đ€ AI Summary
This study identifies systematic misreporting of calcite and other carbonate mineral dissolution rate parameters in the PalandriâKharaka (2004) database, leading to overestimation of reaction timescales by up to one order of magnitude and severely compromising the reliability of reactive transport simulations. To address this, we first systematically identify and quantify the kinetic parameter representation bias within this widely used database, proposing an experimental validationâbased paradigm for parameter provenance tracing and calibration. Using a coupled ReaktoroâDuMuX simulator, we perform forward modeling and sensitivity analysis of batch calcite dissolution experiments. Following parameter correction, modelâdata agreement improves markedly, and timescale prediction error decreases tenfold. This work establishes a methodological framework for ensuring the credible application of geochemical reaction kinetics parameters in reactive transport modeling.
đ Abstract
In systems with slow reaction kinetics, such as mineral dissolution processes, chemical equilibrium cannot be assumed and 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. This misrepresentation leads to a considerable overestimation of reaction timescales. Using the simulators Reaktoro and DuMuX, we simulated a simple calcite dissolution batch test and compared 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.