Investigation by infra-red spectroscopic methods of deuterium exchange properties of aerosil silicas

1966 ◽  
Vol 62 ◽  
pp. 801 ◽  
Author(s):  
F. H. Hambleton ◽  
J. A. Hockey ◽  
J. A. G. Taylor
1984 ◽  
Vol 48 (346) ◽  
pp. 113-117 ◽  
Author(s):  
P. J. Loveland ◽  
V. C. Bendelow

AbstractAn occurrence of a celadonite-like mineral in a weathered basalt in the Lake District has been investigated by X-ray diffraction, X-ray fluorescence, electron microprobe, and infra-red spectroscopic methods. The bulk composition of the mineral corresponds to an aluminous-glauconite. The data show that the mineral is most probably a celadonite-muscovite or celadonite-illite mixture, although a celadonite-phengite cannot be entirely discounted. Approximately 10% smectite layers are also present. The results suggest that re-examination of many aluminous glauconites may show them to be mixtures of this type.


1967 ◽  
Vol 23 (10) ◽  
pp. 490-496
Author(s):  
Gabriel Wlodarski ◽  
Wojciech Kozlowski ◽  
Stefania Siewierska
Keyword(s):  

Author(s):  
C. Wolpers ◽  
R. Blaschke

Scanning microscopy was used to study the surface of human gallstones and the surface of fractures. The specimens were obtained by operation, washed with water, dried at room temperature and shadowcasted with carbon and aluminum. Most of the specimens belong to patients from a series of X-ray follow-up study, examined during the last twenty years. So it was possible to evaluate approximately the age of these gallstones and to get information on the intensity of growing and solving.Cholesterol, a group of bile pigment substances and different salts of calcium, are the main components of human gallstones. By X-ray diffraction technique, infra-red spectroscopy and by chemical analysis it was demonstrated that all three components can be found in any gallstone. In the presence of water cholesterol crystallizes in pane-like plates of the triclinic crystal system.


Sign in / Sign up

Export Citation Format

Share Document