Solutions and case studies for thermally driven reactive transport and porosity evolution in geothermal systems (reactive Lauwerier problem)

• Published in: Hydrology and earth system sciences Vol. 28; no. 20; pp. 4559 - 4576
• Main Authors: Roded, Roi, Aharonov, Einat, Szymczak, Piotr, Veveakis, Manolis, Lazar, Boaz, Dalton, Laura E
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 23.10.2024; Copernicus Publications
• Subjects: Aquatic resources; Aquifer storage; Aquifers; Carbon dioxide; Carbonates; Case studies; Chemical precipitation; Chemical reactions; Confined aquifers; Contamination; Dissolution; Dissolving; Energy; Energy storage; Evolution; Fluid injection; Force and energy; Groundwater; Heat; Hydraulic equipment; Hydraulic systems; Hydrochemicals; Injection; Management; Minerals; Permeability; Porosity; Precipitation; Reinjection; Sandstone; Sedimentary rocks; Sediments; Silica; Solubility; Supersaturation; Technology application; Temperature dependence; Thermal energy; Water; Water injection; Water resources
• ISSN: 1607-7938; 1027-5606; 1607-7938
• DOI: 10.5194/hess-28-4559-2024

Subsurface non-isothermal fluid injection is a ubiquitous scenario in energy and water resource applications, which can lead to geochemical disequilibrium and thermally driven solubility changes and reactions. Depending on the nature of the solubility of a mineral, the thermal change can lead to either mineral dissolution or precipitation (due to undersaturation or supersaturation conditions). Here, by considering this thermo-hydro-chemical (THC) scenario and by calculating the temperature-dependent solubility using a non-isothermal solution (the so-called Lauwerier solution), thermally driven reactive transport solutions are derived for a confined aquifer. The coupled solutions, hereafter termed the “reactive Lauwerier problem”, are developed for axisymmetric and Cartesian symmetries and additionally provide the porosity evolution in the aquifer. The solutions are then used to study two common cases: (I) hot CO2-rich water injection into a carbonate aquifer and (II) hot silica-rich water injection into a sandstone aquifer, leading to mineral dissolution and precipitation, respectively. We discuss the timescales of such fluid–rock interactions and the changes in hydraulic system properties. The solutions and findings contribute to the understanding and management of subsurface energy and water resources, such as aquifer thermal energy storage, aquifer storage and recovery and reinjection of used geothermal water. The solutions are also useful for developing and benchmarking complex coupled numerical codes.