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The resulting binding isotherm can be fit to three linear regions.
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The adsorption isotherm can be described by Freundlich isothermal model.
Nevertheless, acquisition of adsorption isotherm can be very laborious.
Temkin isotherm can be expressed in linear form: q_{text{e}} = B_{text{T}} ln K_{text{T}} + B_{text{T}} ln C_{text{e}}, (15 where R is the gas constant (8.314 J/mol/K), T the absolute temperature in Kelvin, B T is the constant related to the heat of adsorption and K T (l/min) is the Temkin isotherm binding constant.
The Freundlich isotherm can be described as follows: (6) q e = K F C e 1 / n.
Mixing processes are generally more active in coastal areas, so that isotherms can be expected to slope downward toward shore.
It is clear that the adsorption isotherms can be fitted well using two isotherm models.
By plotting the freezing line, isotherms can be useful in determination of precipitation type.
Isotherms can be drawn on these maps, which are lines of equal temperature.
While a binding isotherm can provide useful information on electrostatics and cooperative binding behavior of the multivalent protein ligand interaction, it overlooks the concentration dependence of the binding kinetics.
The equilibrium binding constant, b T (mol/g) which is the Temkin isotherm constant, can be determined from the Temkin isotherm model.
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