TY - JOUR
T1 - Clathrate hydrate formation in the system methane + 3-methyl-1-butanol + water
T2 - Equilibrium data and crystallographic structures of hydrates
AU - Ohmura, R.
AU - Takeya, S.
AU - Uchida, T.
AU - Ikeda, I. Y.
AU - Ebinuma, T.
AU - Narita, H.
N1 - Funding Information:
The authors thank Mr. Katsunori Matsushita (Hokkaido Branch, Suzuki Shoko Co., Sapporo, Japan) and Mr. Junji Itoh (Itoh Keiki Kogyosho, Co., Sapporo, Japan) for their help in the experimental work and in the maintenance of the apparatus. The authors also thank Ms. Y. Maeda and Mr. Sadatoshi Matsuda (AIST, Sapporo) for their help in preparing the manuscript. This study was supported by Industrial Technology Research Grant Program in 2003 (Grant No. 03B64003c) from New Energy and Industrial Technology Development Organization (NEDO) of Japan.
PY - 2004/7/30
Y1 - 2004/7/30
N2 - Clathrate hydrate formation in the system methane + 3-methyl-1-butanol + water is demonstrated. The data of four-phase-equilibria for methane + 3-methyl-1-butanol + hydrate + water equilibria are determined in the temperature range of 273-282 K. The equilibrium pressures at temperatures below 279 K are lower, by 0.4 MPa at most, than those of structure I hydrate formed in the methane + water system without 3-methly-1-butanol, suggesting the formation of a hydrate different from structure I methane hydrate. Conversely, at temperatures above 279 K, the equilibrium pressures are higher by 0.2 MPa than those of the methane structure I hydrate, suggesting the thermodynamically inhibited formation of structure I methane hydrate. To confirm the crystallographic structures of the hydrates, X-ray diffraction and Raman-spectroscopy measurements were performed with hydrate crystal samples prepared at two conditions: at 274.0 K and 2.55 MPa, and at 279.5 K and 6.30 MPa. The measurements revealed a structure II hydrate formation at the lower temperature, contrary to the expectation of the structure H hydrate formation. The hydrate formed at the higher temperature was determined to be of structure I.
AB - Clathrate hydrate formation in the system methane + 3-methyl-1-butanol + water is demonstrated. The data of four-phase-equilibria for methane + 3-methyl-1-butanol + hydrate + water equilibria are determined in the temperature range of 273-282 K. The equilibrium pressures at temperatures below 279 K are lower, by 0.4 MPa at most, than those of structure I hydrate formed in the methane + water system without 3-methly-1-butanol, suggesting the formation of a hydrate different from structure I methane hydrate. Conversely, at temperatures above 279 K, the equilibrium pressures are higher by 0.2 MPa than those of the methane structure I hydrate, suggesting the thermodynamically inhibited formation of structure I methane hydrate. To confirm the crystallographic structures of the hydrates, X-ray diffraction and Raman-spectroscopy measurements were performed with hydrate crystal samples prepared at two conditions: at 274.0 K and 2.55 MPa, and at 279.5 K and 6.30 MPa. The measurements revealed a structure II hydrate formation at the lower temperature, contrary to the expectation of the structure H hydrate formation. The hydrate formed at the higher temperature was determined to be of structure I.
KW - 3-Methyl-1-butanol
KW - Clathrate hydrate
KW - Gas hydrate
KW - Methane
KW - Mixture
KW - Solid-fluid equilibria
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U2 - 10.1016/j.fluid.2004.05.003
DO - 10.1016/j.fluid.2004.05.003
M3 - Article
AN - SCOPUS:3242716195
SN - 0378-3812
VL - 221
SP - 151
EP - 156
JO - Fluid Phase Equilibria
JF - Fluid Phase Equilibria
IS - 1-2
ER -