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Finally, kinetics parameters (V max and K m) were determined using Michaelis Menten models.
The melting temperature (T m ) and enthalpy of fusion (ΔH m ) were determined from the DSC endotherms.
Simultaneously, the maximum photo-oxidizable P700 (P m ) were determined with saturation pulses using the Dual PAM-100 system.
Analytical enhancement factor (AEF) of Au substrates between 105 and 106 and limits of detection (LOD) of TMPyP ∼5 × 10−8 M were determined.
When the optimum NMBI or TBP-based electrolyte compositions (0.45 M) were determined (respectively), 0.05 M of GuNCS (Aldrich) was added in each system [16, 17].
Hydraulic conductivities in the fractured zone between 2850 and 3100 m were determined to be up to 6·10−8 m s−1 (Sausse et al. 2006).
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When α ≠ β, λ m is determined by the following recursion formulas: (4.6) (4.6).
where the parameter m is determined in such a way that 0 ≤ λ X (x) < 1.
Values of Freundlich isotherm constants b and m are determined from the plot.
As n m is already known, the total marginal land used in traditional agriculture N m is determined.
The material softening parameter, m is determined from the finite element simulation of a single element model.
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