Propriétés des argiles marines de grande profondeur
Identifieur interne : 000349 ( PascalFrancis/Corpus ); précédent : 000348; suivant : 000350Propriétés des argiles marines de grande profondeur
Auteurs : J.-L. Favre ; M. HattabSource :
- Revue française de géotechnique [ 0181-0529 ] ; 2006.
Descripteurs français
- Pascal (Inist)
English descriptors
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Abstract
A 14 meter long deepwater marine clay coree, from the Gulf of Guinea, is analysed with a 16.7 cm step and its behaviour compared on one hand, with the reference behaviour of the remoulded normally consolidated mineral clays established by Biarez et Favre (1975, 1977), and on the other hand with intrinsic compression (ICL) line proposed by Burland (1990). The index parameters wL, wP, MBV, wnat and the mechanical parameters cu, Cc, Cs, σc, OCR are highlighted in this experimental study. The thinness of the step, the agreement of the profiles, reveals a complex genesis as well as the specificities of this natural marine smectite such as: the void ratio of sedimentation, sensitivity, and a apparent « overconsolidation » which translates a physico-chemical cohesion type.
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Format Inist (serveur)
| NO : | PASCAL 07-0187350 INIST |
|---|---|
| FT : | Propriétés des argiles marines de grande profondeur |
| ET : | (Properties of deepwater marine clays) |
| AU : | FAVRE (J.-L.); HATTAB (M.) |
| AF : | Laboratoire de mécanique des sols structures et matériaux UMR CNRS 8579 École centrale Paris grande voie des Vignes/92295 Châtenay-Malabry/France (1 aut.); Laboratoire de physique et mécanique des matériaux ISGMP-UMR CNRS 7554 Île du Saulcy/57045 Metz/France (2 aut.) |
| DT : | Publication en série; Niveau analytique |
| SO : | Revue française de géotechnique; ISSN 0181-0529; France; Da. 2006; No. 116; Pp. 3-13; Abs. anglais; Bibl. 25 ref. |
| LA : | Français |
| EA : | A 14 meter long deepwater marine clay coree, from the Gulf of Guinea, is analysed with a 16.7 cm step and its behaviour compared on one hand, with the reference behaviour of the remoulded normally consolidated mineral clays established by Biarez et Favre (1975, 1977), and on the other hand with intrinsic compression (ICL) line proposed by Burland (1990). The index parameters wL, wP, MBV, wnat and the mechanical parameters cu, Cc, Cs, σc, OCR are highlighted in this experimental study. The thinness of the step, the agreement of the profiles, reveals a complex genesis as well as the specificities of this natural marine smectite such as: the void ratio of sedimentation, sensitivity, and a apparent « overconsolidation » which translates a physico-chemical cohesion type. |
| CC : | 226B01; 001E01O01 |
| FD : | Argile minéral; Profondeur; Compression; Etude expérimentale; Genèse; Smectite; Sédimentation; Compressibilité; Golfe de Guinée |
| FG : | Phyllosilicate; Silicate; Océan Atlantique Nord; Océan Atlantique |
| ED : | clay minerals; depth; compression; experimental studies; genesis; smectite; sedimentation; compressibility; Gulf of Guinea |
| EG : | sheet silicates; silicates; North Atlantic; Atlantic Ocean |
| SD : | Arcilla mineral; Profundidad; Compresión; Génesis; Esmectita; Sedimentación; Compresibilidad; Golfo de Guinea |
| LO : | INIST-18765.354000152312780010 |
| ID : | 07-0187350 |
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Pascal:07-0187350Le document en format XML
