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作 者:林梅钦[1] 李明远[1] 彭勃[1] 纪淑玲[1] 吴肇亮[1]
机构地区:[1]石油大学化工学部,北京100083
出 处:《高分子学报》1999年第5期606-611,共6页Acta Polymerica Sinica
摘 要:用低浓度不同分子量的部分水解聚丙烯酰胺( H P A M) 和柠檬酸铝制备了胶态分散凝胶( C D G) ,并用奥氏粘度计、超细粒度分析仪、岩芯流动实验对 C D G 的性质进行了研究.结果表明, C D G 的粘度比 H P A M 粘度低,粒径在450 ~520n m 之间.岩芯流动实验结果表明, C D G 能够使岩芯的流动阻力大幅度增加,且在岩芯中达到同样的流动阻力所需通过 C D G 的体积与形成 C D G 的 H P A M 的分子量、浓度及岩芯渗透率有关.The colloidal dispersion gels ( C D G) were prepared by low concentration partiallyhydrolyzed polyacrylamide with different molecular weights and aluminum citrate. Theproperties of C D G were investigated by the Oswald capillary viscometer,ultrafine sizeanalyzer and theflow experiment. The resultsshowedthatthe viscosity of C D Gislowerthanthat of hydrolyzed polyacrylamide ( H P A M) and the viscosity of C D G decreases withincreasing the reaction time. The particle diameter of C D Gwith H P A M molecular weightsof4 ×106 and 1 4 ×107 was determined to be 460 and 510 nm , respectively . The flowresistance of C D G, which generally increased with increasing H P A M molecular weight andconcentration ,is much larger than that of H P A Msolutionsin the core . The flow resistanceofthe C D Gin lower permeability core was increased more quick than that of the C D Ginhigher permeability core. The flow resistance of C D Gin the core was associated with themoleculare weight and concentration of H P A Mand the permeability ofthe core . C D Gis abletoincrease the flow resistancein the core effectively .
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