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: 785 (including HTML, PDF, and XML)
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EndNote
627
121
37
785
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46
HTML: 627
PDF: 121
XML: 37
Total: 785
Supplement: 38
BibTeX: 40
EndNote: 46
Views and downloads (calculated since 04 Aug 2023)
Cumulative views and downloads
(calculated since 04 Aug 2023)
Total article views: 629 (including HTML, PDF, and XML)
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472
121
36
629
38
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45
HTML: 472
PDF: 121
XML: 36
Total: 629
Supplement: 38
BibTeX: 39
EndNote: 45
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)
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155
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1
156
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HTML: 155
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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: 785 (including HTML, PDF, and XML)
Thereof 778 with geography defined
and 7 with unknown origin.
Total article views: 629 (including HTML, PDF, and XML)
Thereof 629 with geography defined
and 0 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...