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: 3,517 (including HTML, PDF, and XML)
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3,251
184
82
3,517
51
75
HTML: 3,251
PDF: 184
XML: 82
Total: 3,517
BibTeX: 51
EndNote: 75
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 1,837 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,577
184
76
1,837
51
75
HTML: 1,577
PDF: 184
XML: 76
Total: 1,837
BibTeX: 51
EndNote: 75
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 1,680 (including HTML, PDF, and XML)
HTML
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BibTeX
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1,674
0
6
1,680
0
0
HTML: 1,674
PDF: 0
XML: 6
Total: 1,680
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: 3,517 (including HTML, PDF, and XML)
Thereof 3,483 with geography defined
and 34 with unknown origin.
Total article views: 1,837 (including HTML, PDF, and XML)
Thereof 1,803 with geography defined
and 34 with unknown origin.
Total article views: 1,680 (including HTML, PDF, and XML)
Thereof 1,680 with geography defined
and 0 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...