Abstract
It is generally assumed that limestone reservoir rocks will react much more rapidly with acid than dolomite reservoir rocks. This work is the first to show this assumption to be false in some cases, due to mineral impurities commonly found in these rocks. Trace amounts of clay impurities in limestone were found to reduce the acid dissolution rate by nearly an order of magnitude, to make the acid reactivity of these rocks similar to fully dolomitized rock. A rotating disk instrument was used to measure dissolution rates of reservoir rock from a deep, dolomitic gas reservoir in Saudi Arabia (275 °F, 7,500 psi). More than 60 experiments were made at temperatures of 23 and 85 °C and HCl concentrations of 1.0 M (3.6 wt%). Eight distinctly different rock types that varied in composition from 0 to 100% dolomite were used in this study. In addition, the mineralogy of each rock disk was examined before and after each rotating disk experiment with an Environmental Scanning Electron Microscope (ESEM) using secondary and backscattered electron imaging and energy dispersive X-ray (EDS) spectroscopy. Acid reactivity was correlated with the detailed mineralogy of the reservoir rock. It was also shown that bulk anhydrite in the rock samples was converted to anhydrite fines by the acid, a potential source of formation damage.
