2014
DOI: 10.1080/07373937.2013.873804
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A Generalized Relationship for Determination of Tensile Strength of Fine-Grained Soils from Shrinkage Characteristics

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Cited by 6 publications
(3 citation statements)
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“…Shrinkage and subsequent crack formation are important phenomena in sludge drying because the sample loses its moisture and exhibits volumetric reduction, and then the internal stresses exceed the tensile strength. [11][12][13][14][15] First, mathematical modeling for determination of diffusion coefficients was established and convective drying experiments of sludges and sawdust=sludge mixtures were done. X-ray tomography, a non-destructive imaging technique, is used to get the volume, surface, and porosity of the sample bed directly.…”
Section: Introductionmentioning
confidence: 99%
“…Shrinkage and subsequent crack formation are important phenomena in sludge drying because the sample loses its moisture and exhibits volumetric reduction, and then the internal stresses exceed the tensile strength. [11][12][13][14][15] First, mathematical modeling for determination of diffusion coefficients was established and convective drying experiments of sludges and sawdust=sludge mixtures were done. X-ray tomography, a non-destructive imaging technique, is used to get the volume, surface, and porosity of the sample bed directly.…”
Section: Introductionmentioning
confidence: 99%
“…Results obtained from these techniques were critically evaluated vis-à-vis those obtained from triaxial tests and empirical relationships available in the literature. It has been observed that there is a unique relationship between the results of the thin and thick samples and hence thin samples of expansive clays can be employed for determining their tensile strength [207,214,215]. This shows the usefulness of the proposed techniques for measuring the tensile strength of the finegrained that too expansive soils.…”
Section: Role Of Environmental Stresses: Cracking Of Fine-grained Soilsmentioning
confidence: 78%
“…Most tensile strength experiments are induced by external loading and not by the internal desiccation stresses [1] or fail to incorporate stage-wise drying of soils [2], which is essential for investigations related to cracking characteristics in clays. Commonly studies investigate full saturated conditions, few researchers performed experiments on initially unsaturated and compacted clays.…”
Section: Introductionmentioning
confidence: 99%