Institut für Geometrie und Praktische Mathematik, RWTH Aachen University, Templergraben 55, 52056 Aachen, Germany
Viewed
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: 1,758 (including HTML, PDF, and XML)
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EndNote
1,606
102
50
1,758
23
45
HTML: 1,606
PDF: 102
XML: 50
Total: 1,758
BibTeX: 23
EndNote: 45
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 1,202 (including HTML, PDF, and XML)
HTML
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BibTeX
EndNote
1,053
102
47
1,202
23
45
HTML: 1,053
PDF: 102
XML: 47
Total: 1,202
BibTeX: 23
EndNote: 45
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 556 (including HTML, PDF, and XML)
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553
0
3
556
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Total: 556
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
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: 1,758 (including HTML, PDF, and XML)
Thereof 1,721 with geography defined
and 37 with unknown origin.
Total article views: 1,202 (including HTML, PDF, and XML)
Thereof 1,181 with geography defined
and 21 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...