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与地下储氢(UHS)相关的岩心尺度非均质砂岩中[化学式:见原文]/水多相流的实验表征。

Experimental characterization of [Formula: see text]/water multiphase flow in heterogeneous sandstone rock at the core scale relevant for underground hydrogen storage (UHS).

作者信息

Boon Maartje, Hajibeygi Hadi

机构信息

Faculty of Civil Engineering and Geosciences, Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands.

出版信息

Sci Rep. 2022 Aug 26;12(1):14604. doi: 10.1038/s41598-022-18759-8.

Abstract

Geological porous reservoirs provide the volume capacity needed for large scale underground hydrogen storage (UHS). To effectively exploit these reservoirs for UHS, it is crucial to characterize the hydrogen transport properties inside porous rocks. In this work, for the first time in the community, we have performed [Formula: see text]/water multiphase flow experiments at core scale under medical X-ray CT scanner. This has allowed us to directly image the complex transport properties of [Formula: see text] when it is injected or retracted from the porous rock. The important effective functions of capillary pressure and relative permeability are also measured, for both drainage and imbibition. The capillary pressure measurements are combined with MICP data to derive a receding contact angle for the [Formula: see text]/water/sandstone rock system. The rock core sample is a heterogeneous Berea sandstone (17 cm long and 3.8 cm diameter). Our investigation reveals the interplay between gravitational, capillary, and viscous forces. More specifically, it illustrates complex displacement patterns in the rock, including gravity segregation, enhancement of spreading of [Formula: see text] due to capillary barriers, and the formation of fingers/channel during imbibition which lead to significant trapping of hydrogen. These findings shed new light on our fundamental understanding of the transport characteristics of [Formula: see text]/water relevant for UHS.

摘要

地质多孔储层为大规模地下氢存储(UHS)提供了所需的容积。为了有效地利用这些储层进行地下氢存储,表征多孔岩石内部的氢传输特性至关重要。在这项工作中,我们在该领域首次在医学X射线计算机断层扫描(CT)扫描仪下进行了核心尺度的氢气/水多相流实验。这使我们能够直接成像氢气注入或从多孔岩石中抽出时的复杂传输特性。同时还测量了排水和吸水过程中毛细管压力和相对渗透率的重要有效函数。将毛细管压力测量结果与压汞法(MICP)数据相结合,得出氢气/水/砂岩系统的后退接触角。岩芯样品是一种非均质的贝雷亚砂岩(长17厘米,直径3.8厘米)。我们的研究揭示了重力、毛细管力和粘性力之间的相互作用。更具体地说,它说明了岩石中复杂的驱替模式,包括重力分异、由于毛细管屏障导致氢气扩散增强,以及吸水过程中形成指进/通道,从而导致大量氢气滞留。这些发现为我们对与地下氢存储相关的氢气/水传输特性的基本理解提供了新的思路。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5a07/9418204/97c13c7cbec3/41598_2022_18759_Fig1_HTML.jpg

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