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BAKER HUGHES - Drilling Fluids Reference Manual

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

Oven testing of a fluid can be done at the wellsite and, on many wells, is considered standard<br />

operating procedure. Timely test results are the key for making quicker adjustments to the fluid.<br />

MIL-TEMP ® (or ALL-TEMP ® ) has been found to be an excellent product in cement<br />

contaminated drilling fluids to decrease the gel strength and high-temperature gelation properties.<br />

Generally, about 1 to 3 lb m /bbl of MIL-TEMP ® can correct the flow properties of a cement<br />

contaminated system. MIL-TEMP is a higher temperature application product and generally is<br />

not used for temperatures lower than 250°F to 300°F.<br />

Anhydrite-Gypsum Contamination<br />

Anhydrite and gypsum, both calcium sulfate compounds (CaSO 4 ), are sometimes encountered<br />

while drilling. Gypsum is calcium sulfate with water of crystallization (CaSO 4 +2H 2 0), while<br />

anhydrite is the anhydrous form of calcium sulfate (without water). Anhydrite may occur as thin<br />

stringers. In some areas, it occurs as massive beds ranging from 100 to 800+ feet thick. Anhydrite<br />

has also been associated with salt (stringers, inclusions, overhang, massive salt, etc.) and could<br />

signal potential salt contamination.<br />

Anhydrite contamination contributes calcium ions, which could result in flocculation. Unlike<br />

cement anhydrite does not cause a pH increase since it supplies a sulfate radical in lieu of an<br />

hydroxyl radical. The sulfate radical contributes to flocculation of clay solids only marginally.<br />

In lightly treated fluids, small amounts of anhydrite increase the rheological properties of a fluid.<br />

The severity of change depends to a great degree on the bentonite content and solids particle size<br />

distribution. When anhydrite goes into solution and soluble calcium increases above 200 mg/L,<br />

viscosity may fluctuate noticeably and fluid loss could become more difficult to control. As<br />

anhydrite concentrations increase toward a maximum solubility of approximately 600 mg/L Ca ++ ,<br />

a Base Exchange or change in bentonite characteristics occurs. Flow properties tend to decrease,<br />

and fluid loss becomes difficult to control. Conversion to a gypsum-based fluid has occurred. If a<br />

gypsum fluid is acceptable, then treatments should be made specifically for a gypsum fluid.<br />

When anhydrite contamination occurs, there are several methods for handling it. The drilling<br />

fluid can be maintained as a low-calcium fluid by chemically precipitating most of the calcium<br />

from solution, or it can be converted to a gypsum-type system. For smaller amounts of anhydrite<br />

contamination, chemical removal of calcium is best achieved by adding soda ash. Approximately<br />

0.093 lb m /bbl of soda ash is required to precipitate 100 mg/L of Ca ++ ion, but caution should be<br />

exercised to avoid over-treatment. When Ca ++ ions are reduced to 100 to 150 mg/L, consider<br />

stopping soda ash treatment. The reaction between anhydrite and soda ash is as follows.<br />

CaSO 4 + Na 2 CO 3 → CaCO 3 ↓ + Na 2 SO 4<br />

Remember, pilot testing should support treatment specific to anhydrite contamination.<br />

Soluble sodium sulfate is formed from this reaction and could cause flocculation problems with<br />

prolonged treatments. For this reason, it is sometimes necessary to convert to a gypsum-base fluid<br />

when massive anhydrite is to be drilled with a freshwater system. Over treatment with soda ash<br />

can also cause a carbonate problem.<br />

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

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

Revised 2006 4-5

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