Impact of plasticity and stress history on thermal volume changes in clays.

Computed \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$k$$\end{document} k values for low-plasticity (LP) and high-plasticity (HP) clay samples, stratified by varying over-consolidation ratios (OCR), are summarized in Table 3 : Analysis of these results reveals a clear trend for LP samples, where the slope \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$k$$\end{document} k increases consistently with higher OCR.

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