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塔里木盆地油气层低阻成因实验研究(Ⅱ) 被引量:10

Experimental Study on the Genesis of Low Resistivity Pay Zone in North Region of Tarim Basin.
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摘要 毛志强,朱卫红,汪如军.塔里木盆地油气层低阻成因实验研究(Ⅱ).测井技术,1999,23(6):404~410对塔里木盆地塔北地区低阻油气层的实验数据进行了全面分析。根据实验数据,提出用后三点法确定Co- Cw 实验关系基本参数。数据分析表明,指数m与温度及溶液矿化度无关。根据实验数据确定了阳离子当量电导B值与地层温度和溶液矿化度(或电阻率)关系图版。电阻率指数与含水饱和度实验结果证实了油层阳离子交换量随含水饱和度降低而增加的理论推断,指数n与温度及溶液矿化度无相关关系。塔里木盆地塔北地区低阻油气层表现出了与Waxm an-Sm its方程类似的规律,但阳离子当量电导B值这一重要参数与Waxm an 等人发表的结果又有一定差别。 This part of the paper presents the detailed data analysis of the experimental investigation on the genesis of low resistivity pay zone in northern region of Tarim Basin. A three point method is proposed to define the linear segment of C o- C w relation.The measurements show that both m and n  are independent of the additional conductivity of clays and the equivalent cation exchange capacity of oil bearing zone increases as brine saturation decreases, which agrees well with what Waxman et al.concluded in seventies. The equivalent conductance of the counterions as a function of brine resistivity and temperature is determined based on lab measurements of ten samples at the conditions of four temperatures and six solution salinities.The data analysis demonstrates that Waxman and Smits formula can be well used to describe the samples resistivity properties.Since the equivalent conductance of the counterions is different from that Waxman and Thomas presented,it is believed that the equivalent conductance of the counterions is not independent of reservoir. Subject Terms:Tarim basin resistivity clay mineral lab testing cation exchange capacity water saturation
出处 《测井技术》 CAS CSCD 北大核心 1999年第6期404-410,共7页 Well Logging Technology
基金 中国博士后基金会 中国石油天然气集团公司"九五"科技攻关项目
关键词 塔里木盆地 电阻率 含水饱和度 油气层 低阻成因 Tarim basin resistivity clay mineral lab testing cation exchange capacity water saturation
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参考文献1

  • 1毛志强.塔里木盆地油气低阻在因实验研究(Ⅰ)[J].测井技术,1999,23(4).

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