An oil field in central Saudi Arabia produces super-light crude from a sand
stone reservoir. The formation contains up to 7.0 wt% authigenic clays domi
nated by kaolinite and illite/montmorillonite mixed layer clays. To mitigat
e sand production and improve well productivity, a frac pack stimulation tr
eatment was conducted on most producing wells in this field. The treatment
introduced several fluids, which might invade the formation and induce form
ation damage.
An experimental study was conducted to determine potential formation damage
due to fines migration and clay swelling, and to design an effective clay
stabilizer treatment. The work included performing coreflood experiments us
ing reservoir cores under reservoir conditions. The critical salt concentra
tion (defined, as the salt concentration below which there is loss of perme
ability) was first determined. Several commercial clay stabilizers, cationi
c polymers, were evaluated. The effects of stabilizer type, concentration a
nd acids on core permeability were investigated in detail.
The experimental results indicated that the critical salt concentration (KC
I brine) was nearly 5 wt%. Severe loss of permeability was observed when br
ines of lower salt concentrations were injected into reservoir cores. The e
ffectiveness of clay stabilizers was found to be a function of chemical typ
e and concentration. Some of the chemicals caused loss of injectivity at hi
gher concentrations. It was found that these chemicals did not readily diss
olve in water and formed fish eyes. When these chemicals were injected into
reservoir cores, they formed an external filter cake, which caused loss of
permeability. Good mixing of the stabilizer and proper filtration solved t
his problem. Hydrochloric acid at 15 wt% did improve the performance of at
least one of the clay stabilizers examined.
Based on lab testing, a cost effective clay stabilizer was tested in the fi
eld. Field results indicated that the chemical did not cause loss of inject
ivity, and minimized formation damage due to fines migration and clay swell
ing.