Work

Implementation Pitfalls for carbonate mineral dissolution — A technical note

Year: 2025

Type: article

Abstract: In reactive transport modeling, an accurate understanding of reaction rates is essential; discrepancies in parameter reporting can greatly affect simulation results. This technical note identifies an issue with the reporting of rate parameters for carbonate mineral dissolution in a widely used database for reactive transport modeling based on Palandri and Kharaka (2004). Specifically, the reaction order was reported with respect to the partial pressure P ( CO 2 ) rather than the activity of H 2 CO 3 ∗ , causing a considerable overestimation of reaction timescales. We demonstrate the implications of this error by simulating a calcite dissolution batch experiment using Reaktoro and DuMuX and comparing the results to experimental data. By adjusting the parameter to align with established literature, we demonstrate an improved fit between simulated and experimental data. Discrepancies in reaction timescales were reduced by an order of magnitude, emphasizing the importance of regular validation of simulations with experimental data. • Reporting error found in carbonate dissolution parameters (Palandri & Kharaka, 2004). • Original literature shows reaction orders must reference H 2 CO 3 ⁎ activity. • Reported parameters overestimate dissolution timescales by ̃20-fold. • Corrected parameters align simulations with experimental observations.

Source: Applied Geochemistry

DOI: 10.1016/j.apgeochem.2025.106611

Authors: Fiona J. Weiss, Leon Keim, Kai Wendel, Holger Class

Institution: University of Stuttgart

Language: English

Topic: CO2 Sequestration and Geologic Interactions

Subfield: Environmental Engineering

Field: Environmental Science

Domain: Physical Sciences

Open Access status: hybrid

Estimated APC paid: $3,490

Funder: Deutsche Forschungsgemeinschaft