西南石油大学学报(自然科学版) ›› 2012, Vol. 34 ›› Issue (1): 134-140.

• 石油与天然气工程 • 上一篇    下一篇

高温高压气藏地层水结垢规律实验研究

李丽1,刘建仪1,张威2,张广东1,张俊良3   

  1. 1.“油气藏地质及开发工程”国家重点实验室 西南石油大学,四川成都610500;2. 昆明理工大学国土资源学院,云南昆明650093;3. 中国石油西南油气田分公司川东北气矿,四川达州635000
  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:2012-02-01 发布日期:2012-02-01

Experimental Research for Gas Feild Water’s Scaling Rule Under theCondition of High Pressure and High Temperature

Li li1, Liu Jianyi1, Zhang Wei2, Zhang Guangdong1, Zhang Junliang3   

  1. 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Southwest Petroleum University,Chengdu,Sichuan 610500,China2. Technology Land Resources Institute,Kunming University of Science,Kunming,Yunnan 650093,China3. Southwest oil and gas field,Sichua Northeastern Gas Company,Dazhou,Sichuan 635000,China
  • Received:1900-01-01 Revised:1900-01-01 Online:2012-02-01 Published:2012-02-01

摘要: 针对目前国内外缺乏直接检测高温高压地层水离子含量设备的问题,设计了测试高温、高压条件下实际气藏
流体中地层水离子含量及结垢量的静态实验。采用实际气藏流体进行了高温高压PVT 分析及离子含量检测实验,测
试不同条件下水中气、气中水含量及地层水离子组成,确定地层流体结垢量,综合研究了高温高压地层水相态变化和
离子含量的变化规律及其内在联系。结果表明:随地层压力降低,天然气在水中的溶解度降低,水的蒸发加剧,地层水
矿化度升高,结垢趋势增加。一定的低压高温条件下,地层流体中的无机盐结垢且结垢量随压力降低而增加,随温度
降低而减小;实际地层流体结垢量比脱气地层水低且结垢量随温度压力的变化趋势更为明显。

关键词: 高温高压, 地层水, 离子含量, 赋存状态, 结垢

Abstract: To solve the lack of equipment that can directly measure formation water’s ion content in the condition of high
temperature and high pressure at home and abroad. The static experiment for test ion content and scaling amount in formation
fluid under the condition of high temperature and high pressure was made. PVT analysis for the actual gas field’s fluid of
high temperature and high pressure and ion content detection experiments were carried on in this paper. Water content in
gas,amount of gas dissolved in water and the icon formation content in water are tested,scaling amount of formation fluid was
firmed. The change rule of gas and water’s phase state and ionic content have been studied comprehensively,the internal relation
influence was analyzed. The results show that quantity of dissolved gas in water reduces with formation pressure decreasing,
the evaporation water to natural gas formation intensifies,electrolyticion’s concentration and salinity increases,and the scaling
trends increase. In certain low pressure and high temperature conditions,the inorganic salt in formation fluid began scaling. The
scaling quantity increases with experiment pressure increasing,and decreases with the experimental temperature decreasing.
Scaling quantity of the under actual production condition is lower than that of the degassing formation water,and change trend
of scaling quantity with temperature and pressure is more obvious.

Key words: high temperature and high pressure, ion content, formation water, occurrence state, scaling

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