Gas Hydrate Deposition on a Cold Surface in Water-Saturated Gas Systems

被引:88
作者
Rao, Ishan [1 ]
Koh, Carolyn A. [1 ]
Sloan, E. Dendy [1 ]
Sum, Amadeu K. [1 ]
机构
[1] Colorado Sch Mines, Ctr Hydrate Res, Chem & Biol Engn Dept, Golden, CO 80401 USA
关键词
FROST FORMATION; FLOW LOOP;
D O I
10.1021/ie400493a
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
One of the major issues in flow assurance includes pipeline plugging due to hydrate formation and deposition. A key uncertainty in gas pipelines is hydrate deposition on the pipe wall. This work demonstrates hydrate formation and deposition on a cold surface in water-saturated gas systems. Methane hydrate deposition can be achieved in a laboratory-scale apparatus by formation of hydrates from the gas phase on the outer surface of a cold surface. The deposit evolves from the initial formation to growth to hardening stages, observed to be initially a porous deposit that later anneals to a relatively nonporous deposit. The hydrate deposit thickness gradually reaches a limit as the hydrate surface approaches the hydrate equilibrium temperature. Performing the measurements at higher initial subcooling in the system results in a thicker hydrate deposit. The average calculated hydrate deposit porosity decreases during the experiment and reaches similar to 5% during the annealing stage.
引用
收藏
页码:6262 / 6269
页数:8
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