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Updated: Jun 6, 2025

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
Published on: June 4, 2021
Synergized Effects of Amino Acids and NaCl to Enhance Silicate Mineral Dissolution in Aqueous Environments for
Jiajie Wang1, Sena Kikuchi1, Noriyoshi Tsuchiya1,2
1Department of Environmental Studies for Advanced Society, Graduate School of Environmental Studies, Tohoku University, Sendai 980-8579, Japan.
Abstract:
Enhanced weathering of silicate minerals is a promising approach for reducing atmospheric CO2 levels by increasing the aquatic pH and facilitating CO2 dissolution. However, the slow and unsustainable dissolution of silicate minerals in natural environments remains a challenge. This study proposed a new CO2 capture system that uses the combined effect of amino acids and NaCl to promote mineral dissolution, and its characteristics were investigated experimentally. The results showed that amino acids are promising for enhancing the near-congruent dissolution of silicate minerals, specifically at weakly alkaline pHs (i.e., 8), implying the long-term effectiveness of the system. Comprehensive findings revealed a 13-fold increase in the level of Ca extraction from wollastonite (CaSiO3) in the presence of 0.1 mol/L glutamic acid (Glu) over 72 h at 35 °C and a 22-fold increase in the level of CO2 capture efficiency. However, Fe-bearing minerals, such as olivine ((Mg,Fe)2SiO4), are unsuitable for application, because the enhanced Fe extraction results in the generation of Fe hydroxide, which lowers pH and consequently reduces CO2 capture efficiency. Moreover, NaCl facilitates the release of the Ca-Glu complex from mineral surfaces into the solution, synergizing amino acids to promote mineral dissolution. A semiclosed application system is proposed, with future studies needed to assess ecological impacts and ensure long-term sustainability.
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