摘要
实验研究表明,不管是干燥岩石还是含束缚水岩石,低渗透砂岩储层的应力敏感性是客观存在的,而且这种应力敏感性对储层渗透率造成的伤害不可忽视。随着有效压力的升高,渗透率是逐渐降低的,并且在有效压力升高的早期降低的幅度最明显,在后期则趋于平缓。而在有效压力恢复过程中,渗透率不能恢复到原来大小,即应力敏感对渗透率的伤害具有永久性。通过干燥样品与含束缚水样品的对照实验数据及分析表明,含束缚水样品的应力敏感性更明显,即应力造成含束缚水样品的渗透率降低幅度更大、伤害程度更大。
By the experiment study, the stress-sensitivity of low-permeability gas reservoirs is being existed objectively. And the hurt for reservoir's permeability can't be ignored. The permeability descend by the effective stress ascend, and descend range in earlier period is most significantly and gently in later period. But the permeability can not restore by descend the effective stress, so the hurt for permeability is permanence. Compare to the dry rock samples, the samples with irreducible water have more significantly stress sensitivity, or more seriously hurt for permeability.
出处
《天然气地球科学》
EI
CAS
CSCD
2004年第3期227-229,共3页
Natural Gas Geoscience
基金
国家重点基础研究发展规划项目子课题"气藏变形介质渗流规律研究"(编号:2001CB209108)资助.
关键词
应力敏感
气藏
束缚水
渗透率
岩石
Key words:Stress sensitivity
Gas reservoir
Irreducible water
Permeability
Rock.