Microstructure of a compacted silt
This paper presents a qualitative and quantitative study of the microstructure of a compacted silt, carried out using a scanning electron microscope and mercury intrusion pore size distribution measurements. Samples have been statically compacted at three water contents: on the dry side of the stand...
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| Published in: | Canadian geotechnical journal Vol. 33; no. 1; pp. 150 - 158 |
|---|---|
| Main Authors: | , , , |
| Format: | Journal Article |
| Language: | English |
| Published: |
Ottawa, Canada
NRC Research Press
25-03-1996
National Research Council of Canada |
| Subjects: | |
| Online Access: | Get full text |
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| Abstract | This paper presents a qualitative and quantitative study of the microstructure of a compacted silt, carried out using a scanning electron microscope and mercury intrusion pore size distribution measurements. Samples have been statically compacted at three water contents: on the dry side of the standard Proctor optimum water content, at the optimum, and on the wet side. The wet sample has a matrix type structure, with a clayey fraction filling the voids and adhering to the silt-sized grains, whereas the other samples display a structure characterized by a skeleton made of silt grain aggregates linked together by clayey bidges. The distribution of water and air within the microstructure of the compacted soil is described for each of the three compaction states.
Key words: compacted soil, microstructure, scanning electron microscope, pore size distribution, mercury intrusion, clay hydration. |
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| AbstractList | This paper presents a qualitative and quantitative study of the microstructure of a compacted silt, carried out using a scanning electron microscope and mercury intrusion pore size distribution measurements. Samples have been statically compacted at three water contents: on the dry side of the standard Proctor optimum water content, at the optimum, and on the wet side. The wet sample has a matrix type structure, with a clayey fraction filling the voids and adhering to the silt-sized grains, whereas the other samples display a structure characterized by a skeleton made of silt grain aggregates linked together by clayey bidges. The distribution of water and air within the microstructure of the compacted soil is described for each of the three compaction states.
Key words: compacted soil, microstructure, scanning electron microscope, pore size distribution, mercury intrusion, clay hydration. |
| Abstract_FL | On présente les résultats d'une étude à la fois qualitative et quantitative, menée en microscopie électronique à balayage et en porosimétrie au mercure, de la microstructure d'un limon compacté statiquement à l'optimum Proctor, du coté humide et du coté sec. Alors que l'échantillon humide présente une structure matricielle avec une phase argileuse emplissant l'ensemble des vides et tapissant les grains, les deux autres échantillons ont une structure caractérisée par un squelette formé d'agrégats granulaires avec des liens argileux. On identifie la répartition de l'eau et de l'air au sein de la microstructure, dans les trois cas.
Mots clés : sol compacté, microstructure, microscopie électronique à balayage, granulométrie, intrusion au mercure, hydratation de l'argile. |
| Author | Cui, Yu-Jun Audiguier, Martine Delage, Pierre Howat, Michael D |
| Author_xml | – sequence: 1 givenname: Pierre surname: Delage fullname: Delage, Pierre – sequence: 2 givenname: Martine surname: Audiguier fullname: Audiguier, Martine – sequence: 3 givenname: Yu-Jun surname: Cui fullname: Cui, Yu-Jun – sequence: 4 givenname: Michael D surname: Howat fullname: Howat, Michael D |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=3033709$$DView record in Pascal Francis |
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| CODEN | CGJOAH |
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| Title | Microstructure of a compacted silt |
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