Colloidal gas aphrons (CGA) have the unique ability to form a bridge in the pores of the reservoirs which stops fluid invasion. Sizing microbubbles in accordance with the rock pore size distribution is imperative for effective sealing during drilling.
Effects of time, temperature, and pressure on the stability and size of the microbubbles needs to be better understood in order to design a fluid that will sufficiently block the pores of the formation for extended periods.
In this study, effects of time, pressure and temperature on the size of the microbubbles and the stability of microbubble (CGA) based drilling fluids were investigated. The change in the CGA diameter with time is determined by using a microscopic imaging technique.
The effect of base fluid viscosity and surfactant concentration on the size and stability with time of the microbubbles was also investigated.
CGA based drilling fluids have been successfully used in high-angle and horizontal well drilling in highly depleted reservoirs1. Micro-bubbles in CGA based drilling fluids form a bridge in front of the pores of the rock. This bridge is believed stabilize the rock while allowing minimal damage to the formation.
Stability of the micro- bubbles and how bubble size changes as a function of downhole conditions (i.e., temperature and pressure) are some of the major concerns associated with the application of CGA based drilling fluids. A stable CGA structure requires maintaining an ideal film wall thickness of 4 to 10 micron2. Another factor affecting CGA stability is the rate of transfer of the surfactant molecules between the viscous water shell and the bulk phase due to gravity drainage or temperature gradients. This leads to a surface tension gradient at the surface of the shell. As a result, the Marangoni Effect will counteract this deformation3–4. Increasing the viscosity of the shell can help to minimize the transfer of surfactant molecules. Usually a biopolymer is added to adjust the shell viscosity3. The third property that the CGA structure must have is low diffusivity, which is the ability of the air that is in the core to transfer to the aqueous shell.
CGA bubble size and stability have been the subject of earlier studies5–12. Longe6 analyzed the bubble size distribution of CGAs for soil and groundwater decontamination applications. Longe's analyses included effects of surfactant concentration, surfactant type and electrolytes on the stability of the CGAs over the time. Jauregi et al. 7 also investigated the stability of CGAs as a function of surfactant concentration. Results from both studies indicated that the stability of CGAs increases with increasing surfactant concentration. Chaphalkar et al. 8 measured the size distribution of CGAs using a particle size analyzer. It was found that for three different types of surfactant, the CGAs were virtually nonexistent after 20 minutes. Roy et al. 9 reported similar results.
Amiri and Woodburn10 studied the rate of drainage as well as the CGA bubble size by recording the images of the CGAs over the time. They showed that after 10 minutes, the bubble shape had changed from spheres to polyhedral structures.
