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               16/248  PRODUCTION ENHANCEMENT
               where                                     The designed acid volume and injection rate should be
                                                         adjusted based on the real-time monitoring of pressure
                 g a ¼ acid specific gravity, water ¼ 1:0  during the treatment.
                 g m ¼ mineral specific gravity, water ¼ 1:0.
               Based on the volumetric model, the required acid volume
               per unit thickness of formation can be estimated using the  Summary
               following equation:                       This chapter briefly presents chemistry of matrix acidizing
                                                         and a guideline to acidizing design for both sandstone and
                      2
                          2
               V h ¼ pf r wh    r ð PVÞ ,         (16:11)  carbonate formations. More in-depth materials can be
                               bt
                          w
               where (PV) bt is the number of pore volumes of acid  found in McLeod (1984), Economides et al. (1994), and
               injected at the time of wormhole breakthrough at the end  Economides and Nolte (2000).
               of the core. Apparently, the volumetric model requires
               data from laboratory tests.
                                                         References
               Example Problem 16.3 A 28 wt% HCl is needed to  daccord, g., touboul, e., and lenormand, r. Carbonate
               propagate wormholes 3 ft from a 0.328-ft radius wellbore  acidizing: toward a quantitative model of the worm-
               in a limestone formation (specific gravity 2.71) with a  holing phenomenon. SPEPE Feb. 1989:63–68.
               porosity of 0.15. The designed injection rate is 0.1 bbl/  da motta, e.p. Matrix Acidizing of Horizontal Wells,
                                            2
               min-ft, the diffusion coefficient is 10  9  m =sec, and the
                                          3
               density of the 28% HCl is 1:14 g=cm . In linear core  Ph.d. Dissertation. Austin: University of Texas at
               floods, 1.5 pore volume is needed for wormhole  Austin, 1993.
               breakthrough at the end of the core. Calculate the acid  economides, m.j., hill, a.d., and ehlig-economides, c.
               volume requirement using (a) Daccord’s model and (b) the  Petroleum Production Systems. Englewood Cliffs, NJ:
               volumetric model.                           Prentice Hall, 1994.
                                                         economides, m.j. and nolte, k.g. Reservoir Stimulation,
                                                           3rd edition. New York: John Wiley & Sons, 2000.
               Solution
                                                         fogler, h.s., lund, k., and mccune, c.c. Predicting the
                                                           flow and reaction of HCl/HF mixtures in porous
               (a) Daccord’s model:                        sandstone cores. SPEJ Oct. 1976, Trans. AIME,
                                                           1976;234:248–260.
                        y m MW m    (1)(100:1)           hekim, y., fogler, h.s., and mccune, c.c. The radial
                  b ¼ C a     ¼ (0:28)
                        y a MW a    (2)(36:5)              movement of permeability fronts and multiple reaction
                    ¼ 0:3836 lb m CaCO 3 =lb m 28 wt% HCl solution:  zones in porous media. SPEJ Feb. 1982:99–107.
                              (0:15)(0:3836)(1:14)       hill, a.d. and galloway, p.j. Laboratory and theoretical
                       fbg a
                 N Ac ¼      ¼              ¼ 0:0285       modeling of diverting agent behavior. JPT June
                      (1   f)g m  (1   0:15)(2:71)
                                           3
                  q h ¼ 0:1 bbl= min -ft ¼ 8:69   10  4  m =sec-m  1984:1157–1163.
                                                         hill, a.d., lindsay, d.m., silberberg, i.h., and schechter,
                 r wh ¼ 0:328 þ 3 ¼ 3:328 ft ¼ 1:01 m
                                                           r.s. Theoretical and experimental studies of sandstone
                           q
                             r
                      pfD 2=3 1=3 d f                      acidizing. SPEJ Feb. 1981;21:30–42.
                  V h ¼    h  wh                         hoefner, m.l. and fogler, h.s. Pore evolution and channel
                         bN Ac
                                        4 1=3
                              9 2=3
                      p(0:15)(10 )  (8:69   10 )  (1:01) 1:6  formation during flow and reaction in porous media.
                    ¼                                      AIChE J. Jan. 1988;34:45–54.
                                   5
                            (1:5   10 )(0:0285)          lund, k., fogler, h.s., and mccune, c.c. Acidization I: the
                           3
                    ¼ 0:107 m =m ¼ 8:6 gal=ft              dissolution of dolomite in hydrochloric acid. Chem.
                                                           Eng. Sci. 1973;28:691.
               (b) Volumetric model:
                                                         lund, k., fogler, h.s., mccune, c.c., and ault, j.w.

                                  2
                       V h ¼ pf r  2    r ð PVÞ            Acidization II: the dissolution of calcite in hydro-
                              wh  w    bt                  chloric acid. Chem. Eng. Sci. 1975;30:825.
                                          2
                                    2
                         ¼ p(0:15)(3:328   0:328 )(1:5)  mcleod, h.o., jr. Matrix acidizing. JPT 1984;36:2055–
                               3
                         ¼ 7:75 ft =ft ¼ 58 gal=ft:        2069.
                                                         paccaloni, g. and tambini, m. Advances in matrix stimu-
               This example shows that the Daccord model gives opti-
                                                           lation technology. JPT 1993;45:256–263.
               mistic results and the volumetric model gives more realistic
               results.                                  paccaloni, g., tambini, m., and galoppini, m. Key factors
                The maximum injection rate and pressure for carbon-  for enhanced results of matrix stimulation treatment.
               ate acidizing can be calculated the same way as that for  Presented at the SPE Formation Damage Control
               sandstone acidizing. Models of wormhole propagation  Symposium held in Bakersfield, California on Febru-
               predict that wormhole velocity increases with injection  ary 8–9, 1988. SPE Paper 17154.
                              1
               rate to the power of ⁄ 2 to 1. Therefore, the maximum  schechter, r.s. Oil Well Stimulation. Englewood Cliffs,
               injection rate is preferable. However, this approach may  NJ: Prentice Hall, 1992.
               require more acid volume. If the acid volume is con-  smith, c.f., and hendrickson, a.r. Hydrofluoric acid
               strained, a slower injection rate may be preferable. If a
               sufficient acid volume is available, the maximum injection  stimulation of sandstone reservoirs. JPT Feb. 1965,
               rate is recommended for limestone formations. However,  Trans. AIME 1965;234:215–222.
               a lower injection rate may be preferable for dolomites.  taha, r., hill, a.d., and sepehrnoori, k. Sandstone acid-
               This allows the temperature of the acid entering the for-  izing design with a generalized model. SPEPE Feb.
               mation to increase, and thus, the reaction rate increases.  1989:49–55.
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