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dc.contributor.author Kugan, R
dc.contributor.author Puswewala, UGA
dc.contributor.author Kulathilaka, SAS
dc.contributor.author Peiris, TA
dc.date.accessioned 2013-12-27T13:32:19Z
dc.date.available 2013-12-27T13:32:19Z
dc.date.issued 2003
dc.identifier.uri http://dl.lib.mrt.ac.lk/handle/123/9572
dc.description.abstract The first rational theory to explain the settlements occurring in saturated clays was the 1- D theory of consolidation proposed by Terzaghi (1925). One of the main advantages of the theoretical modelling of consolidation is that it becomes possible to carryout laboratory tests on thin samples of clay. a few centimetres thick (with one increment of load normally maintained for 24 hours). and then from the laboratory results predict the settlements in the field where the clay layer may be several meters thick and where the settlements may take place over a long period of time. en_US
dc.language.iso en en_US
dc.title Consolidation testing of peaty clay en_US
dc.type Conference-Extended-Abstract en_US
dc.identifier.year 2003 en_US
dc.identifier.conference ERU Research for industry en_US
dc.identifier.pgnos E5-E6 en_US
dc.identifier.proceeding Proceeding of the 9th annual symposium en_US


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