Institut für Geometrie und Praktische Mathematik, RWTH Aachen University, Templergraben 55, 52056 Aachen, Germany
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 604 (including HTML, PDF, and XML)
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593
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604
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Total: 604
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Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 48 (including HTML, PDF, and XML)
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40
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Total: 48
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Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
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Total article views: 556 (including HTML, PDF, and XML)
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553
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556
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Total: 556
BibTeX: 0
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Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
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Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 604 (including HTML, PDF, and XML)
Thereof 588 with geography defined
and 16 with unknown origin.
Total article views: 48 (including HTML, PDF, and XML)
Thereof 48 with geography defined
and 0 with unknown origin.
Total article views: 556 (including HTML, PDF, and XML)
Thereof 540 with geography defined
and 16 with unknown origin.
Understanding porous fluid flow is key for many geology applications. Traditional methods cannot resolve cases with sharp discontinuities in hydraulic/mechanical properties across those layers. Here we present a new space-time method that can handle such discontinuities. This approach is coupled with trace element transport. Our study reveals that the layering of rocks significantly influences the formation of fluid-rich channels and the material distribution adjacent to discontinuities.
Understanding porous fluid flow is key for many geology applications. Traditional methods cannot...