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The phase fraction and velocity measured from two techniques are compared.
We compare the results obtained from two techniques for all reference years and combinations of two shot years.
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Open image in new window Fig. 8 a Comparison between measured with calculated water saturation from four techniques, and b relative error between four techniques.
Figure 1 shows a comparison of disparity maps from three techniques that support spatio-temporal disparity estimation, including TDCBG [23], PRSM [28], and our method.
The frequency of occurrences of the genes along with means of coefficients and standard errors over 100 replicates, obtained from three techniques, was shown in Table 1.
These insights emerge from the complementary data extracted from the two techniques, such as 'dry' and 'wet' mass values, layer solvation, thickness, density and viscoelastic properties.
The results from these two techniques were compared with each other and with experimental data obtained from wind-tunnel and towing-tank tests on a 1 70 scale model.
We directly compare seismic velocity changes from these two techniques.
The results from these two techniques are compared and discussed.
In all cases, the results from these two techniques are consistent with each other.
Hence, the results from these two techniques are consistent with each other.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com