From: Thermal modeling of subduction zones with prescribed and evolving 2D and 3D slab geometries
Description | Condition | Location |
---|---|---|
Velocity | Â | Â |
Free slip | \(\varvec{u} \cdot \hat{\varvec{n}} = 0\) and \((\varvec{\sigma }\cdot \hat{\varvec{n}}) \cdot \hat{\varvec{\tau }}_i = \varvec{0}\), \(i=1,\ldots ,D-1\) | \({\partial \Omega _\text {top} \cup \partial \Omega _\text {near} \cup \partial \Omega _\text {far} \cup \partial \Omega _\text {bottom}}\) |
Natural in/outlet | \(\varvec{\sigma }\cdot \hat{\varvec{n}} = \varvec{0}\) | \(\partial \Omega _\text {slab inlet} \cup \partial \Omega _\text {slab outlet} \cup \partial \Omega _\text {wedge outlet}\) |
Velocity coupled driven slab | \(\varvec{u} = u_\text {conv} \hat{\varvec{\tau }}_\text {conv} + \varvec{u}_\text {slab}\) | \(\Gamma _\text {slab} \cup \Gamma _\text {slab fault}\) |
Fault zone no slip | \(\varvec{u} = \varvec{u}_\text {slab}\) | \(\Gamma _\text {wedge no slip}\) |
Temperature | Â | Â |
Surface temperature | \(T = T_0\) | \(\partial \Omega _\text {top}\) |
Inlet slab temperature | \(T = T_\text {in}\) | \(\partial \Omega _\text {slab inlet}\) |
Outlet temperature influx | \(T = T_\text {out}\) | \(\partial \Omega _\text {wedge outlet} \cup \partial \Omega _\text {slab outlet}\) where \(\varvec{u} \cdot \hat{\varvec{n}} < 0\) |
Outlet temperature outflux | \(k \nabla T \cdot \hat{\varvec{n}} = 0\) | \(\partial \Omega _\text {wedge outlet} \cup \partial \Omega _\text {slab outlet}\) where \(\varvec{u} \cdot \hat{\varvec{n}} \ge 0\) |
Zero heat flux | \(k \nabla T \cdot \hat{\varvec{n}} = 0\) | \(\partial \Omega _\text {near} \cup \partial \Omega _\text {far} \cup \partial \Omega _\text {bottom}\) |
Temperature coupling | \(T_\text {slab} \hat{\varvec{n}}_\text {slab} = - T_\text {plate} \hat{\varvec{n}}_\text {plate}\) | Â |
 | and \(T_\text {slab} \hat{\varvec{n}}_\text {slab} = - T_\text {wedge} \hat{\varvec{n}}_\text {wedge}\) | \(\Gamma _\text {slab} \cup \Gamma _\text {wedge no slip} \cup \Gamma _\text {slab fault}\) |