Raman spectroscopic studies on the structural changes of poly(3-methylthiophene) during heating and cooling processes

2002 ◽  
Vol 47 (21) ◽  
pp. 1791-1793
Author(s):  
Feng’en Chen ◽  
Jiaxin Zhang ◽  
Mingxiao Fu ◽  
Gaoquan Shi
2010 ◽  
Author(s):  
Jonathan Dusting ◽  
Grant Webster ◽  
Stavroula Balabani ◽  
Ewan W. Blanch ◽  
P. M. Champion ◽  
...  

2010 ◽  
Vol 24 (01) ◽  
pp. 51-58 ◽  
Author(s):  
S. C. BAIDOC ◽  
I. ARDELEAN

Structural analysis of x Ag 2 O · (100-x)[ B 2 O 3 · As 2 O 3] glass system, with 0 ≤ x ≤ 10 mol%, was performed by means of FT-IR and Raman spectroscopies. The purpose of this work is to investigate the structural changes that appear in the B 2 O 3 · As 2 O 3 glass matrix with the addition and increase of silver ion content. Boroxol rings, pyro-, ortho-, di-, tri-, tetra- and penta-borate groups, structural units characteristic to As 2 O 3 were found in the structure of the studied glasses. FT-IR spectroscopy measurements show that BO 3 units are the main structural units of the glass system. The presence of structural units characteristic to Ag 2 O were not directly evidenced by FT-IR spectroscopy. The Raman analysis leads to similar conclusions as the FT-IR measurements.


2012 ◽  
Vol 57 (4) ◽  
pp. 951-974 ◽  
Author(s):  
Andrzej Nowakowski ◽  
Mariusz Młynarczuk

Abstract Temperature is one of the basic factors influencing physical and structural properties of rocks. A quantitative and qualitative description of this influence becomes essential in underground construction and, in particular, in the construction of various underground storage facilities, including nuclear waste repositories. The present paper discusses the effects of temperature changes on selected mechanical and structural parameters of the Strzelin granites. Its authors focused on analyzing the changes of granite properties that accompany rapid temperature changes, for temperatures lower than 573ºC, which is the value at which the β - α phase transition in quartz occurs. Some of the criteria for selecting the temperature range were the results of measurements carried out at nuclear waste repositories. It was demonstrated that, as a result of the adopted procedure of heating and cooling of samples, the examined rock starts to reveal measurable structural changes, which, in turn, induces vital changes of its selected mechanical properties. In particular, it was shown that one of the quantities describing the structure of the rock - namely, the fracture network - grew significantly. As a consequence, vital changes could be observed in the following physical quantities characterizing the rock: primary wave velocity (vp), permeability coefficient (k), total porosity (n) and fracture porosity (η), limit of compressive strength (Rσ1) and the accompanying deformation (Rε1), Young’s modulus (E), and Poisson’s ratio (ν).


1984 ◽  
Vol 115 ◽  
pp. 473-476 ◽  
Author(s):  
Pham V. Huong ◽  
D. Mencaraglia ◽  
P. Andro ◽  
J. Baixeras

1982 ◽  
Vol 25 (6A) ◽  
pp. 685-687 ◽  
Author(s):  
E J Samuelsen ◽  
U Buchenau ◽  
M Dieter ◽  
K Ehrhardt ◽  
E Fjær ◽  
...  

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