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In the numerical calculation, fundamental density functions and polynomials are used to approximate unknown body force densities.
In order to satisfy the boundary conditions along the ellipsoidal boundaries, eight kinds of fundamental density functions proposed in our previous papers are applied.
In the numerical analysis, unknown body force densities are approximated by the products of the fundamental density functions and power series, where the fundamental density functions are chosen to express singular behavior along the crack front of the interface crack exactly.
In the numerical analysis, unknown body force densities are approximated by the products of the fundamental density functions and power series, where the fundamental densities are chosen to express a two-dimensional interface crack exactly.
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Here, the fundamental densities are chosen to represent the symmetric stress singularity, and the skew-symmetric stress singularity.
To obtain the GSIF accurately, the unknown body force densities are expressed as piecewise smooth functions using fundamental densities and power series.
The quantity which is fundamental to density based crystal plasticity models is the slip system specific dislocation density vector ρ.
I.B.M. plans to announce on Monday that its researchers have succeeded in expanding what was thought to be a fundamental data-density limit in the most common form of computer storage technology.
[C2.] I.B.M. Expands Storage of Data I.B.M. plans to announce today that its researchers have succeeded in expanding what was thought to be a fundamental data-density limit in the most common form of computer storage technology, increasing the amount of data that can be held on a disk.
C2 Big Blue Pushing Data Horizon I.B.M. plans to announce today that its researchers have succeeded in expanding what was thought to be a fundamental data-density limit in the most common form of computer storage technology, increasing the amount of data that can be held on a disk.
Our design allowed us to analyse the effects on the fundamental pgr-density relationship of variation between squares and years.
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