matrix. As pressure invasion occurs, the pore pressure at the<br />

shale surface rapidly increases to a level equivalent to that of the mud<br />

column. Then, the differential pressure at the surface is reduced and<br />

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

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

3-72 Revised 2006

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