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The functionally graded material properties follow a power-law function.
It is assumed that material properties follow power law distributions through thickness direction.
It is assumed that material properties follow exponential distributions through thickness direction.
It is assumed that material properties follow exponential distributions through beam thickness.
The heterogeneity of rocks at a mesoscopic level is considered by assuming that the material properties follow the Weibull distribution.
It is assumed that the material properties follow a power-law variation through the thickness direction of the beams.
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It is assumed that the materials properties follow an exponential variation through the thickness direction.
This discretization procedure accommodates arbitrarily shaped cross-sections of inhomogeneous anisotropic material properties that follow the pretwist rotation rate.
These integral conservation properties follow from material conservation of potential vorticity in the continuous shallow water equations.
Let α and C be the thermal boundary conductance and the perimeter of the fin cross sections, respectively, m be linked to geometry, and material properties as follows: (15).
The experimental set-up, connection configurations and material properties are introduced followed by a detailed account of the test results and observations.
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