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Electrokinetic behavior of artificial and natural calcites: A review of experimental measurements and surface complexation models

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ELSEVIER
DOI: 10.1016/j.cis.2022.102600

关键词

Calcite; Surface charge; Zeta potential; Electrokinetics; Surface complexation modeling; Reactive transport; Chalk

资金

  1. Danish Hydrocarbon Research and Technology Centre under the Advanced Water Flooding program

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The surface charge of calcite plays a crucial role in various industrial and environmental applications. This paper reviews different surface complexation models proposed to explain the effects of surface interactions on calcite's zeta potential and discusses their main differences. The study reveals that the discrepancies between the models and experimental data can be explained by different levels of disequilibrium.
The surface charge of calcite in aqueous environments is essential to many industrial and environmental ap-plications. Electrokinetic measurements are usually used to assess the calcite charging behavior and characterize its electrical double layer (EDL). Numerous surface complexation models (SCMs) have been proposed to interpret the effect of different surface interactions on the zeta potential. Because of their versatility, SCMs have also become important tools in reactive transport modeling. The research on enhanced oil recovery within the last decade has led to an increased number of publications reporting both zeta potential measurements and SCMs for calcite. Nonetheless, the measurements are often inconsistent and the reasons for choosing one model over another are unclear. In this work, we review the models proposed for calcite and address their main differences. We first collect a large number of published zeta potential measurements and then we fit a Diffuse Layer, Basic Stern, and Charge-Distribution Multi-Site Complexation models to a selected reliable dataset. For each model, we maintain a similar number of adjustable parameters. After optimizing the parameters of the models, we sys-tematically compare their prediction capabilities against data obtained in monovalent and divalent electrolyte systems containing calcium, magnesium, sulfate, or carbonate. We show that, often, the discrepancies between the models and the experimental data can be explained by different levels of disequilibrium. Nonetheless, as-sumptions used in the development of the models may significantly reduce their extrapolability to variable chemical conditions. The poor agreement between the models tuned to electrokinetic data with surface charge measurements and dynamic retention from single-phase flowthrough tests show that zeta potential may not be the best type of data to characterize ion binding at the calcite surface. Including the effect of mineral impurities and temperature on the calcite surface speciation and electrokinetic behavior prevail as main challenges for reactive transport modeling.

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