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Such a variation trend of surface energy density is contrary to the prediction of existing theoretical models but well consistent with the previously atomistic simulations and density functional calculations.
The experimental and theoretical results plotted in Fig. 6 illustrate that the experimental breakdown pressures follow a variation trend similar to theoretical breakdown pressures, but that the values appear much lower in the experimental results.
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Plotting the capillary desaturation curves for both wetting and non-wetting phases through different capillary numbers demonstrate a normal variation trend for the non-wetting phase (approximately a semi-log relationship), while the wetting phase is greatly affected by the capillary end effect and relative permeability variations in the porous medium.
The vertical permeabilities have a similar variation trend with the contents of sand and silt, but an inverse correlation with the mud content (Fig. 3).
Such a different variation trend of the fracture strength in the two directions is attributed to the presence of residual stress inside the material arisen from the fabrication process.
It was very interesting to find that the gasoline compositions for both groups had a similar variation trend.
Even for T = 273 K, the fitting curve by Equation 1 shows a similar variation trend as the measured one.
The chloroform bitumen content of source sediments shows a similar variation trend among distinct sedimentary facies (Fig. 3; Table 3).
The modulus changes with porosity, causing a different variation trend of velocity versus porosity from the general result.
As shown in Fig. 3b, during the period before mining, the steady soil infiltration rate showed a similar variation trend as the initial soil infiltration rate, while in the period 1 year after mining, the steady soil infiltration rate showed a negative relationship with soil bulk density, occurring in the following order: P. simonii > A.
The J sc and V oc exhibit a similar variation trend with increasing N d, i.e., J sc first decreases then increases and finally decreases (a peak around N d = 4.0 × 1017 cm−3), V oc first increases and then decreases (a peak around N d = 3.07 × 1016 cm−3 ).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com