scholarly journals Exploring molecular reorientations in amorphous and recrystallized felodipine at the microscopic level

RSC Advances ◽  
2020 ◽  
Vol 10 (61) ◽  
pp. 37346-37357
Author(s):  
A. Pajzderska ◽  
J. Jenczyk ◽  
J. P. Embs ◽  
J. Wąsicki

Molecular reorientations were studied in amorphous, partially and fully recrystallized felodipine using a set of experimental methods: high-resolution solid-state nuclear magnetic resonance (NMR), relaxometry NMR and quasielastic neutron scattering (QENS).

1991 ◽  
Vol 77 (1) ◽  
pp. 149-161 ◽  
Author(s):  
Claudine Dorémieux-Morin ◽  
Claudine Martin ◽  
Jean-Marie Brégeault ◽  
Jacques Fraissard

Clay Minerals ◽  
1986 ◽  
Vol 21 (5) ◽  
pp. 879-897 ◽  
Author(s):  
M. A. Wilson ◽  
S. A. McCarthy ◽  
P. M. Fredericks

AbstractThe structure of synthetic aluminosilicates prepared at pH 6 has been investigated by 29Si and 27Al high-resolution solid-state nuclear magnetic resonance (NMR) spectroscopy. Fourier transform infrared (FTIR) spectroscopy and electron microscopy have also been used to characterize the products. The amount of Si and Al in protoimogolite, disordered allophane and other structures has been measured. There is a fair correlation between the intensity of the 349 cm−1 band in the FTIR spectra and the proportion by weight of protoimogolite Si measured by NMR. It is shown that disordered allophanes have similar structures to those proposed by van Reeuwijk and de Villiers (Soil Sci. Soc. Am. Proc. 32 (1968) 238–240), i.e. octahedral Al surrounding a tetrahedral core. Moreover, it is clear that at high Al:Si ratios (⩾1:1), protoimogolite can compete with disordered allophane precursors for aluminum. The driving forces for formation of protoimogolite rather than allophane appear to be long range Al-Al repulsive forces through oxygen.


1996 ◽  
Vol 101 (1) ◽  
pp. 71-79
Author(s):  
Hazime Saitǒ ◽  
Satoru Tuzi ◽  
Katsuyuki Nishimura ◽  
Akira Fukutani ◽  
Akira Naito

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