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The hydrostatic validation involves applying gravity loading to a column of material restrained in both lateral components and along the bottom plane. The Newtonian fluid model will yield hydrostatic pressures for all normal stress directions ($\sigma_{xx}$, $\sigma_{yy}$, $\sigma_{zz}$). The linear elastic material will yield geo-static stresses in the vertical direction and the horizontal stresses depend on the Poisson's ratio.
Hydrostatic column with a width w of 0.2 m and height h of 0.1 m. Restrained in both the lateral directions and along the bottom plane
Analysis are carried out using MPM Explicit USF and USL algorithms using velocity update. Note that the results converge with more refined mesh with smaller errors.
Results (Newtonian Fluid)
USF results at t = 0.2s
Parameter
Analytical
Case 1
Case 2
Case 3
$\sigma_{yy} (N/m^2)$
-1765.800
-1680.244
-1724.583
-1746.791
$\sigma_{xx} (N/m^2)$
-1765.800
-1680.244
-1724.583
-1746.791
USL results at t = 0.2s
Parameter
Analytical
Case 1
Case 2
Case 3
$\sigma_{yy} (N/m^2)$
-1765.800
-1680.182
-1724.550
-1746.774
$\sigma_{xx} (N/m^2)$
-1765.800
-1680.182
-1724.550
-1746.774
Results (Linear Elastic)
USF results at t = 0.2s
Parameter
Analytical
Case 1
Case 2
Case 3
$\sigma_{yy} (N/m^2)$
-1765.800
-1680.244
-1724.583
-1746.791
$\sigma_{xx} (N/m^2)$
0.000
0.000
0.000
0.000
USL results at t = 0.2s
Parameter
Analytical
Case 1
Case 2
Case 3
$\sigma_{yy} (N/m^2)$
-1765.800
-1680.182
-1724.550
-1746.774
$\sigma_{xx} (N/m^2)$
0.000
0.000
0.000
0.000
Plot of vertical stresses with time showing convergence of stress osciallations
Vertical stresses component results at t = 0.2s for USF linear elastic model