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The physical equation based upon the model of the pore size distribution did not allow exact fitting of the modelled data to the experimental data due to the rigidity and simplicity of the physical model when compared to the real soil porous system.
Furthermore, in this paper, we compared our modeling data to the experimental data in the under agarose assay [12], [13] and the gradient profile of LTB4 in the under agarose assays at 30 min can be effectively fitted by the power function with the power n = 3.35 (File S1).
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Known complexes in the CYC2008 dataset served as a gold-standard data to evaluate the experimental results.
The best data fit to the experimental data was obtained by the homogenous single-phase model (HSPM).
Examining the figures and data indicate good fitting of the experimental data to the model.
The score represents the sensitivity of the experimental data to the i th physical parameter.
Line shows best fit of the experimental data to the 1 1 binding model.
In this investigation, Φ was obtained by fitting the experimental data to the percolation theory.
A fit of the experimental data to the spectral retardance function in Eq. (5) was performed.
It consists of fitting the experimental data to the GLM computation model.
Kinetic parameters were estimated by fitting the experimental data to the models.
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