Université de Strasbourg, CNRS, EOST, ENGEES, ITES UMR 7063, 67000 Strasbourg, France
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: 595 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
489
77
29
595
27
29
32
HTML: 489
PDF: 77
XML: 29
Total: 595
Supplement: 27
BibTeX: 29
EndNote: 32
Views and downloads (calculated since 04 Aug 2023)
Cumulative views and downloads
(calculated since 04 Aug 2023)
Total article views: 439 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
334
77
28
439
27
28
31
HTML: 334
PDF: 77
XML: 28
Total: 439
Supplement: 27
BibTeX: 28
EndNote: 31
Views and downloads (calculated since 26 Feb 2024)
Cumulative views and downloads
(calculated since 26 Feb 2024)
Total article views: 156 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
155
0
1
156
1
1
HTML: 155
PDF: 0
XML: 1
Total: 156
BibTeX: 1
EndNote: 1
Views and downloads (calculated since 04 Aug 2023)
Cumulative views and downloads
(calculated since 04 Aug 2023)
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: 595 (including HTML, PDF, and XML)
Thereof 588 with geography defined
and 7 with unknown origin.
Total article views: 439 (including HTML, PDF, and XML)
Thereof 440 with geography defined
and -1 with unknown origin.
Total article views: 156 (including HTML, PDF, and XML)
Thereof 148 with geography defined
and 8 with unknown origin.
Vertical maps of seismic velocity reflect variations of subsurface porosity. We use such images to design the geometry of subsurface compartments delimited by velocity thresholds. The obtained patterns are inserted into a hydrogeological model to test the influence of random geometries, velocity thresholds, and hydraulic parameters on data estimated from the model: the depth of the groundwater and magnetic resonance sounding is a geophysical method sensitive to subsurface water content.
Vertical maps of seismic velocity reflect variations of subsurface porosity. We use such images...