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: 696 (including HTML, PDF, and XML)
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565
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696
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HTML: 565
PDF: 99
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Total: 696
Supplement: 31
BibTeX: 34
EndNote: 39
Views and downloads (calculated since 04 Aug 2023)
Cumulative views and downloads
(calculated since 04 Aug 2023)
Total article views: 540 (including HTML, PDF, and XML)
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410
99
31
540
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HTML: 410
PDF: 99
XML: 31
Total: 540
Supplement: 31
BibTeX: 33
EndNote: 38
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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156
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Total: 156
BibTeX: 1
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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: 696 (including HTML, PDF, and XML)
Thereof 691 with geography defined
and 5 with unknown origin.
Total article views: 540 (including HTML, PDF, and XML)
Thereof 540 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...