Calcium sulfate (CaSO4) in the form of gypsum and anhydrite is one of the more prevalent evaporite minerals typically found in the carbonate rocks of the western Canadian sedimentary basin (WCSB). Most calcium sulfate scale inhibitors used for acid treatments rely on either the retardation of CaSO4crystal growth or the creation of soluble complex salts with the calcium ions. A broad-spectrum scale inhibitor has been specially formulated for high-salinity and acid solutions that not only prevents the precipitation of CaSO4but also helps inhibit the initial dissolution of CaSO4.
Introduction
Covering a vast extension of 1.4 million km2, the WCSB is between the southwestern border of the Canadian shield in Manitoba and the eastern flank of the Canadian Rocky Mountain system in British Columbia. Approximately half of the WCSB is composed of carbonate reservoirs.
Commonly, these carbonate formations are stimulated with acid. Depending on the formation itself and the presence of formation damage, two main acid-stimulation techniques are used: matrix acidizing and acid fracturing.
