scholarly journals Medical and Biochemical Application of Infrared Absorption Spectra. IV. Studies on Gall Stones by Infrared Spectra and their New Classification

1960 ◽  
Vol 8 (9) ◽  
pp. 771-777 ◽  
Author(s):  
Goro Chihara ◽  
Emiko Kobayashi ◽  
Ayako Mizushima ◽  
Kimiko Shirakuma ◽  
Haruo Kameda
1965 ◽  
Vol 38 (1) ◽  
pp. 219-226 ◽  
Author(s):  
E. Suito ◽  
M. Arakawa

Abstract Infrared spectra of 33 kinds of commercial reinforcing fillers were measured by use of the KBr pellet method in connection with studies of the filler effect in rubber-filler systems. Characteristic absorptions of individual fillers are discussed in relation to their method of preparation.


1970 ◽  
Vol 53 (2) ◽  
pp. 275-287
Author(s):  
J -Y T Chen ◽  
Nancy C Oates ◽  
David Firestone

Abstract The infrared spectra of five 3,5-dialkyl phenols, six 2-allyl-3,5-dialkyl phenols, and five 4-allyl-3,5-dialkyl phenols are presented. The characteristic infrared absorption frequencies are tabulated in correlation charts. The hyperconjugation and mass effects of substituent groups are discussed.


1982 ◽  
Vol 47 (4) ◽  
pp. 1100-1111 ◽  
Author(s):  
Jaroslav Majer ◽  
Vladimír Kadeřábek

Infrared absorption spectra of N-substituted derivatives of 2,4-dinitro- and 2,6-dinitroanilines have been measured and interpreted from the point of view of bond and sterical interactions of the substituted amino groups with the both nitro groups.


1968 ◽  
Vol 5 (2) ◽  
pp. 223-230 ◽  
Author(s):  
J. F. Dormaar

Saxicolous lichens and associated mosses, and their weathered and fresh rock zones, were collected from a number of locations. All material was treated with hydrogen peroxide and infrared spectra of the remanining mineral matter were obtained.Spectra of the mineral matter obtained from the lichens and mosses differ generally from those of the substrata. There is evidence that quartz and dioctahedral structures could be products of weathering of rocks by lichens and mosses. It is likely that saxicolous lichens obtain at least part of their minerals from the substrata. There is no indication of the presence of magnesium or of carbonates in the peroxidized material of lichens obtained from calcareous or dolomitic substrata. Peroxidation of the organic tissues leads, in the presence of calcium, to the formation of calcium oxalate; the relative intensities of the bands related to calcium oxalate, in particular those at 1325 and 780 cm−1, may be used to assess the amount of calcium present. It is suggested that this change in intensity may be a useful criterion in evaluating the transformation of Chernozemic humic acids to Podzolic humic acids in soil.


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