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地层多孔介质中地层水蒸发盐析研究进展 被引量:1

Research progress of formation water evaporation and salting out in formation porous media
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摘要 近年来地下储气库发展迅速,为了解决地下储气库注采过程中地层出现的结盐问题,针对储气库周期性运行过程中注气期和采气期两个阶段,研究地层的温度和压力等条件发生变化时造成地层存在不同程度的结盐现象,得出地下储气库结盐主要原因是由于高矿化度的地层水蒸发作用导致盐析结晶。对地层多孔介质内水分蒸发扩散热力学条件方面研究进行了总结。 In recent years,underground gas storage has developed rapidly.In order to solve the problem of salt formation in underground gas storage during injection and production,the temperature and pressure of stratum is studied for the two phases of gas injection and gas production during the periodic operation of the gas storage.When the conditions such as temperature and pressure change,there are different degrees of salt formation in the formation.It is concluded that the main reason for salt formation in underground gas storage is the salt precipitation and crystallization due to the evaporation of formation water with high salinity.Therefore,this paper summarizes the research on the thermodynamic conditions of water evaporation and diffusion in the formation porous media.
作者 王春燕 吴宇航 王雨薇 张静 文守成 WANG Chun-yan;WU Yu-hang;WANG Yu-wei;ZHANG Jing;WEN Shou-cheng(School of Petroleum Engineering,Yangtze University,Wuhan 430100 China;PetroChina North China Oilfield Exploration and Development Research Institute,Renqiu 062552,China;No.1 Drilling Company,Sinopec Jianghan Petroleum Engineering Co.,Ltd.,Qianjiang 43100,China;Zhanjiang Branch,CNOOC Energy Tech-Drilling&Production Co.,Ltd.,Zhanjiang 524057,China)
出处 《应用化工》 CAS CSCD 北大核心 2020年第S02期261-265,共5页 Applied Chemical Industry
关键词 多孔介质 地层水蒸发 盐析热力学 结晶动力学 孔隙几何尺寸 porous media formation water evaporation salting out thermodynamics crystallization kinetics pore geometry
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