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Hattab</name><affiliation><inist:fA14 i1="02"><s1>Laboratoire de physique et mécanique des matériaux ISGMP-UMR CNRS 7554 Île du Saulcy</s1><s2>57045 Metz</s2><s3>FRA</s3><sZ>2 aut.</sZ></inist:fA14></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">07-0187350</idno><date when="2006">2006</date><idno type="stanalyst">PASCAL 07-0187350 INIST</idno><idno type="RBID">Pascal:07-0187350</idno><idno type="wicri:Area/PascalFrancis/Corpus">000349</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="fr" level="a">Propriétés des argiles marines de grande profondeur</title><author><name sortKey="Favre, J L" sort="Favre, J L" uniqKey="Favre J" first="J.-L." last="Favre">J.-L. Favre</name><affiliation><inist:fA14 i1="01"><s1>Laboratoire de mécanique des sols structures et matériaux UMR CNRS 8579 École centrale Paris grande voie des Vignes</s1><s2>92295 Châtenay-Malabry</s2><s3>FRA</s3><sZ>1 aut.</sZ></inist:fA14></affiliation></author><author><name sortKey="Hattab, M" sort="Hattab, M" uniqKey="Hattab M" first="M." last="Hattab">M. Hattab</name><affiliation><inist:fA14 i1="02"><s1>Laboratoire de physique et mécanique des matériaux ISGMP-UMR CNRS 7554 Île du Saulcy</s1><s2>57045 Metz</s2><s3>FRA</s3><sZ>2 aut.</sZ></inist:fA14></affiliation></author></analytic><series><title level="j" type="main">Revue française de géotechnique</title><title level="j" type="abbreviated">Rev. fr. géotech.</title><idno type="ISSN">0181-0529</idno><imprint><date when="2006">2006</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Revue française de géotechnique</title><title level="j" type="abbreviated">Rev. fr. géotech.</title><idno type="ISSN">0181-0529</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Gulf of Guinea</term><term>clay minerals</term><term>compressibility</term><term>compression</term><term>depth</term><term>experimental studies</term><term>genesis</term><term>sedimentation</term><term>smectite</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Argile minéral</term><term>Profondeur</term><term>Compression</term><term>Etude expérimentale</term><term>Genèse</term><term>Smectite</term><term>Sédimentation</term><term>Compressibilité</term><term>Golfe de Guinée</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">A 14 meter long deepwater marine clay coree, from the Gulf of Guinea, is analysed with a 16.7 cm step and its behaviour compared on one hand, with the reference behaviour of the remoulded normally consolidated mineral clays established by Biarez et Favre (1975, 1977), and on the other hand with intrinsic compression (ICL) line proposed by Burland (1990). The index parameters w<sub>L</sub>, w<sub>P</sub>, MBV, w<sub>nat</sub> and the mechanical parameters c<sub>u</sub>, C<sub>c</sub>, C<sub>s</sub>, σ<sub>c</sub>, OCR are highlighted in this experimental study. The thinness of the step, the agreement of the profiles, reveals a complex genesis as well as the specificities of this natural marine smectite such as: the void ratio of sedimentation, sensitivity, and a apparent « overconsolidation » which translates a physico-chemical cohesion type.</div></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0181-0529</s0></fA01><fA03 i2="1"><s0>Rev. fr. géotech.</s0></fA03><fA06><s2>116</s2></fA06><fA08 i1="01" i2="1" l="FRE"><s1>Propriétés des argiles marines de grande profondeur</s1></fA08><fA11 i1="01" i2="1"><s1>FAVRE (J.-L.)</s1></fA11><fA11 i1="02" i2="1"><s1>HATTAB (M.)