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The presented paper describes procedures of numerical upscaling and experience with X-ray CT based finite element (FEM) analysis of properties of geocomposites.
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The procedure of numerical calculation shows that the formulation presented here is simple and direct.
The suggested procedure of numerical solution of a local minimum problem allows converging towards the solution with the desired accuracy in a fast and effective way.
When the transmitting frequency is fixed at 2 MHz and the dielectric constant of an earth formation is changed during the procedure of numerical simulation, there are also changes in the amplitude ratios and phase differences of the receiving signal and these variations in the high-resistivity formation are more sensitive than in low-resistivity formation.
However, if the dynamics of isotopomer distribution is simulated in the conditions of metabolic steady state, the procedure of numerical solution could be simplified so that the general kinetic equations (1) could be solved separately from the solution for isotopomers (3).
Thereafter, the calculation of the element variation and collectivity synthesis is done, and the procedures of the numerical simulation of vulcanization process are described in detail.
We developed a framework of procedures for numerical optimization in spatially explicit dynamic ecosystem simulation models.
The procedure of the numerical analysis is described in Appendix A Numerical methods in the case of the homogeneous assignment rule.
The procedure of the numerical analysis is described in Appendix B Numerical methods in the case of the heterogeneous assignment rule.
This is a procedure of effective numerical transformation of the one-dimensional scattering profiles into three-dimensional model structures.
The response surface approximate functions between the output stress/strain values and the major packaging parameters are produced in the design of experiment (DOE) procedure of the numerical simulations.
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