Earth Science Frontiers ›› 2025, Vol. 32 ›› Issue (2): 195-205.DOI: 10.13745/j.esf.sf.2025.2.8

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Study on the influence of L-methionine concentrations on carbon dioxide hydrate stability under different decomposition pressures

WANG Yingmei1(), WANG Lijin1, TENG Yadong1, JIANG Xuechen1, ZHANG Peng2   

  1. 1. Department of Energy and Power Engineering, Lanzhou University of Technology, Lanzhou 730050, China
    2. State Key Laboratory of Permafrost Engineering, Northwest Academy of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2024-01-09 Revised:2024-11-27 Online:2025-03-25 Published:2025-03-25

Abstract:

The storage of carbon dioxide (CO2) hydrate using promoters has garnered significant attention in the context of increasing energy demand and the “dual carbon” goals. However, different promoters exhibit varying effects on the properties of CO2 hydrate. This study investigates the formation and stability of CO2 hydrate using silica gel as a porous medium under initial formation conditions of 3.0 MPa and 274.15 K, followed by decomposition at 275.15 K. The effects of decomposition pressures (0, 0.5, and 1 MPa) on the stability of CO2 hydrate were analyzed in systems containing pure water and L-Met (L-methionine) solutions at concentrations of 0.8, 0.9, 1.0, 1.1, and 1.2 g/L. The results show that the CO2 hydrate in the 1.1 g/L L-Met solution exhibits the highest stability at a decomposition pressure of 0 MPa. The 0.9 g/L L-Met solution provides the best hydrate stability at decomposition pressures of 0.5 MPa and 1 MPa, which is favorable for stable hydrate storage. In addition to analyzing the influence of L-Met concentrations on hydrate stability, the effect of decomposition pressure on hydrate dissociation rates was also studied. In the pure water system, the dissociation rate initially increases and then decreases under a decomposition pressure of 0 MPa. For all other decomposition pressures, the maximum dissociation rate occurs at the initial stage, followed by a monotonic decrease. Furthermore, in L-Met systems, except for the 0.8 g/L concentration, the dissociation rate of hydrate under atmospheric pressure (0 MPa) initially increases and then decreases, demonstrating the “self-protection” effect of hydrate. However, the dissociation rate reaches its maximum at the initial moment and monotonically decreases at decomposition pressures of 0.5 MPa and 1 MPa, indicating that higher pressures undermine the self-protection effect. This study provides insights into the effects of promoter concentration and decomposition pressure on the stability and dissociation behavior of CO2 hydrate, contributing to advancements in hydrate-based CO2 storage technologies.

Key words: carbon dioxide hydrate, silica gel, L-Methionine, dissociation pressure, stability

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