Water-calcite (104) surface interactions using first-principles simulations

An in-depth understanding of the water and mineral interaction is indispensable for many fields including enhanced oil recovery, global carbon cycle, and environment sustainability. In this work, using first-principles calculations based on density functional theory supplemented with semiempirical DFT-D2 dispersion corrections, we study the structural, energetic, electronic, and optical properties of hydrated calcite (104) surfaces via an exhaustive sampling of all the adsorption sites with up to full (monolayer) water coverage. Our results suggest that on-top Ca surface sites are the most energetically favorable sites for water adsorption. Also, we found sizable differences in the binding energies among the configurations having the same number of adsorbed water molecules, highly likely due to the differences in the organization and tilting of Ca-s-O-s octahedra along with the differences in the Ca-s-O-w bond distance and Ca-s-O-w-H bond angles. We also report intriguing variations in the optical absorption spectra of hydrated calcite (104) surfaces with respect to pristine (anhydrous) calcite (104) surface. Interestingly, we find significant variations in the optical absorption spectra among the hydrated calcite (104) surfaces having the same of adsorbed water molecules. The findings in this theoretical study would help in improving our fundamental understanding of hydrated calcite (104) surface that has impact on many processes in nature.

Automated summary

This study used density functional theory calculations to analyze the structural and energetic properties of hydrated calcite surfaces, finding that on-top Ca surface sites are the most energetically favorable for water adsorption, and significant variations in binding energies exist among configurations with the same number of adsorbed water molecules. Additionally, intriguing differences in the optical absorption spectra were observed among hydrated calcite surfaces with the same number of adsorbed water molecules, suggesting a fundamental understanding of hydrated calcite surfaces that impacts natural processes.