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BAKER HUGHES - Drilling Fluids Reference Manual

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Oil / Synthetic <strong>Fluids</strong><br />

As the concentration of ions increases, so does the concentration of water molecules tied up in<br />

hydration. As the concentration of water molecules tied up in hydration increases, the concentration of<br />

free water molecules (not involved in hydration) decreases. The availability of the water molecules in<br />

a solution to hydrate additional solutes can be quantified by the “activity” scale. All the water<br />

molecules in freshwater are available for hydration and the activity (Aw) is defined as “1”. As salt, or<br />

any substance that hydrates, is added, the concentration of hydrated ions or molecules increases and<br />

the availability of the brine molecules in the solution to hydrate any additional material decreases the<br />

activity (Aw).<br />

If two solutions of different Aw are poured together, diffusional mixing will result in a uniform Aw<br />

intermediately between the two. If two solutions of different Aw are separated by a semi-permeable<br />

membrane, an unusual situation occurs, as shown in Figure 5-15. A semi-permeable membrane is<br />

defined as a thin membrane which will allow water molecules to freely pass, but not salt ions.<br />

Water molecules in the solution of higher Aw will diffuse into the solution with lower Aw, as before,<br />

but not the ions. If the chamber with the solution of lower Aw is sealed, then the water diffusing<br />

through the membrane increases the pressure in the chamber. This is defined as osmotic pressure<br />

(Figure 5-15)<br />

Semi-permeable membranes are created between emulsified water droplets in water in oil emulsions<br />

and between emulsified water droplets and the formation drilled (see Figure 5-16). The layer of<br />

surfactant-rich oil will allow water molecules to pass, but not salt. Unless the Aw values are equal, an<br />

osmotic imbalance, or potential, will exist and water will migrate.<br />

As the concentration of salt in the aqueous phase increases and the Aw decreases, less water is<br />

available to solubilize and hydrate other materials. Lime, for example, is less soluble in CaCl 2<br />

solutions than in water.<br />

Figure 5-15<br />

Osmosis<br />

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

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

5-20 Revised 2006

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