Shrinkage anisotropy characteristics from soil structure and initial sample/layer size
V. Y. Chertkov

TL;DR
This paper develops a physical model to predict soil shrinkage anisotropy based on sample size, layer thickness, and soil structure, providing new insights into how drying affects soil deformation.
Contribution
It introduces a novel approach linking soil shrinkage anisotropy to sample size, layer thickness, and soil structure through a new size ratio framework.
Findings
Predicted shrinkage anisotropy varies with sample size and soil structure.
Established relationships between shrinkage curves and physical soil parameters.
Provided illustrative estimates for different soil samples and sizes.
Abstract
The objective of this work is a physical prediction of such soil shrinkage anisotropy characteristics as variation with drying of (i) different sample/layer sizes and (ii) the shrinkage geometry factor. With that, a new presentation of the shrinkage anisotropy concept is suggested through the sample/layer size ratios. The work objective is reached in two steps. First, the relations are derived between the indicated soil shrinkage anisotropy characteristics and three different shrinkage curves of a soil relating to: small samples (without cracking at shrinkage), sufficiently large samples (with internal cracking), and layers of similar thickness. Then, the results of a recent work with respect to the physical prediction of the three shrinkage curves are used. These results connect the shrinkage curves with the initial sample size/layer thickness as well as characteristics of soil texture…
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