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: 1,348 (including HTML, PDF, and XML)
HTML
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BibTeX
EndNote
1,243
70
35
1,348
20
31
HTML: 1,243
PDF: 70
XML: 35
Total: 1,348
BibTeX: 20
EndNote: 31
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 792 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
690
70
32
792
20
31
HTML: 690
PDF: 70
XML: 32
Total: 792
BibTeX: 20
EndNote: 31
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)
HTML
PDF
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BibTeX
EndNote
553
0
3
556
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HTML: 553
PDF: 0
XML: 3
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: 1,348 (including HTML, PDF, and XML)
Thereof 1,327 with geography defined
and 21 with unknown origin.
Total article views: 792 (including HTML, PDF, and XML)
Thereof 787 with geography defined
and 5 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...