Drilling through shale and clay-rich formations can be challenging because these formations may react with water-based drilling fluids. When shale absorbs water, it may swell, soften, disperse or break away from the wellbore wall.
This can contribute to operational issues such as tight hole conditions, poor hole cleaning, excess drilled solids, bit balling or wellbore instability. The role of shale inhibition is to reduce the interaction between the drilling fluid and the shale formation.
The root cause: why shale reacts with water
Shale is made up of fine clay minerals arranged in layered structures. Common clay minerals include smectite, illite and kaolinite. These clay particles can carry surface charges and may attract water and ions when exposed to a water-based drilling fluid.
When an uninhibited water-based mud comes into contact with reactive shale, water may enter the clay structure or move into the formation because of salinity and chemical differences between the mud and the formation water.
Crystalline hydration
In crystalline hydration, water molecules enter the spaces between clay layers and attach themselves to clay surfaces and exchangeable cations. This can increase the spacing between the layers and cause swelling at the microscopic level.
Osmotic hydration
In osmotic hydration, water movement is driven by chemical potential differences between the drilling fluid and the formation. If the mud is not properly inhibited, water may move into the shale, increasing pore pressure and weakening the formation.
This is why shale inhibition is an important consideration in water-based mud systems used in reactive formations.