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: 3,983 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
3,540
284
159
3,983
107
145
HTML: 3,540
PDF: 284
XML: 159
Total: 3,983
BibTeX: 107
EndNote: 145
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 2,245 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,809
284
152
2,245
107
145
HTML: 1,809
PDF: 284
XML: 152
Total: 2,245
BibTeX: 107
EndNote: 145
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 1,738 (including HTML, PDF, and XML)
HTML
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XML
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BibTeX
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1,731
0
7
1,738
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0
HTML: 1,731
PDF: 0
XML: 7
Total: 1,738
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: 3,983 (including HTML, PDF, and XML)
Thereof 3,921 with geography defined
and 62 with unknown origin.
Total article views: 2,245 (including HTML, PDF, and XML)
Thereof 2,186 with geography defined
and 59 with unknown origin.
Total article views: 1,738 (including HTML, PDF, and XML)
Thereof 1,735 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...