SPE Production & Operations
Volume 26,
Number 4,
November 2011,
pp. 381-387
Summary
Guar gum and its derivatives have been the most commonly used polymers to
increase the viscosity of fracturing fluids. However, the conductivity of many
fractures created with guar-based polymers is low because of residual unbroken
polymer gel remaining in the fracture. This residue can cause permeability
impairment in the proppant pack, resulting in low fracture conductivity and
decreased effective fracture length. In this study, we experimentally evaluated
two important aspects of the gel damage process--the thickness of the
polymer-gel filter cake that is created as fracture-fluid filtrate leaks off
into the formation and the yield stress of the concentrated polymer gel that
accumulates in the fracture. The thickness of the filter cake created during
the leakoff process was measured as a function of the polymer loading and the
volume of leakoff. We created the filter cake following the procedure described
by Ayoub et al. (2006) and then measured the filter-cake thickness with a
precise laser profilometer. We found that the filter-cake thickness varied
linearly with leakoff volume, meaning that the gel concentration factor is
constant for this guar polymer fluid. The concentrated polymer filter cakes
created by leakoff behave rheologically as Herschel-Bulkley fluids having a
yield stress. The yield stress of this material is a critical parameter
influencing whether the gel can be removed from the fracture. We measured the
yield stress of borate-crosslinked guar polymer fracture fluids at
concentrations up to 200 lbm/1,000 gals by use of a unique flat-plate device.
The yield stresses of the polymer filter cakes were found to depend strongly on
the concentration of both polymer and breaker.
© 2011. Society of Petroleum Engineers
View full textPDF
(
1,952 KB
)
History
- Original manuscript received:
23 November 2010
- Meeting paper published:
25 January 2011
- Revised manuscript received:
14 April 2011
- Manuscript approved:
24 June 2011
- Published online:
12 October 2011
- Version of record:
22 November 2011