scholarly journals Assessment of approximate computational methods for conical intersections and branching plane vectors in organic molecules

2014 ◽  
Vol 141 (12) ◽  
pp. 124122 ◽  
Author(s):  
Alexander Nikiforov ◽  
Jose A. Gamez ◽  
Walter Thiel ◽  
Miquel Huix-Rotllant ◽  
Michael Filatov
2021 ◽  
Author(s):  
Alondra López-Colón ◽  
Mariela E. Santiago-Mercado ◽  
Jonathan I. Aguirre-Santiago ◽  
Ariana de Jesús-Hernández ◽  
Jenlyan Negrón-Hernández ◽  
...  

In the discovery process of new drugs and the development of novel therapies in medicine, computational modeling is a complementary tool for the design of new molecules by predicting for example their solubility in different solvents. Here, we benchmarked several computational methods to calculate the partition coefficients of a diverse set of 161 organic molecules with experimental logP values obtained from the literature. In general, density functional theory methods yielded the best correlations and lower average deviations. Although results are obtained faster with semiempirical and molecular mechanics methodologies, these methods yielded higher average deviations and lower correlation coefficients than hybrid density functional theory methods. We recommend the use of an empirical formula to correct the calculated values with each methodology tested.


2020 ◽  
Vol 221 ◽  
pp. 245-264 ◽  
Author(s):  
Francesco Segatta ◽  
Artur Nenov ◽  
Silvia Orlandi ◽  
Alberto Arcioni ◽  
Shaul Mukamel ◽  
...  

In the present contribution we introduce an accurate theoretical approach for the simulation of NEXAFS spectra of organic molecules, employing azobenzene as a test case.


Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.


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