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contributor authorHideki Oshita
contributor authorTada-aki Tanabe
date accessioned2017-05-08T22:39:16Z
date available2017-05-08T22:39:16Z
date copyrightMay 2000
date issued2000
identifier other%28asce%290733-9399%282000%29126%3A5%28544%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/85198
description abstractThe material parameters to express the degree of discontinuity of hydraulic gradient in the developed model (Part I) are calibrated based on the sensible analysis of the experimental results, and then the applicability of the calibrated parameters is discussed. As a result, the material parameters are calibrated by the sensible analysis, and then its relevance can be confirmed by another experiment. Moreover, it can be seen that the normalized permeability of concrete as a nonhomogeneous material by the initial permeability (homogeneous material) can be regressed with three straight lines in the crack width axis with the logarithm. Then the intersection point at the crack width axis shows the critical width at which leakage will not occur. The intersection point at the last two straight lines shows the critical Reynolds number at which flow becomes laminar to turbulent according to the experimental result.
publisherAmerican Society of Civil Engineers
titleWater Migration Phenomenon Model in Cracked Concrete. II: Calibration
typeJournal Paper
journal volume126
journal issue5
journal titleJournal of Engineering Mechanics
identifier doi10.1061/(ASCE)0733-9399(2000)126:5(544)
treeJournal of Engineering Mechanics:;2000:;Volume ( 126 ):;issue: 005
contenttypeFulltext


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