</s1></fA11><fA14 i1="01"><s1>Laboratoire de mécanique des sols structures et matériaux UMR CNRS 8579 École centrale Paris grande voie des Vignes</s1><s2>92295 Châtenay-Malabry</s2><s3>FRA</s3><sZ>1 aut.</sZ></fA14><fA14 i1="02"><s1>Laboratoire de physique et mécanique des matériaux ISGMP-UMR CNRS 7554 Île du Saulcy</s1><s2>57045 Metz</s2><s3>FRA</s3><sZ>2 aut.</sZ></fA14><fA20><s1>3-13</s1></fA20><fA21><s1>2006</s1></fA21><fA23 i1="01"><s0>FRE</s0></fA23><fA24 i1="01"><s0>eng</s0></fA24><fA43 i1="01"><s1>INIST</s1><s2>18765</s2><s5>354000152312780010</s5></fA43><fA44><s0>0000</s0><s1>© 2007 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>25 ref.</s0></fA45><fA47 i1="01" i2="1"><s0>07-0187350</s0></fA47><fA60><s1>P</s1></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>Revue française de géotechnique</s0></fA64><fA66 i1="01"><s0>FRA</s0></fA66><fA68 i1="01" i2="1" l="ENG"><s1>Properties of deepwater marine clays</s1></fA68><fC01 i1="01" l="ENG"><s0>A 14 meter long deepwater marine clay coree, from the Gulf of Guinea, is analysed with a 16.7 cm step and its behaviour compared on one hand, with the reference behaviour of the remoulded normally consolidated mineral clays established by Biarez et Favre (1975, 1977), and on the other hand with intrinsic compression (ICL) line proposed by Burland (1990). The index parameters w<sub>L</sub>, w<sub>P</sub>, MBV, w<sub>nat</sub> and the mechanical parameters c<sub>u</sub>, C<sub>c</sub>, C<sub>s</sub>, σ<sub>c</sub>, OCR are highlighted in this experimental study. The thinness of the step, the agreement of the profiles, reveals a complex genesis as well as the specificities of this natural marine smectite such as: the void ratio of sedimentation, sensitivity, and a apparent « overconsolidation » which translates a physico-chemical cohesion type.</s0></fC01><fC02 i1="01" i2="2"><s0>226B01</s0></fC02><fC02 i1="02" i2="2"><s0>001E01O01</s0></fC02><fC03 i1="01" i2="2" l="FRE"><s0>Argile minéral</s0><s2>NZ</s2><s5>01</s5></fC03><fC03 i1="01" i2="2" l="ENG"><s0>clay minerals</s0><s2>NZ</s2><s5>01</s5></fC03><fC03 i1="01" i2="2" l="SPA"><s0>Arcilla mineral</s0><s2>NZ</s2><s5>01</s5></fC03><fC03 i1="02" i2="2" l="FRE"><s0>Profondeur</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="ENG"><s0>depth</s0><s5>02</s5></fC03><fC03 i1="02" i2="2" l="SPA"><s0>Profundidad</s0><s5>02</s5></fC03><fC03 i1="03" i2="2" l="FRE"><s0>Compression</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="ENG"><s0>compression</s0><s5>03</s5></fC03><fC03 i1="03" i2="2" l="SPA"><s0>Compresión</s0><s5>03</s5></fC03><fC03 i1="04" i2="2" l="FRE"><s0>Etude expérimentale</s0><s5>04</s5></fC03><fC03 i1="04" i2="2" l="ENG"><s0>experimental studies</s0><s5>04</s5></fC03><fC03 i1="05" i2="2" l="FRE"><s0>Genèse</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="ENG"><s0>genesis</s0><s5>05</s5></fC03><fC03 i1="05" i2="2" l="SPA"><s0>Génesis</s0><s5>05</s5></fC03><fC03 i1="06" i2="2" l="FRE"><s0>Smectite</s0><s2>NZ</s2><s5>06</s5></fC03><fC03 i1="06" i2="2" l="ENG"><s0>smectite</s0><s2>NZ</s2><s5>06</s5></fC03><fC03 i1="06" i2="2" l="SPA"><s0>Esmectita</s0><s2>NZ</s2><s5>06</s5></fC03><fC03 i1="07" i2="2" l="FRE"><s0>Sédimentation</s0><s5>07</s5></fC03><fC03 i1="07" i2="2" l="ENG"><s0>sedimentation</s0><s5>07</s5></fC03><fC03 i1="07" i2="2" l="SPA"><s0>Sedimentación</s0><s5>07</s5></fC03><fC03 i1="08" i2="2" l="FRE"><s0>Compressibilité</s0><s5>08</s5></fC03><fC03 i1="08" i2="2" l="ENG"><s0>compressibility</s0><s5>08</s5></fC03><fC03 