Experimental evidence for self-limiting reactive flow through a fractured cement core: implications for time-dependent wellbore leakage.
We present a set of reactive transport experiments in cement fractures. The experiments simulate coupling between flow and reaction when acidic, CO(2)-rich fluids flow along a leaky wellbore. An analog dilute acid with a pH between 2.0 and 3.15 was injected at constant rate between 0.3 and 9.4 cm/s into a fractured cement core. Pressure differential across the core and effluent pH were measured to track flow path evolution, which was analyzed with electron microscopy after injection. In many experiments reaction was restricted within relatively narrow, tortuous channels along the fracture surface. The observations are consistent with coupling between flow and dissolution/precipitation. Injected acid reacts along the fracture surface to leach calcium from cement phases. Ahead of the reaction front, high pH pore fluid mixes with calcium-rich water and induces mineral precipitation. Increases in the pressure differential for most experiments indicate that precipitation can be sufficient to restrict flow. Experimental data from this study combined with published field evidence for mineral precipitation along cemented annuli suggests that leakage of CO(2)-rich fluids along a wellbore may seal the leakage pathway if the initial aperture is small and residence time allows mobilization and precipitation of minerals along the fracture.
Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78712, United States. njhuerta@utexas.edu
Nicolas J
NJ
Huerta
Marc A
MA
Hesse
Steven L
SL
Bryant
Brian R
BR
Strazisar
Christina L
CL
Lopano
D002245:Carbon Dioxide / Q000737:chemistry*; D011232:Chemical Precipitation; D003252:Construction Materials; D055593:Geological Phenomena; D006851:Hydrochloric Acid / Q000737:chemistry; D011312:Pressure; D012995:Solubility; D014872:Water Movements
D002245:Carbon Dioxide; D006851:Hydrochloric Acid