Structural, Mineralogical, and Rheological Properties of Methane Hydrates in Smectite Clays

Smectite clays are widely dispersed in deep ocean sediments and can be subdivided into two representative clay types, Cheto- and Wyoming-montmorillonites. In this study, we measured the thermodynamic phase behavior of methane hydrates intercalated at various concentrations of these clays and found t...

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Bibliographic Details
Published in:Journal of Chemical & Engineering Data
Main Authors: Seo, YJ Seo, Young-Ju, Seol, JW Seol, Ji-Woong, Yeon, SH Yeon, Sun-Hwa, Koh, DY Koh, Dong-Yeun, Cha, MJ Cha, Min-Jun, Kang, SP Kang, Sung-Pil, Seo, YT Seo, Yu-Taek, Bahk, JJ Bahk, Jang-Jun, Lee, JH Lee, Jae-Hyoung, Lee, H Lee, Huen
Format: Article in Journal/Newspaper
Language:English
Published: AMER CHEMICAL SOC 2009
Subjects:
X-RAY-DIFFRACTION; PHASE-EQUILIBRIUM; GAS-HYDRATE; MONTMORILLONITE; PHYLLOSILICATES; ETHANE; PORES; SI-29; RAMAN
Methane hydrate
Online Access:http://hdl.handle.net/10203/8887
https://doi.org/10.1021/je800833y
Description
Summary:Smectite clays are widely dispersed in deep ocean sediments and can be subdivided into two representative clay types, Cheto- and Wyoming-montmorillonites. In this study, we measured the thermodynamic phase behavior of methane hydrates intercalated at various concentrations of these clays and found the relatively weak promotion tendency when compared to that of pure methane hydrate stability. The structure and morphology of intercalated methane hydrate (IMH) samples were analyzed using the MAS NMR, RAMAN, LT-XRD, and Cryo-FE-SEM. The (27)Al and (29)Si solid-state MAS NMR spectra of IMH Cheto and Otay clays represent that the structural stability is preserved during the IMH formation, which is also indicated with the XRD pattern showing no structural transformation but different d-spacing values due to clay-water suspension and IMH. In addition, Cryo-SEM images of IMH samples show that IMH Otay clays provide well-developed methane hydrate (MH) morphology, compared to the IMH Cheto clay. This work was supported by the Korea Science and Engineering Foundation (KOSEF) through the National Research Laboratory. Program funded by the Ministry of Education, Science and Technology(No.R0A-2005-000-10074-0(2008)), and “Identifying the Natural Phenomenon of Methane Hydrate Formation in Clay and Sand Layers for recovering of gas hydrate” funded by the Ministry of Knowledge, Economy of Korea, also partially funded by the Brain Korea 21 Project. This work was supported by the Korea Science and Engineering Foundation (KOSEF) grant (WCU program, 31-2008-000-10055-0) funded by the Ministry of Education and Science and Technology(MEST).

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