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BAKER HUGHES - Drilling Fluids Reference Manual

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HORIZONTAL AND EXTENDED REACH DRILLING<br />

to the selection of a suitable drilling fluid density being even more difficult. The extent and effect<br />

of Equivalent Circulating Density (ECD) needs careful consideration.<br />

No increase in mud weight with hole inclination is necessary across permeable formations such as<br />

sands. Formations with reasonable matrix permeability can be drilled with nominal overbalance,<br />

regardless of well trajectory or formation strength. Fracture gradient may decrease with increased<br />

inclination.<br />

In locally tectonically stressed areas, e.g. Colombia, the collapse gradient may exceed the fracture<br />

gradient, even in vertical wells. In this case one or both of lost circulation and hole collapse must<br />

be tolerated to some degree. Thus, there is a limitation that can be accomplished by fluid weight,<br />

and it is therefore imperative that the virgin strength and integrity of the rock be maintained as<br />

much as possible.<br />

Shale Interaction<br />

Interaction of the fluid with the formation which produces instability is primarily related to shale<br />

bodies. Shales, which include other classifications such as mudstones, siltstones, and claystones, all<br />

contain a relatively high percentage of hydratable and expandable clays. Typical mineral<br />

compositions of a young marine shale and an older indurated shale are shown in Table 11-1.<br />

It is the interaction of these clays with the water phase of the fluid that weakens the shale structure.<br />

The absorption of water by the shales through capillarity or diffusion causes instability by creating<br />

internal stress, weakening of cementing components of the shale, and lubricating micro-fractures<br />

that may exist.<br />

Classifications<br />

Shales can be classified into three broad categories:<br />

1. Soft, sticky shales<br />

2. Dispersive shales<br />

3. Hard, brittle shale<br />

Component<br />

Quartz<br />

Feldspar<br />

Calcite<br />

Dolomite<br />

Illite<br />

Mixed Layer<br />

Kaolinite<br />

Chlorite<br />

Typical Gumbo Shale, Gulf of<br />

Mexico, % Composition<br />

5 - 10<br />

Trace<br />

2 - 3<br />

2 - 3<br />

20 - 25<br />

50 - 55*<br />

5 - 10<br />

5 – 10<br />

* Mixed layer has 50% expandable layers<br />

** Mixed layer has 25% - 35% expandable layers<br />

Table 11 - 1 Shale Composition<br />

Vicksburg Formation, Starr<br />

County, Texas, % Composition<br />

10 - 15<br />

2 - 3<br />

10 - 15<br />

⎯<br />

25 - 30<br />

35 - 40**<br />

3 - 5<br />

5 - 10<br />

<strong>BAKER</strong> <strong>HUGHES</strong> DRILLING FLUIDS<br />

REFERENCE MANUAL<br />

REVISION 2006. 11-9

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