Please use this identifier to cite or link to this item: https://doi.org/10.1680/geot.52.10.713.38851
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dc.titleOne-dimensional self-weight consolidation of a lumpy clay fill
dc.contributor.authorYang, LA
dc.contributor.authorTan, TS
dc.contributor.authorTan, SA
dc.contributor.authorLeung, CF
dc.date.accessioned2021-12-22T04:03:00Z
dc.date.available2021-12-22T04:03:00Z
dc.date.issued2002-12-01
dc.identifier.citationYang, LA, Tan, TS, Tan, SA, Leung, CF (2002-12-01). One-dimensional self-weight consolidation of a lumpy clay fill. GEOTECHNIQUE 52 (10) : 713-725. ScholarBank@NUS Repository. https://doi.org/10.1680/geot.52.10.713.38851
dc.identifier.issn00168505
dc.identifier.issn17517656
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/211456
dc.description.abstractThe need to use a large amount of dredged and excavated materials as fill for land reclamation necessitates an examination of the consolidation of a lumpy fill. Experimental results have shown the existence of two systems of voids in such a fill: inter-lump voids and intra-lump voids. The consolidation of this fill is highly complicated, and a simple box-spring model analogy is used to provide a better interpretation of the consolidation of this fill. To model this consolidation, the dualporosity model developed for fissured clay is used to model the consolidation of the lumpy fill; the primary motivation is the similarity between fissured clay and a lumpy fill with inter-lump voids. In the paper, this theory is re-derived using a two-phase flow analogy. Self-weight is explicitly included in the derivation: this is considered to be more relevant than the case of surcharge only, as the fill is often left to stand for a long period before sand fill is placed on top. A previously derived analytical solution is now modified to include self-weight. Using the analytical solution, salient features of the consolidation are demonstrated. In a lumpy fill, owing to the large inter-lump voids, the permeability of the inter-lump system is much larger than that of the intra-lump system. Parametric analyses using the analytical solution show that the inter-lump permeability dominates the overall consolidation behaviour in two ways. First, it will cause a rapid dissipation of the pore pressure in the inter-lump voids, and this in turn will cause a greater difference between the pore pressure in the inter-lump and intra-lump systems, thereby accelerating the fluid transfer from the intra-lump voids to the inter-lump voids.
dc.description.urihttp://libproxy1.nus.edu.sg/login?url=http://dx.doi.org/10.1680/geot.52.10.713.38851
dc.language.isoen
dc.publisherICE PUBLISHING
dc.sourceElements
dc.subjectScience & Technology
dc.subjectTechnology
dc.subjectEngineering, Geological
dc.subjectEngineering
dc.subjectclays
dc.subjectconsolidation
dc.subjectreclamation
dc.subjecttheoretical analysis
dc.subjectFLOW
dc.subjectBEHAVIOR
dc.typeArticle
dc.date.updated2021-12-19T04:20:44Z
dc.contributor.departmentCIVIL AND ENVIRONMENTAL ENGINEERING
dc.description.doi10.1680/geot.52.10.713.38851
dc.description.sourcetitleGEOTECHNIQUE
dc.description.volume52
dc.description.issue10
dc.description.page713-725
dc.description.codenGTNQA
dc.identifier.isiut000180502700002
dc.published.statePublished
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