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含水饱和度指数n的理论及实验
引用本文:孙德明 褚人杰. 含水饱和度指数n的理论及实验[J]. 石油学报, 1994, 15(4): 66-72. DOI: 10.7623/syxb199404009
作者姓名:孙德明 褚人杰
作者单位:1. 中科院地球物理研究所;2. 石油勘探开发科学研究院
摘    要:
含水饱和度指数n是用电阻率评价地层流体性质的重要参数.本文通过理论推导,得出了影响n指数的几大因素,分别为地层水电阻率Rw、阳离子交换容量Qv、含水饱和度Sw以及地层因素F.并发现砂岩影响n的因素是F和Rw,而泥质砂岩则分别是Rw,QvF.以上某些结论已在实验中得到验证.

关 键 词:含水饱和度  指数  地层  水电阻率  [阳离子交换容量]  
收稿时间:1992-10-20

A THEORETICAL AND EXPERIMENTAL STUDY FOR SATURATION EXPONENT, n
Sun Deming. A THEORETICAL AND EXPERIMENTAL STUDY FOR SATURATION EXPONENT, n[J]. Acta Petrolei Sinica, 1994, 15(4): 66-72. DOI: 10.7623/syxb199404009
Authors:Sun Deming
Affiliation:1. Institute of Ge0physics, Chinese Academy of Sciences;2. Scientific Research Institute of Petroleum Exploration and Development, Beijing
Abstract:
This paper has given a formula to calculate saturation exponent "n".A few of effectsfactors(Rw,Ow,Sw,F)on "n"is deduced from the formula.The main effects are F(toutu-osity)and Rw(formation water resistivity)for clean sand and Rw,Qw(cation exchange capacity) and F for shaly sand Some results have been verified from a laboratory study.
Keywords:water saturation exponent stratum water resistivity[cation exchange capability]  
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