An experimental study of gas-hydrate formation by measuring viscosity and infrared spectra

2003 ◽  
Vol 81 (1-2) ◽  
pp. 485-492 ◽  
Author(s):  
H Oyama ◽  
T Ebinuma ◽  
W Shimada ◽  
S Takeya ◽  
J Nagao ◽  
...  

We measured the viscosities and infrared (IR) spectra before and after hydrate nucleation. During the induction period, the viscosity increases and the infrared spectrum shifts to higher energy. After nucleation, the viscosity decreases abruptly, and the peak positions in the IR spectrum change to the small wave-number side. These results indicate that water acts as a precursor to hydrate nucleation. PACS Nos.: 66.20td, 78.30.30-j, 64.60Qb

1995 ◽  
Vol 45 (6) ◽  
pp. 517-520
Author(s):  
L. Ts. Adzhemyan ◽  
M. Hnatich ◽  
M. Stehlik

2019 ◽  
Vol 137 ◽  
pp. 94-100
Author(s):  
Marek Królikowski ◽  
Marta Królikowska ◽  
Hamed Hashemi ◽  
Paramespri Naidoo ◽  
Deresh Ramjugernath ◽  
...  

Author(s):  
David Colton

SynopsisIntegral operators are used to solve the direct and inverse problems of the scattering of acoustic waves by a spherically stratified inhomogeneous medium of compact support. The results are valid for all values of the wave number and an arbitrarily large index of refraction. In the limiting case of small wave number or small inhomogeneities the results are in agreement with those of Rorres and Born.


2013 ◽  
Vol 310 ◽  
pp. 28-32
Author(s):  
Jian Ye Sun ◽  
Yu Guang Ye ◽  
Chang Ling Liu ◽  
Jian Zhang

The simulate experiments of gas production from methane hydrates reservoirs was proceeded with an experimental apparatus. Especially, TDR technique was applied to represent the change of hydrate saturation in real time during gas hydrate formation and dissociation. In this paper, we discussed and explained material transformation during hydrate formation and dissociation. The hydrates form and grow on the top of the sediments where the sediments and gas connect firstly. During hydrates dissociation by depressurization, the temperatures and hydrate saturation presented variously in different locations of sediments, which shows that hydrates dissociate earlier on the surface and outer layer of the sediments than those of in inner. The regulation of hydrates dissociation is consistent with the law of decomposition kinetics. Furthermore, we investigated the depressurizing range influence on hydrate dissociation process.


2000 ◽  
Vol 253 (2-3) ◽  
pp. 331-337 ◽  
Author(s):  
Hideyuki Nakayama ◽  
Yukiko Minagawa ◽  
Chihiro Abematsu ◽  
Sachiko Yajima ◽  
Kikujiro Ishii

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