Reactive transport modeling of the interaction between water and a cementitious grout in a fractured rock. Application to ONKALO (Finland)

• Published in: Applied geochemistry 2011-07, Vol.26 (7), p.1115-1129
• Main Authors: Soler, Josep M., Vuorio, Marja, Hautojärvi, Aimo
• Format: Article
• Language: English
• Subjects: alkalinity; calcium; cement; Cements; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Fracture mechanics; gels; Geochemistry; gneiss; groundwater; Grout; Hydration; leaching; Mathematical models; mineralogy; monitoring; nuclear fuels; Plumes; Pollution, environment geology; porosity; Repositories; Rock; silica; silicon
• ISSN: 0883-2927; 1872-9134
• DOI: 10.1016/j.apgeochem.2011.04.001

► It is planned to seal conductive fractures near a repository with cementitious grout. ► Modeling includes simultaneous hydration and leaching of the grout. ► Modeling results show a very limited formation of the high-pH plume. ► Results are in qualitative agreement with borehole monitoring data. Grouting of water-conducting fractures with low-alkali cement is foreseen for the potential future repository for spent nuclear fuel in Finland (ONKALO). A possible consequence of the interaction between groundwater and grout is the formation of high-pH solutions which will be able to react with the host rock (gneisses) and alter its mineralogy and porosity. A reactive transport modeling study of this possible alteration has been conducted. First, the hydration of the low-alkali cementitious grout has been modeled, using results from the literature as a guide. The hydrated cement is characterized by the absence of portlandite and the presence of a C–S–H gel with a Ca/Si ratio about 0.8 after tens of years (Ca/Si is about 1.7 in Ordinary Portland Cement). Second, calculations have simulated the interaction between flowing water and grout and the formation of an alkalinity plume, which flows beyond the grouted section of the fracture. The calculations include the hydration and simultaneous leaching of the grout through diffusive exchange between the porewater in the grout and the flowing water in the fracture. The formation of an alkaline plume is extremely limited when the low-pH grout is used. Even when using a grout with a lower silica fume content, the extent and magnitude of the alkaline plume is quite minor. These results are in qualitative agreement with monitoring at ONKALO.