Page 251 - Formation Damage during Improved Oil Recovery Fundamentals and Applications
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222                                                       Xingru Wu


          scale type at low temperatures. Anhydrate is the stable form of calcium

          sulfate scale at temperatures above 100 C. Hemihydrate scale formation

          occurs at temperatures between 100 Cand 120 C in brines with high

          ionic strength and in nonturbulent environments. Among these calcium
          sulfate scales, gypsum is more likely to form in the oil and gas reservoir
          conditions. Given right conditions, gypsum and anhydrate can transform
          from one to the other (Raju and Atkinson, 1990). As an example, the
          reaction of forming barium sulfate is as follows:
                                          22
                               Ba 11  1 SO -BaSO 4 k
                                          4
             Fig. 5.3 shows the solubility of different scales at different conditions.
          Given that barium sulfate has a very low solubility in brine and even in
          mineral acids such as hydrochloric acid, the near wellbore formation
          damage caused by sulfate scale precipitation cannot be effectively reme-
          diated without a well workover. Field experience indicates that well pro-
          ductivity can be severely impacted by sulfate scale in a matter of days or
          weeks if left untreated in sea waterflooded fields. The solubility of barium
          sulfate slightly increases with temperature and the presence of mineral
          salts such as NaCl.



          5.2.3 Other inorganic solids
          Other inorganic solids can also precipitate during scaling process. For
          example, usually the formation brines contain a low concentration of
          iron, but some iron scales such as iron oxides and, hydroxides, and sulfides
          can occur as a result of corrosion when dissolved gases such as CO 2 and
          H 2 S contribute to tubular corrosion, which leads to the formation of var-
          ious iron compounds. Some organic scales such as calcium napthenates
          may also be generated in some particular conditions. Some other inor-
          ganic solids include lead sulfide, zinc sulfide, and calcium fluoride.
             Some naturally occurring radioactive material (NORM) may also pre-
          cipitate in reservoirs or wells. For example, Low Specific Activity (LSA)
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          ( Ra) can be coprecipitated with BaSO 4 and CaSO 4 scale, and it emits
          alpha, beta, and gamma radiations. Therefore, if this type of scale are pro-
          duced in an open environment, special handling permits may be required
          from regulatory authorities to dispose of it, and it needs to be properly
          packed and shipped to registered recipient for proper disposal.
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