G061046 Crystal Growth of Clathrate Hydrate in Flowing Liquid Water System Saturated with Methane Gas

2013 ◽  
Vol 2013 (0) ◽  
pp. _G061046-1-_G061046-3
Author(s):  
AIFAA Mazlan MUHAMMAD ◽  
Takehide KODAMA ◽  
Ryo OHMURA
2015 ◽  
Vol 15 (2) ◽  
pp. 559-563 ◽  
Author(s):  
Muhammad Aifaa ◽  
Takehide Kodama ◽  
Ryo Ohmura

2005 ◽  
Vol 5 (3) ◽  
pp. 953-957 ◽  
Author(s):  
Ryo Ohmura ◽  
Sadatoshi Matsuda ◽  
Tsutomu Uchida ◽  
Takao Ebinuma ◽  
Hideo Narita

2006 ◽  
Vol 6 (6) ◽  
pp. 1428-1439 ◽  
Author(s):  
Ju Dong Lee ◽  
Myungho Song ◽  
Robin Susilo ◽  
Peter Englezos

2011 ◽  
Vol 11 (7) ◽  
pp. 3235-3242 ◽  
Author(s):  
Sho Watanabe ◽  
Kota Saito ◽  
Ryo Ohmura

2011 ◽  
Vol 11 (1) ◽  
pp. 295-301 ◽  
Author(s):  
Kota Saito ◽  
Masatoshi Kishimoto ◽  
Ryo Tanaka ◽  
Ryo Ohmura

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Meku Maruyama ◽  
Riku Matsuura ◽  
Ryo Ohmura

AbstractHydrate-based gas separation technology is applicable to the CO2 capture and storage from synthesis gas mixture generated through gasification of fuel sources including biomass. This paper reports visual observations of crystal growth dynamics and crystal morphology of hydrate formed in the H2 + CO2 + tetrahydropyran (THP) + water system with a target for developing the hydrate-based CO2 separation process design. Experiments were conducted at a temperature range of 279.5–284.9 K under the pressure of 4.9–5.3 MPa. To simulate the synthesis gas, gas composition in the gas phase was maintained around H2:CO2 = 0.6:0.4 in mole fraction. Hydrate crystals were formed and extended along the THP/water interface. After the complete coverage of the interface to shape a polycrystalline shell, hydrate crystals continued to grow further into the bulk of liquid water. The individual crystals were identified as hexagonal, tetragonal and other polygonal-shaped formations. The crystal growth rate and the crystal size varied depending on thermodynamic conditions. Implications from the obtained results for the arrangement of operating conditions at the hydrate formation-, transportation-, and dissociation processes are discussed.


1982 ◽  
Vol 60 (7) ◽  
pp. 881-892 ◽  
Author(s):  
Russell G. Ross ◽  
Per Andersson

Solid phases in the tetrahydrofuran–water (THF–H2O) system were investigated in the temperature range 100–260 K and at pressures up to 1.5 GPa. Thermal conductivity, λ, and heat capacity per unit volume, ρcp, were measured, using the transient hot-wire method. We made measurements on solid phases having nominal compositions THF•17H2O, THF•7•1H2O, and THF•4•6H2O, which we refer to as phases α, β, and γ, respectively. Phase α is known to be a structure II clathrate hydrate, and λ for this phase was found to be similar to other crystalline solids which are glass-like in relation to their thermal properties. Low-energy excitations are known to be relevant to the properties of glass-like solids, and, in the case of phase α, were probably rotational vibrations of the THF guest molecules. Phase β was similar, and we inferred that it was probably a structure I clathrate hydrate. Phase γ behaved nearly like a normal crystal phase at low temperatures, but λ became almost independent of temperature near melting. At 1.1 GPa and 130 K, we found evidence that phase α transformed, on pressurization, to a metastable modification which may be a new high-density form of clathrate hydrate. The astrophysical implications of our results were mentioned briefly.


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