Sentence examples for plane of the core from inspiring English sources

Due to the severe transverse variations in the material properties and the discontinuity of the first order derivative of material parameters at the middle plane of the core, the problem is challenging for point discrete methods and thus is solved by the weak form quadrature element method (QEM).

The second model, due to Frostig, assumes that the plane section of the core in the shear substructure remains vertical and the face sheets are subjected to in-plane deformation as well as flexural ones.

The latter ligands are arranged on opposite sides of the plane of the cluster core, almost perpendicular to the plane.

The defects thus generated greatly influence the out-of-plane stiffness of the core because the folded edges do not remain straight.

First shear deformation theory (FSDT) is used for the facesheets and cubic functions are assumed for the transverse and in-plane displacements of the core.

Parametric studies are performed in order to investigate the influence of the ply angle of face sheets and the core, in-plane rigidity of the core, transverse shear rigidity and boundary conditions on modal density.

The governing equations are derived by applying the Hamilton's principle, where in-plane rigidity of the core is considered and the material and reference axes are not limited to be identical to each other.

The core consists of an alternating stacked sequence of folded sheets in the Miura (double-corrugated) pattern, with the stack oriented such that the folding kinematics define the out-of plane compressive strength of the core.

The displacement of the iron center from the mean plane of the C20N4 porphyrinato core is contracted from 0.52 Å (in 1) to 0.27, 0.30, and 0.31 Å in 2, 3, and 4, respectively.

The formulation has been applied as an illustration, to the laminated sandwich plates made up of transversely isotropic laminae with the axes of symmetry lying in the plane of the lamina and core in-between.

The estimated dip angle of the bedding plane at the core site is approximately 12°, which suggests that the foliation plane reasonably coincides with the bedding plane.