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Measurements of Hydrate Equilibrium Conditions for CH4, CO2, and CH4+C2H6+C3H8 in Various Systems by Step-heating Method 被引量:8

Measurements of Hydrate Equilibrium Conditions for CH4, CO2, and CH4+C2H6+C3H8 in Various Systems by Step-heating Method
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摘要 Phase equilibrium conditions of gas hydrate in several systems were measured by the step-heating method using the cylindrical transparent sapphire cell device.The experimental data for pure CH4 or CO2+deionized water systems showed good agreement with those in the literatures.This kind of method was then applied to CH4/CO2+sodium dodecyl sulfate(SDS)aqueous solution,CH4/CO2+SDS aqueous solution+silica sand,and(CH4+C2H6+C3H8)gas mixture+SDS aqueous solution systems,where SDS was added to increase the hydrate formation rate without evident influence on the equilibrium conditions.The feasibility and reliability of the step-heating method,especially for porous media systems and gas mixtures systems were determined.The experimental data for CO2+silica sand data shows that the equilibrium pressure will change significantly when the particle size of silica sand is less than 96μm.The formation equilibrium pressure was also measured by the reformation of hydrate. Phase equilibrium conditions of gas hydrate in several systems were measured by the step-heating method using the cylindrical transparent sapphire cell device. The experimental data for pure CH4 or CO2 + deionized water systems showed good agreement with those in the literatures. This kind of method was then applied to CH4/CO2+ sodium dodecyl sulfate (SDS) aqueous solution, CH4/CO2+ SDS aqueous solution + silica sand, and (CH4 + C2H6 + C3H8) gas mixture + SDS aqueous solution systems, where SDS was added to increase the hydrate formation rate without evident influence on the equilibrium conditions. The feasibility and reliability of the step-heating method, especially for porous media systems and gas mixtures systems were determined. The experimental data for CO2+ silica sand data shows that the equilibrium pressure will change significantly when the particle size of silica sand is less than 96μm. The formation equilibrium pressure was also measured by the reformation of hydrate.
出处 《Chinese Journal of Chemical Engineering》 SCIE EI CAS CSCD 2009年第4期635-641,共7页 中国化学工程学报(英文版)
基金 Supported by the National Natural Science Foundation of China (20676145, U0633003), the National Basic Research Program of China (2009CB219504) and the Program for New Century Excellent Talents in University of the State Ministry of Education.
关键词 equilibrium condition HYDRATE step-heating sodium dodecyl sullate silica sand 平衡条件 二氧化碳 加热法 甲烷 物相 水合 测量 乙烷
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