On the evolution of solutions of mixed problems in thermoelasticity of porous bodies with dipolar structure

Author(s):  
Marin Marin ◽  
Andreas Öchsner ◽  
Mohamed I. A. Othman
2021 ◽  
Vol 2021 (1) ◽  
Author(s):  
M. Marin ◽  
S. Vlase ◽  
C. Carstea

AbstractWe consider the mixed problem with boundary and initial data in thermoelasticity of porous bodies with dipolar structure. By generalizing some known results developed by Dafermos in a more simple case of the classical theory of elasticity, we prove new theorems in which we address the issues regarding the uniqueness and existence of a solution with finite energy of the respective problem after we define this type of solution.


1987 ◽  
Vol 52 (11) ◽  
pp. 2699-2709 ◽  
Author(s):  
Dalimil Dvořák ◽  
Zdeněk Arnold

Reaction of arylmethylenemalonaldehydes with tributylphosphine and tertiary amines affords compounds of dipolar structure whereas reaction with primary and secondary amines leads to 1,4-addition products. Salts of nucleophilic inorganic anions add to arylmethylenemalonaldehydes under formation of salts of substituted malonaldehydes.


1978 ◽  
Vol 34 (3) ◽  
pp. 974-975 ◽  
Author(s):  
J. Galloy ◽  
J. P. Declercq ◽  
M. Van Meerssche
Keyword(s):  

1978 ◽  
Vol 17 (9) ◽  
pp. 668-671 ◽  
Author(s):  
V. V. Skorokhod ◽  
L. I. Tuchinskii

1952 ◽  
Vol 30 (4) ◽  
pp. 348-371 ◽  
Author(s):  
E. A. Flood ◽  
R. H. Tomlinson ◽  
A. E. Leger

The flow rates of the vapors of benzene, ethyl chloride, diethyl ether, methanol, and water through activated carbon rods have been found to exceed, considerably, flow rates calculated by classical equations. The excess flow rates show maxima in widely different relative pressure regions and are ascribed to flow of adsorbed material. An empirical equation is presented which correlates the observed flow rates with relevant adsorption isotherms. Classical equations of flow through elliptical and rectangular pipes are discussed with reference to flow through fine-grained porous materials. It is shown that equations of the Adzumi type are roughly valid as applied to fine-grained porous bodies, but that without a knowledge of the frequency distributions of pore sizes and shapes, flow data cannot be related to pore dimensions in any literal sense. End effects are discussed.


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