Estimation of overconsolidation ratio from piezocone test in Singapore marine clays
Identifieur interne : 000559 ( PascalFrancis/Checkpoint ); précédent : 000558; suivant : 000560Estimation of overconsolidation ratio from piezocone test in Singapore marine clays
Auteurs : K. K. Phoon [Singapour] ; H. E. Low [Singapour] ; T. S. Tan [Singapour]Source :
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- Pascal (Inist)
- Wicri :
- geographic : Singapour.
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Abstract
The accuracy of the OCR-Qt correlation for Singapore marine clays is examined using site specific data. It is possible to estimate OCR within ± 30% for the lower marine clay layer with more than 90% confidence. To achieve similar accuracy for the upper marine clay layer, additional data such as the in-situ void ratio appears to be necessary
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Low</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>National University of Singapore</s1><s2>Singapore</s2><s3>SGP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Singapour</country><orgName type="university">Université nationale de Singapour</orgName></affiliation></author><author><name sortKey="Tan, T S" sort="Tan, T S" uniqKey="Tan T" first="T. S." last="Tan">T. S. Tan</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>National University of Singapore</s1><s2>Singapore</s2><s3>SGP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Singapour</country><orgName type="university">Université nationale de Singapour</orgName></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">04-0036330</idno><date when="2003">2003</date><idno type="stanalyst">PASCAL 04-0036330 BRGM</idno><idno type="RBID">Pascal:04-0036330</idno><idno type="wicri:Area/PascalFrancis/Corpus">000576</idno><idno type="wicri:Area/PascalFrancis/Curation">000214</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000559</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Estimation of overconsolidation ratio from piezocone test in Singapore marine clays</title><author><name sortKey="Phoon, K K" sort="Phoon, K K" uniqKey="Phoon K" first="K. K." last="Phoon">K. K. Phoon</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>National University of Singapore</s1><s2>Singapore</s2><s3>SGP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Singapour</country><orgName type="university">Université nationale de Singapour</orgName></affiliation></author><author><name sortKey="Low, H E" sort="Low, H E" uniqKey="Low H" first="H. E." last="Low">H. E. Low</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>National University of Singapore</s1><s2>Singapore</s2><s3>SGP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Singapour</country><orgName type="university">Université nationale de Singapour</orgName></affiliation></author><author><name sortKey="Tan, T S" sort="Tan, T S" uniqKey="Tan T" first="T. S." last="Tan">T. S. Tan</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>National University of Singapore</s1><s2>Singapore</s2><s3>SGP</s3><sZ>1 aut.</sZ><sZ>2 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Singapour</country><orgName type="university">Université nationale de Singapour</orgName></affiliation></author></analytic></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Singapore</term><term>clay</term><term>cone penetration tests</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Test pénétration cône</term><term>Argile</term><term>Singapour</term><term>Essai piézocone</term><term>Rapport surconsolidation</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Singapour</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The accuracy of the OCR-Q<sub>t</sub> correlation for Singapore marine clays is examined using site specific data. It is possible to estimate OCR within ± 30% for the lower marine clay layer with more than 90% confidence. To achieve similar accuracy for the upper marine clay layer, additional data such as the in-situ void ratio appears to be necessary</div></front></TEI><inist><standard h6="B"><pA><fA08 i1="01" i2="1" l="ENG"><s1>Estimation of overconsolidation ratio from piezocone test in Singapore marine clays</s1></fA08><fA09 i1="01" i2="1" l="ENG"><s1>Field measurements in geomechanics</s1></fA09><fA11 i1="01" i2="1"><s1>PHOON (K. K.)</s1></fA11><fA11 i1="02" i2="1"><s1>LOW (H. E.)</s1></fA11><fA11 i1="03" i2="1"><s1>TAN (T. 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K." last="Phoon">K. K. Phoon</name></noRegion><name sortKey="Low, H E" sort="Low, H E" uniqKey="Low H" first="H. E." last="Low">H. E. Low</name><name sortKey="Tan, T S" sort="Tan, T S" uniqKey="Tan T" first="T. S." last="Tan">T. S. Tan</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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