Model test studies on soil restraint to pipelines buried in sand

R. Liu*, S. W. Yan, J. Chu

*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingConference contribution

1 Citation (Scopus)

Abstract

The buckling of submarine pipelines may occur due to the action of axial soil frictional force caused by relative movement of soil and pipeline, which is induced by the thermal and internal pressure. The likelihood of occurrence of this buckling phenomenon is largely determined by the capability of the soil to resist pipeline movements. A series of large-scale model tests were carried out to facilitate the establishment of substantial data base for a variety of burial pipeline topologies. Results show that the soil resistance depends on the pipe diameters and the depth of cover. According to the uplift test results, the force-displacement topologies with smaller depth of cover are greatly different from those with larger depth of cover. The results of the lateral sliding and axial pull out tests show that the soil resistance initially increases before a peak value is reached and then keeps the same level. For the same covered depth, the lateral soil resistance is more than twice that for uplift.

Original languageEnglish
Title of host publicationFrontiers in Offshore Geotechnics II - Proceedings of the 2nd International Symposium on Frontiers in Offshore Geotechnics
Pages815-820
Number of pages6
Publication statusPublished - 2011
Externally publishedYes
Event2nd International Symposium on Frontiers in Offshore Geotechnics, ISFOG 2010 - Perth, WA, Australia
Duration: Nov 8 2010Nov 10 2010

Publication series

NameFrontiers in Offshore Geotechnics II - Proceedings of the 2nd International Symposium on Frontiers in Offshore Geotechnics

Conference

Conference2nd International Symposium on Frontiers in Offshore Geotechnics, ISFOG 2010
Country/TerritoryAustralia
CityPerth, WA
Period11/8/1011/10/10

ASJC Scopus Subject Areas

  • Geotechnical Engineering and Engineering Geology

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