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BAKER HUGHES - Drilling Fluids Reference Manual

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Formation Mechanics<br />

Chapter 2<br />

Successful drilling requires knowledge of the formation type into which the borehole<br />

is drilled. The characteristics of that formation, i.e., geological composition, liquid or<br />

gas content, pressure, permeability, porosity, reactivity, hydration, etc. will help<br />

determine the type of fluid to be used in drilling and completing the wellbore.<br />

Clay and Clay Minerals<br />

The importance of clay and clay minerals in the drilling industry is evident from two viewpoints:<br />

• Commercially mined clays are added to drilling fluids to build viscosity, thixotropy, and to<br />

contribute to wall building properties.<br />

• Clay minerals are present in nearly all sedimentary rocks.<br />

• Clay reaction to the drilling process can produce major problems such as,<br />

• Hole enlargement<br />

• Sloughing<br />

• Hydration<br />

• Rheological problems.<br />

The magnitude of the potential problems is apparent when one realizes that more than half of<br />

sedimentary rocks are composed of shales, siltstones, mudstones, etc. These rock types are composed<br />

of more than 50% clay minerals. Even sandstones may have as much as 20% to 30% clay minerals.<br />

The better understanding one has of clays and clay minerals, the greater the control over problems that<br />

may develop in the drilling process.<br />

Definitions / Terminology<br />

Clays can be defined according to physical properties, chemical properties, size, structure, and<br />

reactivity in water. One definition cannot adequately describe all types of clays. A simple definition<br />

used by many people is that clay is a finely ground, earthy material that can be molded into shapes<br />

when wet.<br />

Geologists and mineralogists usually define clays according to the chemical and mineral content that<br />

make up the clay. Elements that commonly make up clays are oxygen, silicon, aluminum, calcium,<br />

magnesium and potassium. Non-clay minerals generally found are quartz, feldspar, pyrite, and calcite.<br />

Clays are also defined according to their size. The American Petroleum Institute (API) defines clays<br />

as being those particles that are two microns or less in size. A micron is equal to one millionth of a<br />

meter. In order to grasp the concept of this size, it is sometimes easier if the sizes are scaled up a<br />

million-fold. For example:<br />

• A million yard sticks end to end would stretch from Houston to El Paso<br />

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

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

Revised 2006 2-1

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