Relating wave frequency and pore fluid homogeneity in quasi-saturated sands

P-wave velocity is regularly proposed as a proxy for water saturation when studying quasisaturated soils. However, several authors have underlined that this velocity can only be reliably correlated to water saturation if the pore fluid is “homogeneous”. Using bender elements to measure compression w...

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Main Authors: Flood-Page Guillaume, Boutonnier Luc, Pereira Jean-Michel
Format: Article
Language:English
Published: EDP Sciences 2023-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_03005.pdf
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author Flood-Page Guillaume
Boutonnier Luc
Pereira Jean-Michel
author_facet Flood-Page Guillaume
Boutonnier Luc
Pereira Jean-Michel
author_sort Flood-Page Guillaume
collection DOAJ
description P-wave velocity is regularly proposed as a proxy for water saturation when studying quasisaturated soils. However, several authors have underlined that this velocity can only be reliably correlated to water saturation if the pore fluid is “homogeneous”. Using bender elements to measure compression wave velocity in quasi-saturated Fontainebleau sand, we show it is highly sensitive to both saturation and frequency. The characteristic length of pore pressure diffusion is used to explain the link between frequency, gas distribution and P-wave velocity. This criterion is shown to be fairly reliable for assessing the homogeneity of a pore fluid distribution in quasi-saturated Fontainebleau sand.
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spelling doaj.art-a3a77f85c68740eba8e38c51993296fc2023-05-02T09:28:19ZengEDP SciencesE3S Web of Conferences2267-12422023-01-013820300510.1051/e3sconf/202338203005e3sconf_unsat2023_03005Relating wave frequency and pore fluid homogeneity in quasi-saturated sandsFlood-Page Guillaume0Boutonnier Luc1Pereira Jean-Michel2EgisEgisNavier, Ecole des Ponts, Univ Gustave Eiffel, CNRSP-wave velocity is regularly proposed as a proxy for water saturation when studying quasisaturated soils. However, several authors have underlined that this velocity can only be reliably correlated to water saturation if the pore fluid is “homogeneous”. Using bender elements to measure compression wave velocity in quasi-saturated Fontainebleau sand, we show it is highly sensitive to both saturation and frequency. The characteristic length of pore pressure diffusion is used to explain the link between frequency, gas distribution and P-wave velocity. This criterion is shown to be fairly reliable for assessing the homogeneity of a pore fluid distribution in quasi-saturated Fontainebleau sand.https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_03005.pdf
spellingShingle Flood-Page Guillaume
Boutonnier Luc
Pereira Jean-Michel
Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
E3S Web of Conferences
title Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
title_full Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
title_fullStr Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
title_full_unstemmed Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
title_short Relating wave frequency and pore fluid homogeneity in quasi-saturated sands
title_sort relating wave frequency and pore fluid homogeneity in quasi saturated sands
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_03005.pdf
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