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dc.contributor.authorHeather Brooks
dc.contributor.authorGuy Doré
dc.contributor.authorAriane Locat
dc.date.accessioned2022-01-30T22:34:33Z
dc.date.available2022-01-30T22:34:33Z
dc.date.issued3/1/2021
dc.identifier.other(ASCE)CR.1943-5495.0000232.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4269195
dc.description.abstractAccidents, infrastructure closures and reductions in capacity, and delays have occurred and are documented in the literature due to bridge formation, sinkholes, or rapid collapses within embankment infrastructure on permafrost. However, the failure mechanics are not well understood or studied. This paper investigates soil particle position, negative pore-pressure generation, and frozen soil flexure as possible mechanisms for bridging. Published literature and laboratory testing confirmed that soil particle position is a possible mechanism for bridging voids within embankments. Factor of safety equations were developed for (1) tensile stress conditions within a loaded frozen soil beam and (2) tensile stress from matric suction conditions within unfrozen soils over a void. Using published data for common embankment materials, example calculations for bridging via matric suction and frozen soil flexure are presented. All of the presented mechanisms for creating and maintaining bridges are possible, depending on site conditions; however, the probability and consequences of bridge collapse after formation vary widely depending on the mechanism.
dc.publisherASCE
dc.titleSoil Bridging Effects within Permafrost-Supported Embankment Infrastructure
dc.typeJournal Paper
dc.journal.volume35
dc.journal.issue1
dc.journal.titleJournal of Cold Regions Engineering
dc.identifier.doi10.1061/(ASCE)CR.1943-5495.0000232
dc.journal.fristpage04020027
dc.journal.lastpage04020027-9
dc.page9
dc.treeJournal of Cold Regions Engineering:;2021:;Volume ( 035 ):;issue: 001
dc.contenttypeFulltext


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