1) sheet conduction model
导电板模型
2) electric conduction model
导电模型
1.
Based on application of three pore water electric conduction models and the needs of reservoir fine evaluation, a numerical solution for the three pore components (free fluid pore, micro pore, and clay water) has been given in this paper.
针对三孔隙水导电模型的应用和储层精细评价的需要,提出了三孔隙组分(自由流体孔隙、微孔隙、粘土水)的数值解法,并根据塔里木盆地北部地区部分低阻层的储层物性特征,利用岩心分析数据与测井数据建立了一组三孔隙组分的地区统计关系式,较好地满足了生产的需要。
3) conductivity model
电导模型
4) conductivity model
电导率模型
1.
Based on the idea that the bedded mud and disperse shaly sand can be electrically conduct in parallel, the conduction of disperse shaly sand can be described with the double eletrode layer conductivity model proposed by V S Afanasyev, etc.
基于层状泥质和分散泥质砂岩并联导电的观点,分散泥质砂岩的导电可采用VSAfanasyev等人提出的双电层电导率模型进行描述,从而建立考虑分散和层状泥质同时存在的混合泥质砂岩通用双电层电导率模型,该模型是关于含水饱和度的隐函数方程。
2.
An experimental comparison is done on the accuracy of the three conductivity models.
从分析泥质砂岩双电层导电机理出发,考察了W-S、D-W、S-B这3种泥质砂岩双电层电导率模型在理论上的优缺点,得出了S-B模型在理论上最完善、D-W模型较完善的结论。
5) ionic of conductivity model
离子导电模型
6) generalized conductivity model
通用电导率模型
补充资料：导电
1.让电流通过。一般金属都能导电。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条