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首页> 外文期刊>Scientific reports. >Functionalisation of Polydimethylsiloxane (PDMS)- Microfluidic Devices coated?with Rock Minerals
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Functionalisation of Polydimethylsiloxane (PDMS)- Microfluidic Devices coated?with Rock Minerals

机译:含岩石矿物的聚二甲基硅氧烷(PDMS)-微流体装置的功能化

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摘要

Fluid flow in porous rocks is commonly capillary driven and thus, dependent on the surface characteristics of rock grains and in particular the connectivity of corners and crevices in which fluids reside. Traditional microfluidic fabrication techniques do not provide a connected pathway of crevices that are essential to mimic multiphase flow in rocks. Here, geo-material microfluidic devices with connected pathways of corners and crevices were created by functionalising Polydimethylsiloxane (PDMS) with rock minerals. A novel fabrication process that provides attachment of rock minerals onto PDMS was demonstrated. The geo-material microfluidic devices were compared to carbonate and sandstone rocks by using energy dispersive X-ray spectroscopy, scanning electron microscopy (SEM), contact angle measurements, and a surface profilometer. Based on SEM coupled with energy-dispersive X-ray spectrometry (SEM-EDS) analyses, roughness measurements, contact angle, wettability, and roughness were comparable to real rocks. In addition, semivariograms showed that mineral deposition across the different geo-material devices was nearly isotropic. Lastly, important multiphase flow phenomena, such as snap-off and corner flow mechanisms, equivalent to those occurring in reservoir?rocks have been visualised. The presented approach can be used to visualise rock-fluid interactions that are relevant to subsurface engineering applications, such as hydrocarbon recovery and CO2 sequestration.
机译:多孔岩石中的流体流动通常是毛细管驱动的,因此,取决于岩石颗粒的表面特性,尤其取决于流体所驻留的拐角和缝隙的连通性。传统的微流体制造技术无法提供缝隙的连接路径,而缝隙对于模拟岩石中的多相流动是必不可少的。在这里,通过用岩石矿物功能化聚二甲基硅氧烷(PDMS)来创建具有角和缝隙连接路径的土工材料微流体装置。演示了一种新颖的制造工艺,该工艺可将岩石矿物附着到PDMS上。通过使用能量色散X射线光谱,扫描电子显微镜(SEM),接触角测量和表面轮廓仪,将土工材料微流体装置与碳酸盐岩和砂岩岩进行了比较。基于SEM和能量色散X射线光谱分析(SEM-EDS)的分析,粗糙度测量,接触角,润湿性和粗糙度与真实岩石相当。此外,半变异函数表明,在不同的地物设备上的矿物沉积几乎是各向同性的。最后,已经可视化了重要的多相流现象,例如折断和角流机制,与储层岩石中发生的现象相同。所提出的方法可用于可视化与地下工程应用(例如碳氢化合物回收和CO2固存)相关的岩液相互作用。

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