研究具有持久同源性的粗糙单一断裂渗透率

IF 3.2 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Solid Earth Pub Date : 2024-03-13 DOI:10.5194/se-15-353-2024
Marco Fuchs, Anna Suzuki, Togo Hasumi, Philipp Blum
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引用次数: 0

摘要

摘要岩石裂缝的渗透性是地下流动过程的一个重要参数。在过去的几十年中,人们开发了不同的方法来研究裂缝的渗透性,如流经实验、数值流动模拟或经验方程。近年来,持续同源性拓扑方法也被用于估算断裂网络和多孔岩石的渗透率,但尚未用于粗糙的单一断裂。因此,我们将持久同源性分析应用于十亿分米尺度的粗糙砂岩垫层节理。为了研究粗糙度的影响,我们创建了三个不同的数据集来进行分析:(1) 200 微米、(2) 100 微米和 (3) 50 微米分辨率。然后将所有估算的渗透率与实验性空气渗透仪测量和数值流动模拟得出的数值进行比较。结果表明,持续同源性分析能够估算单一裂缝的渗透率,尽管与传统方法相比,它往往会略微高估渗透率。之前使用多孔介质进行的研究也显示了同样的高估趋势。此外,还比较了持久同源性分析、空气渗透仪测量和数值流动模拟所花费的时间,结果表明持久同源性分析也是一种可接受的替代方法。
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Investigating rough single-fracture permeabilities with persistent homology
Abstract. The permeability of rock fractures is a crucial parameter for flow processes in the subsurface. In the last few decades, different methods were developed to investigate on permeability in fractures, such as flow-through experiments, numerical flow simulations, or empirical equations. In recent years, the topological method of persistent homology was also used to estimate the permeability of fracture networks and porous rocks but not for rough single fractures yet. Hence, we apply persistent homology analysis on a decimetre-scale, rough sandstone bedding joint. To investigate the influence of roughness, three different data sets are created to perform the analysis: (1) 200 µm, (2) 100 µm, and (3) 50 µm resolutions. All estimated permeabilities were then compared to values derived by experimental air permeameter measurements and numerical flow simulation. The results reveal that persistent homology analysis is able to estimate the permeability of a single fracture, even if it tends to slightly overestimate permeabilities compared to conventional methods. Previous studies using porous media showed the same overestimation trend. Furthermore, the expenditure of time for persistent homology analysis, as well as air permeameter measurements and numerical flow simulation, was compared, which showed that persistent homology analysis can be also an acceptable alternative method.
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来源期刊
Solid Earth
Solid Earth GEOCHEMISTRY & GEOPHYSICS-
CiteScore
6.90
自引率
8.80%
发文量
78
审稿时长
4.5 months
期刊介绍: Solid Earth (SE) is a not-for-profit journal that publishes multidisciplinary research on the composition, structure, dynamics of the Earth from the surface to the deep interior at all spatial and temporal scales. The journal invites contributions encompassing observational, experimental, and theoretical investigations in the form of short communications, research articles, method articles, review articles, and discussion and commentaries on all aspects of the solid Earth (for details see manuscript types). Being interdisciplinary in scope, SE covers the following disciplines: geochemistry, mineralogy, petrology, volcanology; geodesy and gravity; geodynamics: numerical and analogue modeling of geoprocesses; geoelectrics and electromagnetics; geomagnetism; geomorphology, morphotectonics, and paleoseismology; rock physics; seismics and seismology; critical zone science (Earth''s permeable near-surface layer); stratigraphy, sedimentology, and palaeontology; rock deformation, structural geology, and tectonics.
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