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: 3,617 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
3,321
208
88
3,617
53
81
HTML: 3,321
PDF: 208
XML: 88
Total: 3,617
BibTeX: 53
EndNote: 81
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads
(calculated since 15 Jan 2025)
Total article views: 1,930 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,641
208
81
1,930
53
81
HTML: 1,641
PDF: 208
XML: 81
Total: 1,930
BibTeX: 53
EndNote: 81
Views and downloads (calculated since 04 Nov 2025)
Cumulative views and downloads
(calculated since 04 Nov 2025)
Total article views: 1,687 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,680
0
7
1,687
0
0
HTML: 1,680
PDF: 0
XML: 7
Total: 1,687
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: 3,617 (including HTML, PDF, and XML)
Thereof 3,557 with geography defined
and 60 with unknown origin.
Total article views: 1,930 (including HTML, PDF, and XML)
Thereof 1,872 with geography defined
and 58 with unknown origin.
Total article views: 1,687 (including HTML, PDF, and XML)
Thereof 1,685 with geography defined
and 2 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...