2022
DOI: 10.1016/j.compgeo.2021.104592
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An unconstrained stress updating algorithm with the line search method for elastoplastic soil models

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Cited by 13 publications
(4 citation statements)
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“…To this end, the KKT conditions in Equation (20) 4 are replaced equivalently by the Fischer-Burmeister smooth function. 19…”
Section: Unconstrained Implicit Stress Update Based On the Line Searc...mentioning
confidence: 99%
See 3 more Smart Citations
“…To this end, the KKT conditions in Equation (20) 4 are replaced equivalently by the Fischer-Burmeister smooth function. 19…”
Section: Unconstrained Implicit Stress Update Based On the Line Searc...mentioning
confidence: 99%
“…The solving process is also known as the “plastic correction.” The loading/unloading estimation is required at each increment step, which increases the complexity of the model implementation. To this end, the KKT conditions in Equation (20) 4 are replaced equivalently by the Fischer–Burmeister smooth function 19 {}f1f2f3f4badbreak={}pn+1pnexpcκΔεnormalv,n+1normale=0qn+10true32boldsn+2G¯Δbold-italicγn+11+c=0pc,n+1pc,nexpcnormalpΔεnormalv,n+1normalp=0()cdnormalΔϕn+12+fn+12+2βcnormaldΔϕn+1+fn+1=0$$\begin{equation}\left\{ { \def\eqcellsep{&}\begin{array}{@{}*{1}{c}@{}} {{f}_1}\\[15pt] {{f}_2}\\[15pt] {{f}_3}\\[15pt] {{f}_4} \end{array} } \right\} = \left\{ { \def\eqcellsep{&}\begin{array}{@{}*{1}{c}@{}} {{p}_{n + 1} - {p}_n\exp \left( {{c}_\kappa \Delta \varepsilon _{{\rm{v, }}n + 1}^{\rm{e}}} \right) = 0}\\[15pt] {{q}_{n + 1} - \sqrt {\dfrac{3}{2}} \dfrac{{\left\| {{{{\bf s}}}_n + 2\bar{G}\Delta {{{\bm \gamma }}}_{n + 1}} \right\|}}{{1 + c}} = 0}\\[15pt] {{p}_{{\rm{c}},n + 1} - {p}_{{\rm{c}},n}\exp \left( {{c}_{\rm{p}}\Delta \varepsilon _{{\rm{v, }}n + 1}^{\rm{p}}} \right) = 0}\\[15pt] {\sqrt {{{\left( {{c}_{\rm{d}}\Delta {\phi }_{n + 1}} \right)}}^2 + f_{n + 1}^2 + 2\beta } - {c}_{\rm{d}}\Delta {\phi }_{n + 1} + {f}_{n + 1} = 0} \end{array}...…”
Section: Unconstrained Implicit Stress Update Based On the Line Searc...mentioning
confidence: 99%
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