A modified form of the Redlich–Kwong equation was proposed by Soave. It takes the form : p = \frac{R\,T}{V_\text{m}-b} - \frac{a \alpha}{V_\text{m}\left(V_\text{m}+b\right)} : a = \frac{\Omega_a\,R^2 T_\text{c}^2}{P_\text{c}} = \frac{0.42748\,R^2 T_\text{c}^2}{P_\text{c}} : b = \frac{\Omega_b\,R T_\text{c}}{P_\text{c}} = \frac{0.08664\,R T_\text{c}}{P_\text{c}} : \alpha = \left(1 + \left(0.48508 + 1.55171\,\omega - 0.15613\,\omega^2\right) \left(1-T_\text{r}^{0.5}\right)\right)^2 : T_\text{r} = \frac{T}{T_\text{c}} : \Omega_a = \left[9\left(2^{1/3}-1\right)\right]^{-1} \approx 0.42748 : \Omega_b = \frac{2^{1/3}-1}{3} \approx 0.08664 where
ω is the
acentric factor for the species. The formulation for \alpha above is actually due to Graboski and Daubert. The original formulation from Soave is: : \alpha = \left(1 + \left(0.480 + 1.574\,\omega - 0.176\,\omega^2\right) \left(1-T_\text{r}^{0.5}\right)\right)^2 for hydrogen: : \alpha = 1.202 \exp\left(-0.30288\,T_\text{r}\right). By substituting the variables in the reduced form and the
compressibility factor at critical point : \{p_\text{r}=p/P_\text{c}, T_\text{r}=T/T_\text{c}, V_\text{r}=V_\text{m}/V_\text{c}, Z_\text{c}=\frac{P_\text{c} V_\text{c}}{R T_\text{c}}\} we obtain : p_\text{r} P_\text{c} = \frac{R\,T_\text{r} T_\text{c}}{V_\text{r} V_\text{c}-b} - \frac{a \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} V_\text{c}\left(V_\text{r} V_\text{c+}b\right)} = \frac{R\,T_\text{r} T_\text{c}}{V_\text{r} V_\text{c}-\frac{\Omega_b\,R T_\text{c}}{P_\text{c}}} - \frac{\frac{\Omega_a\,R^2 T_\text{c}^2}{P_\text{c}} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} V_\text{c}\left(V_\text{r} V_\text{c}+\frac{\Omega_b\,R T_\text{c}}{P_\text{c}}\right)} = : = \frac{R\,T_\text{r} T_\text{c}}{V_\text{c}\left(V_\text{r}-\frac{\Omega_b\,R T_\text{c}}{P_\text{c} V_\text{c}}\right)} - \frac{\frac{\Omega_a\,R^2 T_\text{c}^2}{P_\text{c}} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} V_\text{c}^2\left(V_\text{r}+\frac{\Omega_b\,R T_\text{c}}{P_\text{c} V_\text{c}}\right)} = \frac{R\,T_\text{r} T_\text{c}}{V_\text{c}\left(V_\text{r}-\frac{\Omega_b}{Z_\text{c}}\right)} - \frac{\frac{\Omega_a\,R^2 T_\text{c}^2}{P_\text{c}} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} V_\text{c}^2\left(V_\text{r}+\frac{\Omega_b}{Z_\text{c}}\right)} thus leading to : p_\text{r} = \frac{R\,T_\text{r} T_\text{c}}{P_\text{c} V_\text{c}\left(V_\text{r}-\frac{\Omega_b}{Z_\text{c}}\right)} - \frac{\frac{\Omega_a\,R^2 T_\text{c}^2}{P_\text{c}^2} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} V_\text{c}^2\left(V_\text{r}+\frac{\Omega_b}{Z_\text{c}}\right)} = \frac{T_\text{r}}{Z_\text{c}\left(V_\text{r}-\frac{\Omega_b}{Z_\text{c}}\right)} - \frac{\frac{\Omega_a}{Z_\text{c}^2} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} \left(V_\text{r}+\frac{\Omega_b}{Z_\text{c}}\right)} Thus, the Soave–Redlich–Kwong equation in reduced form only depends on
ω and Z_\text{c} of the substance, contrary to both the VdW and RK equation which are consistent with the
theorem of corresponding states and the reduced form is one for all substances: : p_\text{r} = \frac{T_\text{r}}{Z_\text{c}\left(V_\text{r}-\frac{\Omega_b}{Z_\text{c}}\right)} - \frac{\frac{\Omega_a}{Z_\text{c}^2} \alpha\left(\omega, T_\text{r}\right)}{V_\text{r} \left(V_\text{r}+\frac{\Omega_b}{Z_\text{c}}\right)} We can also write it in the polynomial form, with: : A = \frac{a \alpha P}{R^2 T^2} : B = \frac{bP}{RT} In terms of the compressibility factor, we have: : 0 = Z^3-Z^2+Z\left(A-B-B^2\right) - AB. This equation may have up to three roots. The maximal root of the cubic equation generally corresponds to a vapor state, while the minimal root is for a liquid state. This should be kept in mind when using cubic equations in calculations, e.g., of
vapor-liquid equilibrium. In 1972 G. Soave replaced the \frac{1}{\sqrt{T}} term of the Redlich–Kwong equation with a function
α(
T,
ω) involving the temperature and the acentric factor (the resulting equation is also known as the Soave–Redlich–Kwong equation of state; SRK EOS). The
α function was devised to fit the
vapor pressure data of hydrocarbons and the equation does fairly well for these materials. Note especially that this replacement changes the definition of
a slightly, as the T_\text{c} is now to the second power. == Volume translation of Peneloux et al. (1982) ==