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The equations used to obtain μ b ′ and to draw the limb of the cross plot (Figure 4) to constrain λ are explained below.
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Figure 2b shows a surface potential map, obtained with KPFM and reveals a pronounced difference (20 mV) in surface potential on the border of two thiols (cross-section plot, Figure 2d).
Cross plots of Figures 9 to 11 for fixed disk diameter D = 0.100 m and for different concentrations are shown in Figure 12a,b,c.
Site matched values of tissue stiffness (elastic modulus) and MD from Calc3 and Calc4 are cross-plotted in Figure 8d.
Figure 8 shows a cross plot between the experimental viscosity data and the predicted viscosity using EoS.
We assumed that the clay volume primarily consisted simply of illite and the rest clay minerals and figure out the volume of illite by using neutron-density cross plot.
Figure 4 Cross plots between the λ and effective coefficient of basal friction.
The specific heat capacity used in the study of Hyndman et al. (1979) was therefore considered suitable for use with the materials of our core samples retrieved from the JFAST borehole in the west Pacific. Figure 5 Cross plots of thermal diffusivity and thermal conductivity.
Figure 1 shows the above-mentioned cross plots.
We obtained the parameters by drawing cross plots between the λ and effective coefficient of basal friction μ b ′ (Figure 4) by referring to Wang et al. ([2010]).
Lactate crosses the membrane through a pore, as it is evident by the low energy of activation (Ea = 7.18±0.7 kcal/mol) estimated from the Arrhenius plots (figure 4D).
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