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contributor authorJeffrey Parks
contributor authorMarc Edwards
contributor authorPeter Vikesland
contributor authorAbhijeet Dudi
date accessioned2017-05-08T21:55:08Z
date available2017-05-08T21:55:08Z
date copyrightMay 2010
date issued2010
identifier other%28asce%29mt%2E1943-5533%2E0000114.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/66423
description abstractAutogenous healing can occur when hairline cracks in concrete repair themselves through reactions with water and/or constituents in water. The chemistry of water contacting the cement affects whether the crack heals autogenously or propagates until leaks occur. The strength testing on concrete specimens demonstrates that appreciable healing can occur at a pH of 9.5 when there is sufficient magnesium and silicon in the water. Scanning electron microscopy with energy dispersive spectroscopy (SEM-EDS) analyses indicate that a magnesium silicate material is present within the crack surfaces when higher strength healing has occurred. Calcium does not appear to promote the sealing of cracks. A carbonation of internal concrete surfaces was not detected when cracks were sealed via autogenous healing. Chloride diffusion rates do not return to levels seen in virgin concrete when cracks are autogenously healed. However, the water permeability and chloride diffusion are impeded by any filling of cracks regardless of the strength attained.
publisherAmerican Society of Civil Engineers
titleEffects of Bulk Water Chemistry on Autogenous Healing of Concrete
typeJournal Paper
journal volume22
journal issue5
journal titleJournal of Materials in Civil Engineering
identifier doi10.1061/(ASCE)MT.1943-5533.0000082
treeJournal of Materials in Civil Engineering:;2010:;Volume ( 022 ):;issue: 005
contenttypeFulltext


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