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The Colburn factor j, friction factor f and 'point of transition' were calculated from the experimental data.
The 350°C depths (isotherm) along with the locations (depths) of the brittle-ductile transition were calculated during this study, as shown in Figure 7. Figure 9 Schematic figure showing the relationship between seismicity and temperature.
First, the radius vectors r⃗ describing the coordinates of all fluorophore centers and the unit vectors u⃗ describing the directions of all electronic transition were calculated by a computer program.
Probabilities of transition were calculated based on the disease severity classes.
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The ice age- gas age difference (Δage) at the firn-ice transition is calculated to be 182+3−9 yr.
Collision energy for each transition was calculated according to standard QTRAP 5500 settings.
The change in ellipticity was measured at 225 and 229 nm for Lig A9 and A10 and the mid-point of thermal unfolding transition was calculated.
The enthalpy change associated with alkyl chain phase transition was calculated by using the area under the curve function in Igor Pro 6.
Tm corresponding to the midpoint for the protein unfolding transition was calculated by fitting the increasing phase of the melting curve by nonlinear least-squares regression using sigmoidal equations (GraphPad Prism).
The respective temperatures of transitions were calculated.
The electronic excitation energies and intensities of the six lowest-energy spin allowed transitions were calculated using time dependent density functional theory (TD-DFT).
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