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Flow enhancement of water-based nanoparticle dispersion through microscale sedimentary rocks

机译:水基纳米颗粒分散液通过微尺度沉积岩的流动增强

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Understanding and controlling fluids flow at the microscale is a matter of growing scientific and technological interest. Flow enhancements of water-based nanoparticle dispersions through microscale porous media are investigated through twelve hydrophilic sedimentary rocks with pore-throat radius between 1.2 and 10 μ m, which are quantitatively explained with a simple model with slip length correction for Darcy flow. Both as wetting phase, water exhibited no-slip Darcy flow in all cores; however, flow enhancement of nanoparticle dispersions can be up to 5.7 times larger than that of water, and it increases with the decreasing of pore-throat radius. The experimental data reveals characteristic slip lengths are of order 500 and 1000?nm for 3M? and HNPs-1 nanoparticles, respectively, independent of the lithology or nanoparticle concentration or shear rate. Meanwhile, the phenomenon of flow degradation is observed for HNPs-2 nanoparticles. These results explore the feasible application of using nanoparticle dispersions to control flow at the microscale.
机译:在微观尺度上理解和控制流体流动是日益增长的科学技术兴趣。通过十二个孔喉半径在1.2到10μm之间的亲水性沉积岩,研究了水基纳米颗粒分散体通过微米级多孔介质的流动增强作用,并通过具有滑动长度校正的简单模型对达西流进行了定量解释。在润湿阶段,水在所有岩心中都显示出防滑的达西流动。然而,纳米粒子分散液的流动增强作用可能是水的5.7倍,并且随着孔喉半径的减小而增加。实验数据表明,对于3M ?,特征滑移长度约为500和1000?nm。 HNPs-1和HNPs-1纳米颗粒分别与岩性或纳米颗粒浓度或剪切速率无关。同时,观察到HNPs-2纳米颗粒的流动降解现象。这些结果探索了使用纳米颗粒分散体在微观尺度上控制流量的可行应用。

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