Injecting carbon dioxide into basalt rock creates a chemical reaction that literally cracks the stone open, making more room for storage.
Basalt rocks undergo reaction-induced fracturing when they react with injected CO2 to form minerals. Standard engineering assumes that as minerals fill up the pores in a rock, the storage capacity would slowly drop to zero. Instead, the pressure from the growing crystals creates a new network of cracks that increases the rock total porosity. This self-expanding storage means basalt formations could hold significantly more carbon than previous estimates suggested. This process turns a major hurdle for carbon sequestration into a natural engine that helps clean the atmosphere.
Experimental observations that carbonation of basalt stores CO2 in coupled reaction induced fractures
SSRN · 6629845
Recent laboratory and field studies have highlighted that in-situ carbonation within basalt formations could provide secure storage for anthropogenic CO2. Here, we present the results of a continuous 93-day laboratory experiment simulating the geological reservoir environment of engineered CO2 mineralisation. The CO2 mineralisation reaction is documented in a time-resolved dataset of 3-dimensional x-ray microtomography images. The chemical, physical, and mineralogical changes in the sample over