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涂覆有岩石矿物的聚二甲基硅氧烷(PDMS)微流控器件的功能化

Functionalisation of Polydimethylsiloxane (PDMS)- Microfluidic Devices coated with Rock Minerals.

作者信息

Alzahid Yara A, Mostaghimi Peyman, Gerami Alireza, Singh Ankita, Privat Karen, Amirian Tammy, Armstrong Ryan T

机构信息

School of Minerals and Energy Resources Engineering, The University of New South Wales, Sydney, NSW, 2052, Australia.

Electron Microscope Unit, The University of New South Wales, Sydney, NSW, 2052, Australia.

出版信息

Sci Rep. 2018 Oct 19;8(1):15518. doi: 10.1038/s41598-018-33495-8.

Abstract

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 CO sequestration.

摘要

多孔岩石中的流体流动通常由毛细管驱动,因此,取决于岩石颗粒的表面特性,特别是流体所占据的角落和缝隙的连通性。传统的微流体制备技术无法提供对于模拟岩石中的多相流至关重要的连通缝隙通道。在此,通过用岩石矿物对聚二甲基硅氧烷(PDMS)进行功能化处理,制造出了具有角落和缝隙连通通道的地质材料微流控装置。展示了一种将岩石矿物附着到PDMS上的新颖制造工艺。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,将地质材料微流控装置与碳酸盐岩和砂岩进行了比较。基于扫描电子显微镜与能量色散X射线光谱法(SEM-EDS)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,不同地质材料装置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,如等效于储层岩石中发生的液桥断裂和角落流动机制。所提出的方法可用于可视化与地下工程应用相关的岩石-流体相互作用,如烃类采收和二氧化碳封存。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ae0e/6195554/eafe148a9c18/41598_2018_33495_Fig1_HTML.jpg

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