地学前缘 ›› 2025, Vol. 32 ›› Issue (2): 195-205.DOI: 10.13745/j.esf.sf.2025.2.8

• 南海北部天然气水物储层精细评价及实验模拟技术 • 上一篇    下一篇

不同分解压力下L-Met浓度对CO2水合物稳定性影响研究

王英梅1(), 王立瑾1, 滕亚栋1, 姜雪晨1, 张鹏2   

  1. 1.兰州理工大学能源与动力工程系, 甘肃 兰州 730050
    2.中国科学院西北生态环境资源研究院冻土工程国家重点实验室, 甘肃 兰州 730000
  • 收稿日期:2024-01-09 修回日期:2024-11-27 出版日期:2025-03-25 发布日期:2025-03-25
  • 作者简介:王英梅(1987—),女,博士,副教授,硕士生导师,主要从事气体水合物生成与分解动力学方面的研究。E-mail:wymch@lzb.ac.cn
  • 基金资助:
    国家自然科学基金项目(41661103);国家自然科学基金项目(41601079);国家重点研发计划项目(2017YFC0307303);甘肃省科技重大专项项目(22ZD6FA004);甘肃省中小企业创新基金项目(22CX3JA003)

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

摘要: 在当前能源需求和“双碳”的大背景下,利用添加促进剂的水合物法储存CO2受到广泛关注,而促进剂的使用对CO2水合物的各项性能影响不同。因此本文以硅胶为多孔介质,以3.0 MPa、274.15 K为初始生成条件,对比分析了分解温度为275.15 K条件下,分解压力分别为0、0.5、1 MPa时纯水体系和不同浓度(0.8、0.9、1.0、1.1、1.2 g/L)的L-蛋氨酸(L-Met)体系对CO2水合物稳定性的影响。结果表明:在0 MPa分解压力下1.1 g/L L-Met体系中的CO2水合物稳定性最好,分解压力为0.5 MPa和1 MPa时,0.9 g/L L-Met体系中水合物均表现出最好的稳定性,有利于水合物的稳定储存。除了研究L-Met浓度对稳定性的影响外,还分析了分解压力对水合物分解的影响。研究发现在纯水体系中,分解压力为0 MPa时水合物分解速率表现为先增大后减小,而其余分解压力条件下均在初始时刻具有最大分解速率,呈现单调递减趋势;同时发现除0.8 g/L L-Met体系外,其他体系在常压下分解初期时水合物分解速率均是先增大后减小,具有水合物的“自保护”效应,而在0.5 MPa和1 MPa压力下,只在初始时刻具有最大的分解速率,呈现单调减小的趋势,对上述效应具有破坏作用。通过上述研究,为CO2水合物的长距离运输和长时间储存提供数据及理论支撑。

关键词: CO2水合物, 硅胶, L-Met, 分解压力, 稳定性

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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