Theoretical Study ofN-Demethylation of SubstitutedN,N-Dimethylanilines by Cytochrome P450:  The Mechanistic Significance of Kinetic Isotope Effect Profiles

2007 ◽  
Vol 111 (26) ◽  
pp. 7700-7710 ◽  
Author(s):  
Yong Wang ◽  
Devesh Kumar ◽  
Chuanlu Yang ◽  
Keli Han ◽  
Sason Shaik

2009 ◽  
Vol 15 (34) ◽  
pp. 8492-8503 ◽  
Author(s):  
Chunsen Li ◽  
Wei Wu ◽  
Kyung-Bin Cho ◽  
Sason Shaik


2015 ◽  
Vol 641 ◽  
pp. 158-162 ◽  
Author(s):  
Fethi Khaled ◽  
Binod Raj Giri ◽  
Milán Szőri ◽  
Béla Viskolcz ◽  
Aamir Farooq






2007 ◽  
Vol 5 (4) ◽  
pp. 1019-1063 ◽  
Author(s):  
David Krinkin

AbstractActivated diffusion of water between macromolecules in swollen cellulose is accompanied by anomalously high kinetic isotope effects of oxygen. The separation factor of heavy-oxygen water (H218O /H216O) is thousands of permilles instead of tens of permilles according to modern Absolute Rate Theory. This anomalous separation under usual conditions is disguised by the opposing process of very fast equalization to equilibrium through water-filled cellulose pores. This process is quicker by approximately 3 orders of magnitude than diffusion through the cellulose body. As a consequence, this opposition-directed equalization virtually eliminates the results of isotope separation. To reveal this anomaly it is necessary to suppress equalization, which was the primary problem for both discovery of this anomaly and its investigation. The method of investigating the anomalous separation in cellulose was developed with suppression of this negative influence. Discussion of the theoretical nature of the anomalous kinetic isotope effect is presented. This theoretical study would probably permit the discovery and use for isotope separation of the anomalously high isotope effect for other chemical elements, in particular, for those heavier than oxygen.





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