The PM3 method uses the same formalism and equations as the AM1 method. The only differences are:
1) PM3 uses two Gaussian functions for the core repulsion function, instead of the variable number used by AM1 (which uses between one and four Gaussians per element);
2) the numerical values of the parameters are different. The other differences lie in the philosophy and methodology used during the parameterization: whereas AM1 takes some of the parameter values from spectroscopical measurements, PM3 treats them as optimizable values.
The original PM3 publication included parameters for the following elements: H, C, N, O, F, Al, Si, P, S, Cl, Br, and I.
The PM3 implementation in the SPARTAN program includes PM3tm with additional extensions for transition metals supporting calculations on Ca, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Zr, Mo, Tc, Ru, Rh, Pd, Hf, Ta, W, Re, Os, Ir, Pt, and Gd. Many other elements, mostly metals, have been parameterized in subsequent work.
A model for the PM3 calculation of lanthanide complexes, called Sparkle/PM3, was also introduced.
References
Stewart, James J. P. (1989). "Optimization of parameters for semiempirical methods I. Method". J. Comput. Chem. 10 (2): 209–220. doi:10.1002/jcc.540100208. S2CID36907984.
Stewart, James J. P. (1989). "Optimization of parameters for semiempirical methods II. Applications". J. Comput. Chem. 10 (2): 221–264. doi:10.1002/jcc.540100209. S2CID98850840.
Stewart, James J. P. (2004). "Optimization of parameters for semiempirical methods IV: Extension of MNDO, AM1, and PM3 to more main group elements". Journal of Molecular Modeling. 10 (2): 155–64. doi:10.1007/s00894-004-0183-z. PMID14997367. S2CID11617476.
For a recent review, Stewart, J. J. P. (1998). "PM3". Encyclopedia of Computational Chemistry. Wiley.
Freire, Ricardo O.; Rocha, Gerd B.; Simas, Alfredo M. (2006). "Modeling rare earth complexes: Sparkle/PM3 parameters for thulium(III)". Chemical Physics Letters. 425 (1–3): 138–141. Bibcode:2006CPL...425..138F. doi:10.1016/j.cplett.2006.04.103.
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