Finite element and isogeometric stabilized methods for the advection-diffusion-reaction equation

We develop two new stabilized methods for the steady advection-diffusion-reaction equation, referred to as the Streamline GSC Method and the Directional GSC Method. Both are globally conservative and perform well in numerical studies utilizing linear, quadratic, cubic, and quartic Lagrange finite el...

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Veröffentlicht in:Computer methods in applied mechanics and engineering 2023-12, Vol.417, p.116354, Article 116354
Hauptverfasser: Key, Konstantin, Abdelmalik, Michael R.A., Elgeti, Stefanie, Hughes, Thomas J.R., Baidoo, Frimpong A.
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Sprache:eng
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Zusammenfassung:We develop two new stabilized methods for the steady advection-diffusion-reaction equation, referred to as the Streamline GSC Method and the Directional GSC Method. Both are globally conservative and perform well in numerical studies utilizing linear, quadratic, cubic, and quartic Lagrange finite elements and maximally smooth B-spline elements. For the streamline GSC method we can prove coercivity, convergence, and optimal-order error estimates in a strong norm that are robust in the advective and reactive limits. The directional GSC method is designed to accurately resolve boundary layers for flows that impinge upon the boundary at an angle, a long-standing problem. The directional GSC method performs better than the streamline GSC method in the numerical studies, but it is not coercive. We conjecture it is inf-sup stable but we are unable to prove it at this time. However, calculations of the inf-sup constant support the conjecture. In the numerical studies, B-spline finite elements consistently perform better than Lagrange finite elements of the same order and number of unknowns. •We develop 2 new methods for the steady advection-diffusion-reaction equation•The methods achieve global conservation, a shortcoming of previous stabilized methods•For one of the methods we prove stability and convergence, and obtain error estimates•The other method is designed to mitigate overshoot in outflow boundary layers•We find B-splines consistently outperform Lagrange elements in our comparisons
ISSN:0045-7825
1879-2138
DOI:10.1016/j.cma.2023.116354