[CIG-SHORT] Meshing Schemes, Mixed Meshes, Mesh Output, & Initial Conditions
Carl W. Gable
gable at lanl.gov
Tue Feb 26 12:22:26 PST 2008
http://meshing.lanl.gov/proj/crustal_dyn_strike_slip_bm/catalog.html
If anyone has the inclination to give it a try, there is a variable
resolution tet mesh, with tets along the fault face and along the fault
tip refined to 125 m.
To compare to the uniform tet mesh:
1000m 500m 250m variable
#node 15625 117649 912673 179978
# elem 82944 663552 4962216 1037548
Also, when you connect a uniform orthogonal point distribution to form
tets, you can form 5 tets from each hex or 6 tets from each hex. Does
that have any significant impact on the results you obtain with the
1000m, 500m and 250m grids?
Cheers,
Carl
Brad Aagaard wrote:
> Following up on Ravi's questions and my response yesterday-
>
> I posted the PyLith poster from the 2007 AGU Fall Meeting in my folder on the
> CIG website (http://www.geodynamics.org/cig/Members/BradAagaard). The poster
> includes plots of the local error in the elastic solution of the strike-slip
> benchmark for both hex8 and tet4 cells at 1000 m, 500 m, and 250 m
> resolutions. We also show the runtime for the serial runs (1000 m and 500 m
> resolutions). We expect similar trends for comparison of linear (p1) quad4
> and tri3 cells.
>
> Note that the largest local error occurs at the edge of the taper region where
> the slip transitions from a uniform value to a constant gradient. This causes
> a sharp gradient in the strain field along this edge, so finer cells are
> needed in this region to accurately capture the solution. For the rest of the
> area where slip is uniform or has a uniform gradient (taper region), the
> linear basis functions do quite a good job of capturing the displacement
> field (the local error is quite small).
>
> These results indicate that for this problem the linear (p1) hex8 cells far
> outperform linear (p1) tet4 cells (factoring in both run time and the global
> error). We suspect that quadratic (p2) tet4 cells will be competitive with p1
> hex8 cells in terms of performance (comparable global error for the about the
> same run time). We have yet to implement automatic creation of p2 cells from
> a p1 mesh, so we have not tested this hypothesis.
>
> Brad
> _______________________________________________
> CIG-SHORT mailing list
> CIG-SHORT at geodynamics.org
> http://geodynamics.org/cgi-bin/mailman/listinfo/cig-short
--
\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\
Dr. Carl W. Gable, Staff Scientist
EES-6, MS T003
Los Alamos National Laboratory
Los Alamos NM 87545
gable at lanl.gov Voice 505-665-3533 Fax 505-665-8737
http://www.ees.lanl.gov/staff/gable http://lagrit.lanl.gov
Hydrology, Geochemistry & Geology Group (EES-6)
Focus: Geophysics, Hydrology, Mesh Generation
Correspondence / TSPA
/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/\/
More information about the CIG-SHORT
mailing list