Open AccessExperimental study on the formation characteristics of CO 2 hydrate in porous media below the freezing point: Influence of particle size and temperature on the formation process and storage capacity
Author(s) -
Zhang Xuemin,
Zhang Mengjun,
Yang Huijie,
Li Jinping,
Li Yinhui,
Wu Qingbai
Publication year - 2022
Publication title -
energy science and engineering
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.638
H-Index - 29
ISSN - 2050-0505
DOI - 10.1002/ese3.1089
Subject(s) - clathrate hydrate , hydrate , permafrost , supercooling , porous medium , particle size , porosity , freezing point , chemistry , particle (ecology) , chemical engineering , ice crystals , mineralogy , thermodynamics , materials science , meteorology , geology , organic chemistry , oceanography , physics , engineering
CO 2 storage in form of hydrate in stratigraphic sediment has been considered to be one of the effective strategies against global warming and mitigating CO 2 emission, which has attracted extensive research interest in the field of greenhouse gas (GHG) reduction and natural gas hydrate exploitation in permafrost regions. How the formation characteristics of CO 2 hydrate influences the storage process is a fundamental issue related to the hydrate‐based technology of CO 2 sequestration and storage in the permafrost regions. In this study, the formation experiments of CO 2 hydrate were carried out in porous media below freezing point under the condition of different particle sizes and temperatures. The influence of different factors on the formation rate, conversion rate, and gas storage capacity of CO 2 hydrate were studied through experiments. It was indicated that temperature and ice particle size had a significant effect on the formation characteristics of CO 2 hydrate in porous media below the freezing point. However, it did not mean that the greater the degree of supercooling was the better the hydrate formation would be. The formation rate and conversion rate of hydrate were relatively higher when the temperature approached to the freezing point. In contrast, the gas storage capacity of CO 2 hydrate was higher than that above the freezing point. The average formation rate, conversion rate, and gas storage capacity of CO 2 hydrate were obtained under the temperature of 270.15 K, which was 3.68 × 10 −4 mol h −1 , 40.47%, and 75.09 L/L, respectively. When the ice particle size was 700 µm under the same particle size of quartz sand, the conversion rate and gas storage capacity of CO 2 hydrate was the maximum, reached to 49.69% and 92.19 L/L, respectively. These results provide greater insights into the hydrate‐based technology of CO 2 sequestration and storage in sediments.