Sodium carbonate and sodium silicate promote the Ca-montmorillonite: the nucleation, stabilization and hydrophilicity mechanisms
Montmorillonite is widely utilized in catalysis, environmental science, and civil engineering. Previous studies have demonstrated that Na<sub>2</sub>CO<sub>3</sub> and Na<sub>2</sub>SiO<sub>3</sub> enhance the stability of Ca-montmorillonite-rich clayey soils in chemical soil stabilization. However, the microscopic mechanisms underlying their effects on nucleation, stabilization, and hydrophilicity remain unclear. This study investigates these mechanisms using Scanning Electron Microscopy (SEM) and Density Functional Theory (DFT) calculations. SEM results show that Na<sub>2</sub>CO<sub>3</sub> and Na<sub>2</sub>SiO<sub>3</sub> enhance the strength of the stabilized soils by promoting the formation of cementitious and crystalline substances. DFT calculations reveal that SiO<sub>3</sub> <sup>2-</sup> and CO<sub>3</sub> <sup>2-</sup> exhibit the most negative adsorption energies of -6.2 eV and -5.1 eV, respectively, in the exchangeable layers of montmorillonite, significantly higher than those of Na<sup>+</sup> and Ca<sup>2+</sup>. On the montmorillonite surface, SiO<sub>3</sub> <sup>2-</sup> and CO<sub>3</sub> <sup>2-</sup> display even lower adsorption energies of -8.7 eV and -6.8 eV, respectively. Water molecules preferentially adsorb dissociatively on the montmorillonite surface with an energy of -3.1 eV; however, their adsorption is suppressed following the adsorption of Ca<sup>2+</sup>, Na<sup>+</sup>, CO<sub>3</sub> <sup>2-</sup>, and SiO<sub>3</sub> <sup>2-</sup>, with energies decreasing to between -1.1 eV and -2.5 eV. Differential charge density plots indicate that ion adsorption leads to charge redistribution and the formation of chemical bonds. Specifically, Ca<sup>2+</sup> and Na<sup>+</sup> donate cationic charge, while CO<sub>3</sub> <sup>2-</sup> and SiO<sub>3</sub> <sup>2-</sup> accept electrons. The study further explains why Na<sub>2</sub>CO<sub>3</sub> and Na<sub>2</sub>SiO<sub>3</sub>, in combination with lime, are more effective than lime alone in soil stabilization. A mechanism model for nucleation, stabilization, and hydrophilicity is proposed to explain the role of Na<sub>2</sub>CO<sub>3</sub> and Na<sub>2</sub>SiO<sub>3</sub> in promoting Ca-montmorillonite stabilization. This work provides valuable insights into the chemical properties of montmorillonite and the synergistic effects of calcium-based stabilizers combined with Na<sub>2</sub>CO<sub>3</sub> and Na<sub>2</sub>SiO<sub>3</sub> for soil stabilization.
Authors
- Yong Peng (ORCID: https://orcid.org/0000-0002-9284-5611)
- Shenghua Deng (ORCID: https://orcid.org/0000-0002-5760-4900)
- Chong Ma (ORCID: https://orcid.org/0000-0002-5423-4449)
- Chenglong Yin
- Jin Huang
Institutions
- Zhejiang Shuren University (CN)
- Zhejiang University (CN)
Publication Details
- Journal
- Frontiers in Chemistry
- Published
- 2025-09-04
- DOI
- https://doi.org/10.3389/fchem.2025.1646971
- Citations
- 2
- Primary Topic
- Clay minerals and soil interactions
- Type
- article
- Field-Weighted Citation Impact
- 1.19