SUBSURFACE MAPPING OF THE PRAIRIE EVAPORITE GROUP SALT DEPOSITS: ASSESSING SALT CAVERN QUALITY FOR COMPRESSED AIR ENERGY STORAGE
We present preliminary data from two cores and 118 well logs from south-central Alberta that penetrate the Prairie Evaporite and Lotsberg Formations of the EPG. From these, it has been found that the Prairie Evaporite Formation contains on the order of 3-5 % siltstone and anhydrite as mud drapes and dissolution lenses, with no thick layers of anhydrite or mudstone. The Lotsberg is nearly pure halite, and is therefore more suited to solution mining operations despite having a thick dolomite and anhydrite layer at its stratigraphic center. Based on our preliminary results, we identify areas containing salt that may be economically brined. We also identify layers of anhydrite or mudstone that may cause damage to drilling equipment or incur extra drilling time; thick layers (>10m) can render a salt bed uneconomic to develop. To delineate those beds, we use drill cores and well logs to correlate inter-salt mudstone and anhydrite layers. This allows us to not only identify concerns for drilling but also large scale environmental cycles and sub basins.
Future work will involve collaboration with researchers from other disciplines such as mechanical, electrical, and civil engineering to plan cavern shape and placement.