i1="08" i2="2" l="SPA"><s0>Compresibilidad</s0><s5>08</s5></fC03><fC03 i1="09" i2="2" l="FRE"><s0>Golfe de Guinée</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="09" i2="2" l="ENG"><s0>Gulf of Guinea</s0><s2>NG</s2><s5>61</s5></fC03><fC03 i1="09" i2="2" l="SPA"><s0>Golfo de Guinea</s0><s2>NG</s2><s5>61</s5></fC03><fC07 i1="01" i2="2" l="FRE"><s0>Phyllosilicate</s0><s2>NZ</s2></fC07><fC07 i1="01" i2="2" l="ENG"><s0>sheet silicates</s0><s2>NZ</s2></fC07><fC07 i1="01" i2="2" l="SPA"><s0>Filosilicato</s0><s2>NZ</s2></fC07><fC07 i1="02" i2="2" l="FRE"><s0>Silicate</s0></fC07><fC07 i1="02" i2="2" l="ENG"><s0>silicates</s0></fC07><fC07 i1="02" i2="2" l="SPA"><s0>Silicato</s0></fC07><fC07 i1="03" i2="2" l="FRE"><s0>Océan Atlantique Nord</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="ENG"><s0>North Atlantic</s0><s2>NG</s2></fC07><fC07 i1="03" i2="2" l="SPA"><s0>Océano Atlántico Norte</s0><s2>NG</s2></fC07><fC07 i1="04" i2="2" l="FRE"><s0>Océan Atlantique</s0></fC07><fC07 i1="04" i2="2" l="ENG"><s0>Atlantic Ocean</s0></fC07><fC07 i1="04" i2="2" l="SPA"><s0>Océano Atlántico</s0></fC07><fN21><s1>122</s1></fN21><fN44 i1="01"><s1>OTO</s1></fN44><fN82><s1>OTO</s1></fN82></pA></standard><server><NO>PASCAL 07-0187350 INIST</NO><FT>Propriétés des argiles marines de grande profondeur</FT><ET>(Properties of deepwater marine clays)</ET><AU>FAVRE (J.-L.); HATTAB (M.)</AU><AF>Laboratoire de mécanique des sols structures et matériaux UMR CNRS 8579 École centrale Paris grande voie des Vignes/92295 Châtenay-Malabry/France (1 aut.); Laboratoire de physique et mécanique des matériaux ISGMP-UMR CNRS 7554 Île du Saulcy/57045 Metz/France (2 aut.)</AF><DT>Publication en série; Niveau analytique</DT><SO>Revue française de géotechnique; ISSN 0181-0529; France; Da. 2006; No. 116; Pp. 3-13; Abs. anglais; Bibl. 25 ref.</SO><LA>Français</LA><EA>A 14 meter long deepwater marine clay coree, from the Gulf of Guinea, is analysed with a 16.7 cm step and its behaviour compared on one hand, with the reference behaviour of the remoulded normally consolidated mineral clays established by Biarez et Favre (1975, 1977), and on the other hand with intrinsic compression (ICL) line proposed by Burland (1990). The index parameters w<sub>L</sub>, w<sub>P</sub>, MBV, w<sub>nat</sub> and the mechanical parameters c<sub>u</sub>, C<sub>c</sub>, C<sub>s</sub>, σ<sub>c</sub>, OCR are highlighted in this experimental study. The thinness of the step, the agreement of the profiles, reveals a complex genesis as well as the specificities of this natural marine smectite such as: the void ratio of sedimentation, sensitivity, and a apparent « overconsolidation » which translates a physico-chemical cohesion type.</EA><CC>226B01; 001E01O01</CC><FD>Argile minéral; Profondeur; Compression; Etude expérimentale; Genèse; Smectite; Sédimentation; Compressibilité; Golfe de Guinée</FD><FG>Phyllosilicate; Silicate; Océan Atlantique Nord; Océan Atlantique</FG><ED>clay minerals; depth; compression; experimental studies; genesis; smectite; sedimentation; compressibility; Gulf of Guinea</ED><EG>sheet silicates; silicates; North Atlantic; Atlantic Ocean</EG><SD>Arcilla mineral; Profundidad; Compresión; Génesis; Esmectita; Sedimentación; Compresibilidad; Golfo de Guinea</SD><LO>INIST-18765.354000152312780010</LO><ID>07-0187350</ID></server></inist></record>Pour manipuler ce document sous Unix (Dilib)
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