Enthalpy of adsorption and adsorption isotherms of polyacrylamide on sea sand

1995 ◽  
Vol 45 (1-2) ◽  
pp. 7-12 ◽  
Author(s):  
Xiang Song ◽  
Jie Ke ◽  
Buxing Han ◽  
Guanying Yang ◽  
Haike Yan

1992 ◽  
Vol 9 (1) ◽  
pp. 17-29 ◽  
Author(s):  
M. Saleem ◽  
M. Afzal ◽  
F. Mahmood ◽  
A. Ali

The porous nature of alumina has been investigated using various techniques. The values obtained for moisture content, surface area, pore volume, average particle size and porosity were 22%, 116 m2/g, 0.76 cm3/g, 17.0±0.5 μm and 68.0%, respectively. The adsorption isotherms of NdIII, PrIII and ErIII on alumina from aqueous solution have been obtained at different temperatures. All these adsorption isotherms obey the Langmuir, Freundlich and Dubinin-Radushkevich isotherm equations. Thermodynamic parameters such as the free energy, entropy and enthalpy of adsorption have been computed and interpreted. It is noteworthy that the adsorption of PrIII and NdIII increases with decreasing temperature while the reverse is observed for ErIII.



2020 ◽  
Vol 49 (30) ◽  
pp. 10295-10307
Author(s):  
Alexander Nuhnen ◽  
Christoph Janiak

This Perspective presents the procedure of the common Freundlich–Langmuir fit/Clausius–Clapeyron approach and the virial fit of adsorption isotherms with usable Excel sheets and Origin files for the subsequent derivation of ΔHads.



2012 ◽  
Vol 57 (10) ◽  
pp. 2766-2773 ◽  
Author(s):  
Wai Soong Loh ◽  
Azhar Bin Ismail ◽  
Baojuan Xi ◽  
Kim Choon Ng ◽  
Won Gee Chun


Author(s):  
Aili Ma ◽  
Chengqian Li ◽  
Wuqing Du ◽  
Jie Chang
Keyword(s):  


1977 ◽  
Vol 27 (1) ◽  
pp. 48-54
Author(s):  
Gerald C. Bye ◽  
Gilbert O. Chigbo


1981 ◽  
Vol 31 (1) ◽  
pp. 597-601 ◽  
Author(s):  
Karim Farag ◽  
Francis Perineau ◽  
Antoine Gaset ◽  
Jacques Molinier


Diabetes ◽  
1984 ◽  
Vol 33 (7) ◽  
pp. 674-680 ◽  
Author(s):  
M. V. Sefton ◽  
G. M. Antonacci
Keyword(s):  


Author(s):  
Г. Выхованец ◽  
G. Vyhovanec

Typical coastal elements of limans and lagoons are barriers, that separate limanic aquatories from a Seas. On limanic shores structure of the Black Sea sand barriers represented three longitudinal landscape “zones”: sea beach (“frontal”), dune-aeolian and limanic (“back of the barrier”). They closely interactive between themselves under influence of lithodynamical exchanges of sediment. General tendency of the barriers dynamics is displacement to Land direction.



2004 ◽  
Vol 68 (3) ◽  
pp. 795 ◽  
Author(s):  
Sabine Goldberg ◽  
Donald L. Suarez ◽  
Nicholas T. Basta ◽  
Scott M. Lesch


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