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. 2009 Oct 1;106(41):17383–17388. doi: 10.1073/pnas.0907455106

Table 1.

Comparison of kinetic ΔG with equilibrium ΔG and β-Tanford values

CTPRan ΔG0→jH2O (kcal mol−1)* ΔGI-UH2O (kcal mol−1) ΔGI-NH2O (kcal mol−1) ΔGU-NH2O (kcal mol−1)§ βT TS1 βT Intermediate βT TS2
2 3.3 ± 0.9 - - 2.8 ± 0.4 0.56 - -
3 6.1 ± 1.2 4.0 ± 1.5 5.1 ± 1.5 9.1 ± 2.1 0.35 0.49 0.58
4 9.0 ± 1.5 3.8 ± 1.4 5.9 ± 1.7 9.8 ± 2.2 0.37 0.47 0.49
5 11.8 ± 1.9 4.2 ± 1.2 6.4 ± 2.4 10.6 ± 2.7 0.30 0.45 0.46
6 14.7 ± 2.2 4.3 ± 0.6 10.7 ± 2.5 15.0 ± 2.6 0.24 0.34 0.36
8 20.4 ± 2.8 4.0 ± 0.3 14.6 ± 2.6 18.6 ± 2.6 0.16 0.25 0.26
10 26.1 ± 3.5 4.3 ± 0.4 17.8 ± 3.7 22.2 ± 3.7 0.15 0.23 0.23

All errors from kinetic data are obtained from propagation of errors obtained from the fitting of the data (shown in Table S3).

*Values averaged from the Ising fit of all equilibrium data and using Eq. 5 (SI Appendix); errors obtained from the propagation of a standard deviation of 3 averaged data sets (shown in Table S2).

Calculated from kinetic data using ΔGU-1H2O = −RTln(kIUH2O/kUIH2O).

Calculated from kinetic data using ΔGI-NH2O = − RTln(kNIH2O/kINH2O).

§Calculated from kinetic data using ΔGU-NH2O = − RTln(kIUH2OkNIH2O/kUIH2OkINH2O). βT values were obtained using Σxmximi, where Σxmx is the sum of kinetic m-values between the unfolded state and state X on the reaction coordinate, and Σimi is the sum of all kinetic m-values along the reaction coordinate.