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: 4,106 (including HTML, PDF, and XML)
HTML
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XML
Total
BibTeX
EndNote
3,620
314
172
4,106
113
151
HTML: 3,620
PDF: 314
XML: 172
Total: 4,106
BibTeX: 113
EndNote: 151
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 2,345 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,867
314
164
2,345
113
151
HTML: 1,867
PDF: 314
XML: 164
Total: 2,345
BibTeX: 113
EndNote: 151
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 1,761 (including HTML, PDF, and XML)
HTML
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BibTeX
EndNote
1,753
0
8
1,761
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0
HTML: 1,753
PDF: 0
XML: 8
Total: 1,761
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: 4,106 (including HTML, PDF, and XML)
Thereof 4,044 with geography defined
and 62 with unknown origin.
Total article views: 2,345 (including HTML, PDF, and XML)
Thereof 2,286 with geography defined
and 59 with unknown origin.
Total article views: 1,761 (including HTML, PDF, and XML)
Thereof 1,758 with geography defined
and 3 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...