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BAKER HUGHES - Drilling Fluids Reference Manual

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Hydraulics<br />

term “viscosity” is confused with the term “rheology”. A more detailed analysis of the term<br />

“rheology” follows.<br />

Rheology<br />

Rheology is defined as physics of the flow and the deformation of matter. Rheology and the<br />

associated annular hydraulics (Chapter 9) relate directly to borehole stability and how effectively the<br />

borehole is cleaned. An understanding of rheology is essential if wellsite engineering of the drilling<br />

fluid is to cost effectively complement the objective of drilling the well. Rheology and hydraulics of<br />

drilling fluids are not exact sciences, but are based upon mathematical models that closely describe<br />

the rheology and hydraulics of the fluid and do not conform exactly to any of the models.<br />

Consequently, different methods are used to calculate rheology and hydraulic parameters.<br />

Fluid Deformation<br />

Rheology is the study of the deformation of all forms of matter. The deformation of a fluid can<br />

simply be described by two parallel plates separated by some distance as shown in Figure 1-1.<br />

Figure 1-1<br />

Deformation of a Fluid by Simple Shear<br />

Shear Stress<br />

An applied force (F), acting over an area (A), causes the layers to slide past one another. However,<br />

there is a resistance, or frictional drag, force that opposes the movement of these plates. This<br />

resistance or drag force is called shear stress ( τ ). In equation form,<br />

τ<br />

=<br />

F<br />

-----<br />

A<br />

with shear stress having typical units of lb f /100 ft 2 .<br />

Additionally, the fluid layers move past each other easier than between a pipe wall and fluid layer.<br />

Therefore, we can consider a very thin layer of fluid next to the pipe wall as stationary.<br />

Shear Rate<br />

The difference in the velocities between two layers of fluid divided by the distance between the two<br />

layers is called the shear rate ( γ ). In equation form,<br />

γ<br />

velocity difference<br />

= -----------------------------------------------<br />

distan<br />

ce<br />

With typical units of<br />

or, reciprocal seconds.<br />

ft/sec 1<br />

------------ = ------ =<br />

ft sec<br />

se c 1<br />

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

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

1-6 Revised 2006

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