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: 3,571 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
3,291
193
87
3,571
52
78
HTML: 3,291
PDF: 193
XML: 87
Total: 3,571
BibTeX: 52
EndNote: 78
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 1,888 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,615
193
80
1,888
52
78
HTML: 1,615
PDF: 193
XML: 80
Total: 1,888
BibTeX: 52
EndNote: 78
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 1,683 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,676
0
7
1,683
0
0
HTML: 1,676
PDF: 0
XML: 7
Total: 1,683
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: 3,571 (including HTML, PDF, and XML)
Thereof 3,521 with geography defined
and 50 with unknown origin.
Total article views: 1,888 (including HTML, PDF, and XML)
Thereof 1,839 with geography defined
and 49 with unknown origin.
Total article views: 1,683 (including HTML, PDF, and XML)
Thereof 1,682 with geography defined
and 1 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...