2022
DOI: 10.1002/nag.3369
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General analytical solutions for one‐dimensional nonlinear consolidation of saturated clay under non‐isothermal distribution condition

Abstract: The fluctuation of temperature leads to the changes of physical‐mechanical properties of clayey soils. In some practical projects such as landfills, the compacted clay liner is usually subjected to a non‐isothermal distribution state. For one‐dimensional nonlinear consolidation process of saturated clay under non‐isothermal distribution condition, the general analytical solutions considering time‐dependent loading are derived for the first time, where the methods of algebraic transformation and separation vari… Show more

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Cited by 10 publications
(12 citation statements)
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“…The proposed analytical solutions will be promoted if the time‐dependent variations of these consolidation‐related parameters are involved 28,29 . In addition, the proposed analytical solutions are expected to spread into more circumstances, such as unsaturated soft soils causing varying negative and positive friction along the pile shaft 30,22 and nonlinear constitutive models of subsoils 31,32 …”
Section: Discussionmentioning
confidence: 99%
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“…The proposed analytical solutions will be promoted if the time‐dependent variations of these consolidation‐related parameters are involved 28,29 . In addition, the proposed analytical solutions are expected to spread into more circumstances, such as unsaturated soft soils causing varying negative and positive friction along the pile shaft 30,22 and nonlinear constitutive models of subsoils 31,32 …”
Section: Discussionmentioning
confidence: 99%
“…28,29 In addition, the proposed analytical solutions are expected to spread into more circumstances, such as unsaturated soft soils causing varying negative and positive friction along the pile shaft 30,22 and nonlinear constitutive models of subsoils. 31,32 Notation: Basic SI units are given in parentheses…”
Section: Discussionmentioning
confidence: 99%
“…Using the variation of dynamic viscosity coefficients with temperature at standard atmospheric pressure (see Table 1), 61,68 the following relationship can be adopted approximately: η0.33em()Tcbadbreak=36.42×103Tc+19.20.33emPa·normals0.33em(R2=0.99)$$\begin{equation} \eta \ \left({T}_{c}\right)=\frac{36.42\ensuremath{\times{}}{10}^{-3}}{{T}_{c}+19.2}\ \mathrm{Pa}\cdot \mathrm{s}\ (\ {R}^{2}=\ 0.99) \end{equation}$$…”
Section: Mathematical Modelmentioning
confidence: 99%
“…Moreover, the semi‐logarithmic relationship is commonly applied to describe the nonlinear variation of permeability coefficient with void ratio as the CCL consolidation proceeds 7,61,69 : e0.33embadbreak=e00.33emgoodbreak+Ckprefixlg[kvTc/kv0Tc]$$\begin{equation}e\ = {e_0}\ + {C_k}\lg [{k_v}\left( {{T_c}} \right)/{k_{v0}}\left( {{T_c}} \right)]\end{equation}$$where Ck${C_k}$ represents the permeability index; kv0(Tc)${k_{v0}}( {{T_c}} )$ denotes the initial permeability coefficient at temperature Tc${T_c}$.…”
Section: Mathematical Modelmentioning
confidence: 99%
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