DSpace Repository

Laboratory study on the suffusion behaviour of coarse gap-graded soils for use as potential upstream crack-fillers in zoned dams

Show simple item record

dc.contributor.author Santos, R. N. C. pt_BR
dc.contributor.author Caldeira, L. pt_BR
dc.contributor.author Maranha das Neves, E. pt_BR
dc.date.accessioned 2016-04-29T13:51:38Z pt_BR
dc.date.accessioned 2017-04-13T11:52:12Z
dc.date.available 2016-04-29T13:51:38Z pt_BR
dc.date.available 2017-04-13T11:52:12Z
dc.date.issued 2015 pt_BR
dc.identifier.uri https://repositorio.lnec.pt/jspui/handle/123456789/1008200
dc.description.abstract This paper presents an experimental study aiming at the evaluation the suffusion behaviour of coarse gap-graded soils, considered as potential upstream crack-fillers in zoned dams. Six granular gap-graded soils missing the medium-to-coarse sand fraction have been examined. Four soils have no fines, one has 5% of non-plastic fines, and one has 5% of clayey fines (with plasticity index of about 14%). The use of available methods to assess internal stability of soils suggests that the majority of the selected soils are highly susceptible to suffusion. Testing has been carried out in the Upward Flow (UF) seepage test. A cylindrical seepage cell is used to impose vertical flow, from the bottom to the top, along a soil specimen with 200 mm-diameter and 150 mm-thick. During an UF test, the hydraulic gradient in the soil specimen is slowly increased in steps. The observation of the erosion behaviour at the top surface of specimen, together with the evolution of the discharge flow rate, allows determining the hydraulic gradients causing initiation of erosion on top of the specimen and development of suffusion in the soil. A ‘sand boiling’ phenomenon has been observed in soils exhibiting suffusion, resulting in the deposition of the finer particles at the specimen surface. One may conclude that the lower the gradient associated to the onset of ‘sand boiling’ phenomenon, and the higher the amount of material deposited in the top of the specimen, the higher the likelihood of gap-graded soils to be effective acting as upstream crack-filler. Laboratory testing on soils with no fines clearly shows that the higher the content of the fine sand fraction the higher the amount of material deposited on top of the specimen, however, the higher the gradients associated to initiation of suffusion and development of 'sand boiling'. Whenever high hydraulic gradients are not likely to occur, the gap-graded soil with 5% of non-plastic fines should be more reliable at filling in cracks than the gap-graded soil with 5% of clayey fines. pt_BR
dc.language.iso eng pt_BR
dc.publisher LNEC pt_BR
dc.rights openAccess pt_BR
dc.subject Sufusion pt_BR
dc.subject Gap-graded soils pt_BR
dc.subject Crack-filler pt_BR
dc.subject Zoned dam pt_BR
dc.subject Laboratory tests pt_BR
dc.title Laboratory study on the suffusion behaviour of coarse gap-graded soils for use as potential upstream crack-fillers in zoned dams pt_BR
dc.type conferenceObject pt_BR
dc.description.pages 687-698pp pt_BR
dc.identifier.local Lisbon, Portugal pt_BR
dc.description.sector DG/NGOH pt_BR
dc.identifier.conftitle Second International Dam World Conference (Dam World 2015) pt_BR
dc.contributor.peer-reviewed SIM pt_BR
dc.contributor.academicresearchers SIM pt_BR
dc.contributor.arquivo SIM pt_BR


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search DSpace


Advanced Search

Browse

My Account