磁导率
体积热力学
相对渗透率
矿物学
地质学
瞬态(计算机编程)
石油工程
机械
材料科学
岩土工程
化学
物理
多孔性
热力学
计算机科学
膜
生物化学
操作系统
出处
期刊:Spe Formation Evaluation
日期:1997-03-01
卷期号:12 (01): 19-25
被引量:357
摘要
Summary Laboratory pulse-decay measurements using a gas or liquid are effective for determining the permeability of rocks in the range from 0.1 md to 0.01 μd. The actual measurement time with this pressure-transient technique is fairly short, but pressure pre-equilibration sometimes requires hours. This paper shows how the total time can be reduced significantly, especially if the sample's pore volume (PV) is measured independently or estimated accurately. Permeability is calculated from "late-time" measurements. Strategies for minimizing errors and increasing sample throughput are presented.
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